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The CANADIAN
FIELD-NATURALIST
Published by THE OTTAWA FIELD-NATURALISTS’ CLUB, Ottawa, Canada
Volume 118, Number 1 January-March 2004
125" Anniversary of the Ottawa Field-Naturalists Club 1879-2004
The Ottawa Field-Naturalists’ Club
FOUNDED IN 1879
Patrons
Her Excellency The Right Honourable Adrienne Clarkson, C.C., C.M.M., C.D.
Governor General of Canada
His Excellency John Ralston Saul, C.C.
The objectives of this Club shall be to promote the appreciation, preservation and conservation of Canada’s natural heritage; to
encourage investigation and publish the results of research in all fields of natural history and to diffuse information on these fields
as widely as possible; to support and cooperate with organizations engaged in preserving, maintaining or restoring environments
of high quality for living things.
Honorary Members
Edward L. Bousfield Bruce Di Labio John A. Livingston E. Franklin Pope
Donald M. Britton R. Yorke Edwards Stewart D. MacDonald William O. Pruitt,, Jr.
Irwin M. Brodo Anthony J. Erskine Hue N. MacKenzie Joyce and Allan Reddoch
William J. Cody John M. Gillett Theodore Mosquin Mary E. Stuart
Francis R. Cook C. Stuart Houston Eugene G. Munroe John B. Theberge
Ellaine Dickson George F. Ledingham Robert W. Nero Sheila Thomson
2004 Council
President: Mike Murphy Ronald E. Bedford Barbara Gaertner Stanley Rosenbaum
Vice-President: Gillian Marston Fenja Brodo Diane Lepage Louise Schwartz
Recording Secretary: Susan Laurie-Bourque John Cameron Christina Lewis David Smythe
Treasurer: Frank Pope William J. Cody Karen McLachalan Hamilton Henry Steger
Past President: Gary McNulty Kathy Conlan David Hobden Chris Traynor
Francis R. Cook Cendrine Huemer
To communicate with the Club, address postal correspondence to: The Ottawa Field-Naturalists’ Club, P.O. Box 35069, Westgate
P.O. Ottawa, Canada K1Z 1A2, or e-mail: ofnc @achilles.net.
For information on Club activities telephone (613) 722-3050 or check http//www.achilles.net/ofnc/index.htm
The Canadian Field-Naturalist
The Canadian Field-Naturalist is published quarterly by The Ottawa Field-Naturalists’ Club. Opinions and ideas expressed in this
journal do not necessarily reflect those of The Ottawa Field-Naturalists’ Club or any other agency.
We acknowledge the financial support of the Government of Canada toward our mailing cost through the Publication Assistance
Program (PAP), Heritage number 09477.
Editor: Dr. Francis R. Cook, R.R. 3, North Augusta, Ontario KOG IRO; (613) 269-3211; e-mail: fecook @achilles.net
Copy Editor: Elizabeth Morton
Business Manager: William J. Cody, P.O. Box 35069, Westgate P.O. Ottawa, Canada KIZ 1A2; (613) 759-1374
Book Review Editor: Roy John, 2193 Emard Crescent, Ottawa, Ontario K1J 6K5, e-mail: roy.john @pwgsc.gc.ca
Associate Editors: Robert R. Anderson Paul M. Catling David Nagorsen
Charles D. Bird Brian W. Coad Donald F. McAlpine
Robert R. Campbell Anthony J. Erskine William O. Pruitt, Jr.
Chairman, Publications Committee: Ronald E. Bedford
All manuscripts intended for publication except Book Reviews should be addressed to the Editor and sent by postal
mail. Book-review correspondence should be sent by e-mail or postal mail to Roy John, Book-review Editor.
Subscriptions and Membership
Subscription rates for individuals are $28 per calendar year. Libraries and other institutions may subscribe at the rate of $45 per
year (volume). The Ottawa Field-Naturalists’ Club annual membership fee of $28 (individual) $30 (family) $50 (sustaining) and
$500 (life) includes a subscription to The Canadian Field-Naturalist. All foreign subscribers and members (including USA) must
add an additional $5.00 to cover postage. The club regional journal, Trail & Landscape, covers the Ottawa District and Local Club
events. It is mailed to Ottawa area members, and available to those outside Ottawa on request. It is available to Libraries at $28 per
year. Subscriptions, applications for membership, notices of changes of address, and undeliverable copies should be mailed to:
The Ottawa Field-Naturalists Club, P.O. Box 35069, Westgate P.O. Ottawa, Canada K1Z 1A2. Canada Post Publications Mail
Agreement number 40012317. Return Postage Guaranteed. Date of this issue: January—March 2004 (December 2004).
Cover: A male Northern True Katydid, Prerophylla camellifolia Ottawa, from location 3 Figure 1 in Darbyshire pages 124-126.
This is the same individual as in Figure 2, page 125. Photographed by Stephen J. Darbyshire.
MCZ
LIBRARY
JAN § 2005
HARVARD
THERCANAIDEAIN (nt tae ©
FIELD-NATURALIST
Volume 118
2004
Volume 120
The Ottawa Field-Naturalists’ Club Transactions
THE OTTAWA FIELD-NATURALISTS’ CLUB
OTTAWA CANADA
ate
The Canadian Field-Naturalist
Volume 118, Number | January—March 2004
Origins and History of The Ottawa Field-Naturalists’ Club
DANIEL F. BRUNTON
216 Lincoln Heights Road, Ottawa, Ontario K2B 8A8 Canada; e-mail: dbruntonn211@rogers.com
Brunton, Daniel F. 2004. Origins and history of The Ottawa Field-Naturalists’ Club. Canadian Field-Naturalist 118(1): 1-38.
The Ottawa Field-Naturalists’ Club (OFNC) represents an unbroken chain of organized, non-governmental natural history
investigation and education dating back to the early days of the city of Ottawa itself. The Club originated in 1863 with the
formation of the Ottawa Natural History Society which became the Natural History branch of the Ottawa Literary and Scientific
Society in 1870, from which the OFNC formally separated in March 1879. Since that time, it has grown into Canada’s oldest
and largest regional natural history organization and has produced a diverse and internationally recognized publication
program. Since 1880 The Canadian Field-Naturalist and its predecessors have constituted the scientific core of the OFNC’s
publication program, with Trail & Landscape being an important Ottawa Valley publication since the late 1960s. The
importance of both publications to the growth and health of the organization is reflected in the major surges in Club
membership experienced when each of these publications was established. The focus of membership activities has changed
over the history of the OFNC, with enlightened natural resource management, then original scientific research and local
exploration directing energies in the early decades. By the early years of the 20" century the publications program become
the raison d’etre of the Club, almost to the exclusion of local field activities. A renewed interest in field discovery and the
growth of conservation awareness in the 1960s, however, rekindled local activities and re-established the balance which has
sustained the organization throughout its history. Natural environment education has remained a critical theme within OFNC
programs and activities. Over and above inspiring the professional careers and private interests of thousands of individuals
for more than a century, the OFNC has had an important and lasting impact on the conservation of natural environment
features and landscapes in Canada and North America.
Key Words: Ottawa Field-Naturalists’ Club; Ottawa Natural History Society; The Canadian Field-Naturalist; Trail & Landscape.
Canada was a mere 12 years old in 1879 when 34
members of the Ottawa Literary and Scientific Society
(OLSS) gathered together on an early spring evening
to discuss a growing problem within Ottawa’s fledg-
ling naturalist community. Most were full of Victorian
enthusiasm for discovery and intellectual advance-
ment and were convinced of the limitless potential of
their new country. These young men — and they were
all men, mostly in their 20s or 30s — were frustrated
by what they saw as an ineffective, moribund OLSS
Natural History Branch which did not serve their needs.
These impatient “young Turks” wanted to actually do
things, to get out into the countryside of the Ottawa
Valley to explore and discover its natural wonders. And
with true Victorian missionary zeal, they wanted to
share these revelations amongst themselves and with
the larger Canadian — even international — commu-
nity. All of this in the name of personal intellectual
development as well as the chance to advance the
scientific and applied benefits of such knowledge. That
was heady, revolutionary stuff in the staid, conserva-
tive Ottawa of March 1879 when how close one was to
Rideau Hall — the literal and figurative operational base
of the Governor General and his politically and socially
powerful entourage — dictated more about one’s status
and options than personal wealth or political position
(Gwyn 1984).
The events which unfolded that cool spring evening
in the OLSS rooms perched above the muddy streets of
Ottawa launched careers, changed government policy,
protected tens of thousands of hectares of Canadian
natural landscape, produced internationally recognized
and significant scientific publications, made huge con-
tributions to our understanding and appreciation of
North American natural sciences, and enriched thou-
sands upon thousands of lives. Oh yes ... and initiated
what has become the largest and oldest regional natu-
ralist organization in Canada’s history, The Ottawa
Field-Naturalists’ Club (OFNC).
The Pioneers (1840s-1863)
Although the formal beginning of The Ottawa Field-
Naturalists’ Club in 1879 was 125 years ago, natural-
ists’ organizations in the Capital actually pre-date Can-
ada itself (Brault 1946; Dore 1968; Taylor 1986). Prior
to Confederation, Ottawa (and Bytown before it) was
D THE CANADIAN FIELD-NATURALIST
a rude little lumber town characterized more by saw-
dust, beer and brawls than by intellectual achievement.
The only adult education or research institution pre-
sent in those early days was the Mechanics Institute,
a charitable organization initiated in 1847 as something
akin to a continuing education facility and library for
working men. There were no such things as “night
school” or public libraries, let alone publicly accessi-
ble research organizations. An informal group known
as the Silurian Society interested in geological (and
mining?) issues was also reported to be active in the
1850s. “Active” may be a misnomer, since they left
little reference of their doings, other than to suggest
that their meetings were held “in the City of Ottawa”
(Anonymous 1854).
The only natural environment research being under-
taken in the Ottawa Valley before the 1860s was by
three highly active individuals. Edward Van Cortlandt
(1805-1875) was the most socially prominent of these.
He was one of the first doctors in Bytown, arriving in
1832 to attend to the military personnel stationed on
Barracks Hill (now Parliament Hill). He developed an
extensive private museum of curiosities and artifacts in
the 1840s, liberally mixing archaeological specimens
found at aboriginal sites along the Ottawa River with
natural items dug up, collected, and/or shot in the
vicinity of the town. He was, by all accounts, a remark-
ably energetic man who used his high social standing
to influence local business leaders in natural resource-
oriented concerns (Moffatt 1986).
Another dynamo was Elkanah Billings (1820-1876)
(Figure 1), second son of one of Ottawa’s first pio-
neer families. Billings was passionately interested in
natural history in general and geology/paleontology
in particular. At various times he was a newspaper pub-
lisher (The Bytown Citizen, forerunner of The Ottawa
Citizen), a lawyer and finally, Canada’s first profes-
sional paleontologist. Indeed, this latter science was his
true calling and he came to be known as “the father
of Canadian paleontology” (Whiteaves 1876; Clarke
1971). He presumably was involved in the aforemen-
tioned Silurian Society, but no direct evidence of that
was found. The Bytown Citizen was full of natural his-
tory items during Billings’s tenure (1852-1856), mostly
representing accounts of his own observations or text
reprinted from European or American publications.
These publication activities led directly to his produc-
tion in Ottawa of Ontario’s first natural science journal,
The Canadian Naturalist and Geologist, in February
1856 (Figure 2). Delightful and insightful articles in
that first volume such as “On the species of woodpeck-
ers observed in the vicinity of Ottawa” (Billings 1856)
were based on his extensive travels in the Ottawa
Valley. They demonstrated both excellent powers of
observation and a keen appreciation of the importance
of documenting the appearance and constitution of
original landscape conditions. His move to Montreal
later that year to join Sir William Logan at the Cana-
Vol. 118
FiGure |. Elkanah Billings. Billings was born in 1820, became
one of the earliest naturalists in Ottawa, and pub-
lished the first journal on natural history in Ontario in
1856 (see Figure 2). He moved to Montreal later that
year to become the first palaeontologist of the Geo-
logical Survey of Canada, and the initial curator of its
museum. (reproduction of the OFNC-commissioned
portrait, from The Ottawa Naturalist, February 1901).
dian Geological Survey, however, permanently ended
his Ottawa connection (Zaslow 1975).
Elkanah Billings’ older brother, Braddish Billings Jr.
(1819-1871), completes the trio of Ottawa’s pioneer
resident naturalists. Braddish was a keen botanist and
used his position as chief clerk on the Prescott & Otta-
wa Railway to gain access to a wide variety of habitats
across eastern Ontario. Although he published nothing
during this time and relatively little even later, in 1868
he did produce the first list of vascular plants for the
city of Ottawa. It was a superb effort for its day, chron-
icling over 400 species that he found within close
proximity to the City in 1866 (Dore 1968). Billings
was seen as a distinguished figure in natural history
investigations in the Ottawa Valley in the 1860s; like
his younger brother Elkanah, Braddish was widely
consulted by natural science researchers elsewhere in
Canada (Dore 1968).
The days of exclusively private investigation of the
Ottawa Valley natural environment ended in the early
————s
S i,
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F EN_AS AN Vise AD OAS CPS ON BESO Oh _ B
i 4 Gentiemen to whom this Number is sent, and who do wot wish to
i (O Sabserive, arc respectfully requesied to return the same.
RG eee re
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ee «68H CANADIAN
Waturalist «Grnlogist, &
By E. BILLINGS, Barrister at Law,
OTTAWA, CANADA WEST.
Pay lURee
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Corama Fosstts, (Glyptocrizus rainulosus) x new species of Lily Enerivite, fromthe —
~ Trenion Linestose, Bighanys Lake, Coumy of Gilawa.— See quge 54, :
: UBLISHED AT THE OFFICE or tue OTTAWA CITIZEN, OTTAWA.
FIGURE 2. The Canadian Naturalist and Geologist, first pub-
lished in 1856 at the office of The Ottawa Citizen by
Elkanah Billings, and later continued in Montreal.
1860s with the transfer of the seat of government of the
colony of Canada to Ottawa, heralded by the start of
construction of the new Parliament Buildings in 1860
(Eggleston 1961). This represented a mega-project with
huge economic benefits to local businesses. Similarly,
the 1863 transfer of some 300 bright, educated, and rel-
atively financially secure members of the civil service
from the old capital represented both economic and
social opportunities for the city and the Ottawa Valley.
Confederation-era city business and social leaders
quickly embraced the idea of broadening and deepen-
ing the intellectual resources of the community. In
furtherance of this, they encouraged the development
of various clubs and societies to enhance the prestige
and intellectual capacity befitting the new capital (Brault
1946; Gwyn 1984).
It is useful to consider how really rough and ready
Ottawa and the larger world were in 1863. The Arctic
was still largely unknown to Europeans and North
Americans alike but was being charted with great speed
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 3
by the continuing search for the ill-fated Third Frank-
lin Expedition. The United States Civil War and the
accompanying ferocious slavery debate raged uncom-
fortably close to the south, as did intense arguments in
the Old World regarding the newly published (1859)
“heresies” of Charles Darwin’s On the origin of spe-
cies. Closer to home, Ottawa was a bustling, rapidly
growing city of approximately 15 000 people which
boasted but a single operating sewer line along Welling-
ton Street in front of the new Parliament Buildings. The
first railway train had puffed into town fewer than ten
years earlier and a municipal drinking-water system
was still 12 years off (Brault 1946; Eggleston 1961).
Ottawa was very much straddling the line between
pioneer lumber town and developing political centre.
The Ottawa Natural History Society (1863-
1869)
It is against this backdrop that a veritable “Who’s-
who” of the new business and professional elite of
Confederation-era Ottawa (notably including both the
aforementioned Edward Van Cortlandt and Braddish
Billings Jr.) assembled on 3 October 1863 to form the
Ottawa Natural History Society (ONHS). These gentle-
men — and the ONHS constitution made it clear that
membership was open only to gentlemen — were very
economically oriented. The original minute books
maintained in the OFNC collection at Library and
Archives Canada (LAC) records that they were “ ...
desireous to develope [sic] the Natural History of the
Ottawa and general resources of the surrounding coun-
try” (LAC OFNC Collection, 3 October 1863). Explor-
ing and researching the natural sciences of the Ottawa
Valley were all well and good but these gentlemen —
at least initially — wanted to see a profit result from it.
An important aspect of the growth of such endeay-
ours was the potential participation of the relatively
large body of newly arrived civil servants (Brault 1946).
Activity within quasi-professional associations (it’s
called “networking” today) was a very important un-
official avenue for professional advancement within the
small professional community of public servants in the
Capital at this time (Gwyn 1984). The ONHS offered
such an outlet and avenue for civil servants interested
in natural resources and natural environment issues.
A definite pecking order mirroring that of their profes-
sional relationships was soon evident amongst found-
ing ONHS members who were also senior civil ser-
vants. When powerful Finance Department Deputy
Minister John Langton (1808-1894) was ONHS Presi-
dent in the late 1860s, for example, his ambitious sub-
ordinate, Interior Department Deputy Minister Edmund
Meredith (1817-1898), was conspicuously involved in
the organization, but was careful not to hold higher
office nor to publicly disagree with Langton (Gwyn
1984). The social/political significance of the organi-
zation, over and above the fact that 77 men paid the
$1.00 membership fee for 1863/1864, can also be meas-
4 THE CANADIAN FIELD-NATURALIST Vol. 118
ured by the prominent involvement of individuals such
as Sir James A. Grant (1831-1920), the Governor Gen-
eral’s personal physician (Travill 1988) (LAC OFNC Sls = =
Collection, 3 October 1863). iD = oben re ois
The ONHS members chose widely appreciated and £ g 2 a 2 z si cs 6
politically-neutral Braddish Billings Jr. as their first 2) 5 E ee = mm O68 S
president, although he was not very active in subse- S A lai = = = a Ss ice
quent Society affairs (LAC OFNC Collection, 3 Oc-
tober 1863 — 28 October 1864). The Council (Board
of Directors) soon established a schedule for regular =
meetings and made arrangements for the development s =
of “The Cabinet’, a series of cases displaying natural ARE Aer mes = E
: 3 E 3 ‘oO oo av 2 >)
history specimens which were to be held in the rooms eg Weipa) ds se 2
they rented at the Mechanics Institute building on ea Bg Bi = & mm Ss
Sparks Street. Van Cortlandt was elected museum coho areas Re) ead Teal
curator for the Society and remained in that position
throughout the life of the organization. s
Although precise records are sketchy, records at a os =
Library and Archives Canada indicate that the Society eS ees Saas
: Xe) os oY & o
met regularly for lectures and field trips. The last C2 Milfsseehy ssi Sho 2
Saturday of each month was fixed for the latter (LAC Ss 8 ae S = = OS
OFNC Collection, 28 April 1865), during which mem- chr een ee areal i age bad ifs teal
bers actively searched for natural history specimens for
The Cabinet. Indeed, this seemed to be a major focus s
of the organization (Dore 1968). In October 1869, only wee &
months before the organization’s amalgamation with ur 2 ge gel es 5
the Mechanics Institute, Braddish Billings offered his ca) = = Se Ss a
herbarium to the ONHS for $60 (LAC OFNC Collec- Ra ES Es & = & A s
tion, 1 October 1869). Although no supporting motion Co Zagtesie tes te ee} (e\ al
for such a purchase is noted, Billings’s collection did
end up there (it may have been deposited after his 3
death), and was examined in the OLSS museum in the 5 oa thie &
1880s (Fletcher 1888). Unfortunately, the OLSS herbar- e [2+ Bee Fs 5
ium, including the Billings’s specimens, disappeared 2 bere seee 2
sometime in the early 20" century (Dore 1968). g Ali olepese Haya daeiply
The ONHS seems to have been most active between oe ea PA (as esis ea eh teal
1865 and 1867 and to have achieved considerable ic}
standing in the community. In 1866 a group met with S D es
federal Minister Thomas Darcy McGee to discuss a oe in 2
possible ONHS — Mechanics Institute exhibit in the = 8 eae te % :
1867 Paris Exhibition (LAC OFNC Collection, 26 SS ie a Be a2 S
April 1866). Their paths had crossed before, in Que- >a Ie a ae os 3
bec City in 1862-1863, McGee had lectured to the Ss1% BS =S <Os 3%
Quebec Literary and Historical Society along with a of
both E. A. Meredith and John Langton. And while the aS
subject of his speech was not recorded, the Governor = = : ‘2 % 3 =
General apparently spoke to the Society shortly there- é 3 a a 8 aie) ae = S
after (LAC OFNC Collection, 25 May 1866). Within PSS |S 252 88) vols
a month of Confederation an ONHS delegation led by 5 2 SS a § iz § gx Salles
President N. B. Webster lobbied Prime Minister John sE IS c = a ss = HAs z =
A. Macdonald to have the Geological Survey Museum a. || it Ts Sa es
moved to Ottawa from Montreal (LAC OFNC Collec- g 3 5
tion, 26 July 1867) — possibly the first such initiative in aie, i =
the lengthy campaign to effect such a transfer (Zaslow 3Z & 5 BS,
1975). Similarly, early concerns for habitat protection 2 5 2 ¥ = 3
and landscape conservation were discussed amongst the a Q co pee tn i g SS
Society’s influential membership through presentations ae 8 2 gs 2 ay S 5)
like Vice-President Thomas Austin’s lecture “The UI- a & i ae 5 3 ESs|2
ae pa ea el (455) ||
2004
terior Effects of Clearing off the Forests and Draining
the Country” (LAC OFNC Collection, 26 April 1866).
While The Cabinet may not have survived, the Soci-
ety left a more lasting (albeit, modest) record through
its publications program. It commenced in 1867 with a
pamphlet on the possible economic uses of Milkweed
(Asclepias syriaca) by Alexander Kirkwood (1823-
1901) who, with the timely promotional assistance of
ONHS member and OFNC founder Henry B. Small
Sr. (1832-1919), would later be the driving force be-
hind the establishment of Ontario’s Algonquin Prov-
incial Park (Killan 1993). The ONHS published 250
copies of Kirkwood’s lecture (Kirkwood 1867). Ap-
proval for the production of 250 copies of a lecture by
Van Cortlandt entitled “Native Compounds and Metal-
lurgy of Iron” was given by the Council the previous
year but there is no evidence that a publication actually
resulted (LAC OFNC Collection, 28 December 1866).
After a year of discussion and buoyed by the success of
the Kirkwood pamphlet, however, an ONHS Trans-
actions series was initiated. It was short lived, produc-
ing only three numbers. !
Faced with rising financial pressures (including the
costs of renting rooms) and the opportunity to formally
combine resources (including a provincial operating
grant), the ONHS decided in the spring of 1869 to
merge with the Mechanics Institute (LAC OFNC Col-
lection, 16 April 1869). The minutes books describe
surprisingly little of the ensuing discussion, but the
Society did merge with the Institute to form the Ottawa
Literary and Scientific Society (OLSS) on 24 December
1869 (LAC OFNC Collection, 30 December 1869). The
ONHS Cabinet became the basis for the OLSS muse-
um, whose collections disappeared with the dissolution
of the Society in 1906-1907. Unpublished biological
data were apparently also maintained in the Museum,
however, as indicated by later reference (containing
several errors in fact) being made to “lists published
by the Ottawa Natural History Society of 1859-63”
(Small 1883).
Although active for only a decade, the ONHS was
critical in the awakening of interest in the organized
and documented investigation of natural sciences in the
Ottawa Valley. It bridged the gap from hit-and-miss
personal interest to organized and semi-professional in-
vestigation. It also initiated the concern for and partici-
pation in larger issues of national science policy, re-
search priorities, and natural environment conservation
which continue within the Ottawa naturalist commu-
nity to the present day.
The Ottawa Literary and Scientific Society
and OFNC formation (1870-1879)
The combination of the ONHS and the Mechanics
Institute appears to have been seamless, with the mem-
bers of the ONHS effectively becoming the Natural
History Branch of the newly created OLSS. Little
documentation was found, however, concerning the re-
sulting organization in general and the activities of its
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 5
Natural History Branch in particular. Nonetheless, the
OLSS was a socially and culturally significant orga-
nization in Victorian Ottawa by the end of the 1870s,
supporting a regular lecture series, a public reading
room and a lending library of 1100 volumes (LAC
OFNC Collection, OLSS brochure). Despite the larg-
er city population, better local research resources and
the existence of a potential sponsoring organization,
however, there are few indications of more than indi-
vidual efforts in natural science investigations in the
Ottawa Valley. At the least, the momentum of the
1860s seems to have been stymied within the larger,
predominantly culturally-oriented OLSS. The stage was
set for a final transformation of the ineffective OLSS
Natural History Branch into a new and more produc-
tive structure ... an independent naturalist group.
If the organization that morphed into the OFNC
actually began in October 1863, the final stage of its
transformation was achieved with the cordial separa-
tion of the Natural History Branch from the main body
of the OLSS in March 1879. It appears to have been
a classic example of a group of activists becoming
dissatisfied with the pace and effectiveness of a well-
established group and deciding that the only way to
achieve more contemporary goals was to strike out on
their own. The fact that most of the prime movers and
shakers in the new organization were established mem-
bers of the old OLSS and remained members for years
thereafter, indicates that they retained faith with the
original organization as a valuable forum for intellec-
tual development and social debate. Nonetheless, they
wanted to see more activity and greater opportunities
being provided for natural environment investigations
(Harrington 1909).
Once again, national and world affairs played an
important role in the development of naturalist organi-
zations in the Ottawa Valley. Canada was experiencing
the early years of a serious economic downturn that
lasted into the early 1890s (Eggleston 1961). At the
same time, the promise of this new country and the
political, social and economic difficulties of the Old
World were encouraging huge numbers of young, rela-
tively well-educated and mobile immigrants to enter
Canada; some stayed and some moved on in this time
of social and economic upheaval. The decade follow-
ing the founding of the OFNC, for example, saw the
highest number of both Canadian immigrants and emi-
grants of any time in the 19" century (Lingard 1967).
Young Turks and Rebels (1878-1879)
The group which gathered in March 1879 to con-
sider a new natural history organization in Ottawa re-
flected its times. This included a mix of Ottawa vet-
erans enthusiastic about the future, as well as young,
newly-established civil servants, and British immigrants
full of imperial fervour. They seem to have been imbued
with Victorian optimism about the importance and
strength of ideas, a missionary zeal for discovery and
the sharing of knowledge, and a strong desire to con-
6 THE CANADIAN FIELD-NATURALIST
tribute to their community (LAC OFNC Collection,
25 March 1879-15 December 1879). Some stayed on
to become important participants in the exploration of
the Ottawa Valley natural environment while others fol-
lowed different paths elsewhere in Canada and beyond.
The founding meeting was called by James Fletcher
(1852-1908), OLSS museum curator since 1878 and
an up-and-coming entomologist and botanist (Figure
4). Fletcher had emigrated from England in 1874, mov-
ing to Ottawa in 1875 to work as a clerk in the Bank of
British North America and joining the Parliamentary
Library staff as an accounting clerk in 1876 (Cody et
al., 1986). He was a gregarious, personable, and phys-
ically active man who quickly became deeply involved
in sporting and social activities. He was, for example,
a keen snowshoe racer and a founder and principal
player with the Ottawa Football Club, a rugby team
which later evolved into the Ottawa Rough Riders Can-
adian Football League team (Harrington 1909). He was
also a pillar of the Anglican Church community in
Ottawa and remained so throughout his life. And, while
being a young man with shallow Ottawa roots, his so-
cial profile, and thus influence, improved dramatically
when he married Eleanor Schreiber (daughter of Sir
Collingwood Schreiber, Chief Engineer of the Canadian
Pacific Railway and later Chief Engineer of the Depart-
ment of Railway and Canals) in 1879.
Fletcher’s enthusiasm, intelligence, and boundless
energy quickly became known to the small group of
active field naturalists already resident in Ottawa and he
was eagerly sought out (Whyte 1909). Chief amongst
these field associates and life-long friends were Robert
B. Whyte (1851-1918), an Ottawa-born private busi-
nessman and passionate horticulturalist (Macoun 1918)
(Figure 5). The other was William (Will) H. Harring-
ton (1852-1918), a skilled entomologist and botanist
who moved from Nova Scotia in 1870 and spent his
entire working career with the federal post office
department (Gibson 1918). While Whyte is credited
with the idea of an Ottawa Field-Naturalists’ Club,
Fletcher is universally credited with being the fellow
Vol. 118
who made it happen and saw to it that it became firm-
ly established (Harrington 1909; Whyte 1909).?
The dynamic trio of young naturalists were not alone
in this, and were joined by an eclectic mixture of OLSS
members who also felt the need for an organization
focusing exclusively on natural sciences. Many were
prominent in the building of Ottawa and/or the federal
civil service of the new country (Brault 1946; Gywn
1984). These included former ONHS officer and senior
Post Office Department official William White (1830-
1911) (Figure 3); lawyer and politician (later, Premier
of British Columbia) Joseph Martin (1852-1923); for-
mer ONHS officer, teacher, and Geological Survey of
Canada (GSC) librarian John Thorburn (1830-1904);
author and later Deputy Minister of the Interior Henry
Small Sr., and the OLSS president of the day, promi-
nent literary patron and Secretary (Deputy-Minister)
of the Post Office Department, William D. LeSueur
(1840-1917) (LAC OFNC Collection, 25 March 1879).
As noted earlier, the social and political prominence
of members was important to the success of such or-
ganizations in Victorian Ottawa (Gywn 1984). This
early naturalist community (Table 2) was small and
remarkably homogenous, dominated by white, English-
speaking, Anglo-Saxon protestants who worked, lived
and even were buried in close proximity. Overwhelm-
ingly, the children of most early club leaders were
enrolled in the Ottawa Collegiate Institute (MacMillan
et al. 1904), and numerous Club officers — including
almost two dozen former Presidents — are buried at
Beechwood Cemetery. Beechwood, appropriately
enough, was also a favoured 19" Century OFNC ex-
cursion site (Reddoch 1979c).
Founding Meeting (25 March 1879)
The special meeting of OLSS Natural History
Branch members was called to order in the OLSS
museum at 112 4 Sparks Street by James Fletcher (Fig-
ure 4) on 25 March 1879. It seems that the politics
of Victorian Ottawa immediately intervened, however, as
William White (Figure 3) and R. J. Wicksteed moved
TABLE 2. Participants at inaugural meeting of the OFNC, 25 March 1879
(LAC OFNC Collection, 25 March 1879).
W. P. Anderson L. A. Hamilton Dr. Ross
E. D. Arnaud W. H. Harrington H. B. Small Sr.
Prof. George Baptie G. Heron H. B. Small Jr.
W. R. Billings G. A. D. Jones P. D. Symms
W. Chesterton E. V. Johnson John Thorburn*
L. H. Chrysler W. D. LeSueur* H. Watters
R. A. Davy J. Martin W. White*
James Fletcher B. Monk R. B. Whyte
J. M. Greta S. McLaughlin* R. J. Wicksteed*
J. MacD. Gordon Prof. W.R. Riddell A. P. Wright
J. A. Guignard
D. Horsey
*member of ONHS (1863-1869)
C. J. Ripley
P. Robertson
2004
FiGurRE 3. Lieutenant-Colonel William White, May 1901. White
was the first president of the Ottawa Field-Naturalists’
Club, and also the Ottawa Horticultural Society. Earlier
he was president of the Ottawa Athenaeum and Mech-
anical Institute. Photographer William James Topley,
Ottawa, archived at the Library and Archives of Can-
ada, Ottawa: E 81666).
that fellow ONHS veteran John Thorburn chair the
meeting. Perhaps to counter this old guard move, new-
comers Joseph Martin and Henry B. Small Jr. subse-
quently moved that Fletcher be made Secretary of the
meeting. The social pecking order apparently satisfied,
Fletcher then got discussion under way (LAC OFNC
Collection, 25 March 1879).
After some debate of whether to stay affiliated with
the OLSS or to form a separate group, the actual mo-
tion to establish an independent OFNC was moved
by Joseph Martin (seconded by R. B. Whyte): “...
that it is advisable to form a Field Naturalists Club
for the City of Ottawa and do proceed to organize”.
It was only after this motion had been passed that
Fletcher reported to the gentlemen assembled that a
small group (consisting of at least James Fletcher, Will
Harrington, R. B. Whyte (Figure 5), Joseph Martin,
and Henry Small Jr.) had actually held preliminary
consultations on 11 March 1879 to prepare a proposal
to the Council of the OLSS — and no doubt, to map
out strategies. At that preliminary meeting they had
drafted a motion (Fletcher, seconded by H. B. Small
Jr.) that in light of “... an Ottawa-Field Naturalists
Club having been organized in Ottawa...”, this new
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 7
group “... would gladly contribute to the Museum of
the OL & S Society and thereby revive its present
dormant condition”. In exchange, they asked that the
OFNC be allowed to use the OLSS rooms for meetings.
An additional clause asking that the new organization
be “under the auspices” of the OLSS was an apparent
face-saving offer, since the OFNC had virtually noth-
ing further to do with OLSS programs.’ The resolution
was passed by the OLSS Council, though there likely
was little else they could do, being presented with such
a fait accompli. There may have been a good bit of bluff
on the part of Fletcher and his associates, however,
since the Club did not in fact exist on 11 March when
the motion was drafted!
If this was not-too-subtle political manipulation by
the newcomers, the old guard may well have reaped a
bit of revenge in the election of OFNC officers which
followed immediately thereafter. William White, long-
time Ottawa resident, former Mechanics Institute pres-
ident and ONHS member, was elected President. It is
not recorded in the Minute Books if the officer positions
were contested that day, as was often the case in the
first years of the organization. Likely more important
than being an ONHS veteran, White was a senior Post
Office Department official and was socially prominent
as Lieutenant-Colonel of the Governor General’s Foot
Ficure 4. James Fletcher in June 1908. He called the founding
meeting of The Ottawa Field-Naturalists’ Club and was
the prime architect of its early success. Photogra-
pher William James Topley, Ottawa, archived at the
Library and Archives of Canada, Ottawa C96620).
8 THE CANADIAN FIELD-NATURALIST
Guards (Shutt 1912; Anonymous 1929). His election,
however, may very well have also been the wish of the
newcomers since White’s Rideau Hall connections
made the important task of securing the agreement of
the Governor General to serve as Club Patron that
much easier.
The minutes of the founding meeting (LAC OFNC
Collection, 25 March 1879) are very sparse in detail.
As Secretary, James Fletcher would have produced a
hand-written record of events. The preserved minutes
are in the handwriting of R. B. Whyte, however, indi-
cating that Fletcher’s record of events was rewritten.
The development of this simplified record could per-
haps have allowed for the tactful omission of politically
delicate matters such as contested positions and/or
heated exchanges.
In any event, James Fletcher was elected First Vice-
President and the Council and Officer positions were
filled by other young rebels (R. B. Whyte, Henry B.
Small Jr., W. H. Harrington, and Joseph Martin) or
neutral figures (W. R. Riddell and J. A. Guignard)
(Appendix 1). Only one Council position was filled
by a White associate, William P. Anderson (1852-
1927), who also later became Lieutentant-Colonel of
the Governor General’s Foot Guards (Small 1929).
As it turned out, however, Fletcher essentially ran the
affairs of the OFNC in 1879 and 1880, with White
playing a very low-key role.
Earliest Days (1879 — 1880)
The first Council meeting of the new Club was held
under the chairmanship of William White on the after-
noon of 3 April 1879 in the Museum of the OLSS
(LAC OFNC Collection, 3 April 1879). It was fol-
lowed almost immediately by another, longer session
at the home of William Anderson on 5 April 1879 to
prepare details for a formal members’ General Meet-
ing the following Tuesday (8 April 1879) and to accept
the resignation from the Council and from the Club of
J. A. Guignard. No reasons were given for the speedy
and rather dramatic resignation of Guignard but des-
pite being James Fletcher’s assistant at the Experi-
mental Farm from 1891 onward, he did not ever re-
join the Club. He did, however, function as Acting
Editor of The Ottawa Naturalist for several months
in 1903 (Brunton 1986a).
The Ottawa Field-Naturalists’ Club first met public-
ly on 8 April 1879 under the chairmanship of James
Fletcher with about 25 members in attendance in the
Museum of the OLSS. Operational rules for the Club
were described, a Corresponding Members (Honorary
Member) designation was identified, an active excur-
sion program was laid out, and a membership fee
(SO0¢ per annum) was established. The fee was half
that established by the ONHS 16 years earlier, presum-
ably in an effort to keep membership in the OFNC
more affordable for the general public. And also un-
like the ONHS, the OFNC specifically identified mem-
Vol. 118
bership as being open to both “ladies and gentlemen
desiring to join the Club” (LAC OFNC Collection, 8
April 1979).°
There were 25 OFNC Council and public meetings
held in 1879/1880, the busy first year of the newly
independent Club. Most of the public meetings were
in the form of somewhat informal soirées in which
lectures were followed by opportunities for debate and
conversation. Through this year the Council addressed
numerous details of the developing organization in-
cluding the arrangement of Vice-regal patronage, the
establishment of an active excursion program, the
selection of the first OFNC Corresponding Member
(John Macoun [1831-1920]) (Brunton and Gummer
1987), and recognition of the importance of “public
education” (the first gimmers of conservation action?).
James Fletcher was everywhere in this, conducting ex-
cursions, conducting and documenting field research,
and handling many logistical details. President White
chaired 12 of the meetings that year, only a few more
than Fletcher, who oversaw nine because of the presi-
dent’s frequent absence (LAC OFNC Collection, 1879-
1880).
The establishment of various scientific working com-
mittees (botany, ornithology, geology, etc.) generated
a great deal of interest and field activity within the
Ottawa District®, resulting in considerable natural en-
vironment information being gathered. Membership
grew to almost 100. The influence of Lieutentant-
Colonel White and others secured the patronage of
the Governor General and made OFNC membership
socially desirable. This was aided by the membership
within the first year of prominent individuals like the
previously-mentioned Governor General’s personal
physician, Sir James Grant; the founder of the Central
Experimental Farm research institution, Sir William
Saunders (1836-1914) (Anstey 1988; Cody et al.,
1986); and prominent scientist, engineer, and inventor
Sir Sandford Fleming (1827-1915) (Regehr 1988).
The lectures delivered at the Soirées were well
received, leading to requests for their publication for
the benefit of members and other interested parties
alike. The March 1880 Council meeting established
that a transaction of the OFNC’s first year be produced.
Five hundred copies of that first Transactions were
published for a cost of $78.43, likely in June 1880
(Brunton 1986a) (Figure 8). In appreciation of his
production of the lithographed plates for the publica-
tion at no cost, the Council granted Club membership
for the year to J. A. Guignard — the same gentleman
who had resigned from the Council as well as from
Club membership, only days after the Club had been
formed (LAC OFNC Collection, 28 July 1880). This
was done again in 1882 for additional gratis litho-
graphic services, so it appears that whatever difficulty
Guignard had with being on the Council and being a
voluntary Club member, he was prepared to receive
and work for the publication.
——
2004
FicurE 5. Robert B. Whyte, (June 1908), was first secretary-
treasurer and later president of the Ottawa Field-
Naturalists’ Club. Photographer William James Topley,
Ottawa, archived at the Library and Archives of Can-
ada, Ottawa: C 105521).
Publication of the Transactions was the first step
in a renowned publication program that, to date, has
produced seven annual Transactions of The Ottawa
Field-Naturalists’ Club, almost 120 volumes of The
Ottawa Naturalist/The Canadian Field-Naturalist and
almost 40 volumes of Trail & Landscape. Complete
sets of The Canadian Field-Naturalist and its prede-
cessors are rare, however, particularly so in private
libraries. Likely fewer than a dozen complete sets
exist in Canada. The Transactions are especially rare
publications, several of which became unavailable
within a few years of publication. Only 75 copies of
Transactions | were still available by early 1884, for
example (LAC OFNC Collection, 12 March 1884),
and only “virtually complete sets” were being sold (for
$24) by 1909 (LAC OFNC Collection, 23 February
1909).
The Late Victorians (1880s-1890s)
The OFNC was a huge hit at the height of the Vic-
torian era in Ottawa. Aided by improved transportation
— most particularly, the expansion of railways up the
Ottawa and Gatineau Valleys — and the continued
growth of both the federal civil service and the city
(exploding to 60 000 by 1899 — Brault 1946), huge
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 9
strides were being made in the exploration and under-
standing of the natural biodiversity of the Ottawa Valley.
Transfer of the Geological Survey of Canada from
Montreal to Ottawa in 1880 (Zaslow 1975) and with
it, many of the top natural scientists in Canada, pro-
vided a major boost to the OFNC. So too did the 1882
arrival of John Macoun (Macoun 1922). Through their
network of professional connections, Macoun and other
scientists at “The Museum’, as it was known, also
provided an important link between OFNC members
and national and international floral and faunal au-
thorities. Despite becoming increasingly preoccupied
with professional duties after he became Dominion
Entomologist and Botanist in 1886 (Cody et al., 1986)
and being troubled by serious eyesight problems for
a period of time (LAC OFNC Collection, 17 March
1885), James Fletcher remained an inspirational and
hands-on leader within the OFNC throughout the 1880s
and 1890s.
Club membership had more than doubled to 254 by
1899 (Figure 6). This was due to both local and wider-
scale influences. On the local front, OFNC excursions
became major social events and major generators of
additional interest in the organization (Reddoch 1979c).
These were often huge events, with trains being char-
tered to take upwards of 300 participants on day-long
trips. Fortunately, many sites now well within the urban
core of the National Capital Region were in close to
original condition then and became prime locations for
many formal and informal outings. Chief amongst these
were Lac Leamy, Fairy Lake, and Wychwood (Aylmer)
in Gatineau, and Rockcliffe Park, Beechwood Ceme-
tery and the Billings Bridge (Rideau River) area in
Ottawa. Further afield, the huge Mer Bleue peat bog
and Casselman to the east, and King Mountain and
Chelsea to the north offered “exotic” destinations that
were visited repeatedly (Reddoch 1979c).
In striking contrast to the early to mid-19" century
days of the ONHS and its predecessors, these efforts
were well documented in OFNC publications. The
annual Transactions, modelled on the Transactions
of the Manchester Field-Naturalists’ Society (Brunton
1986a), were produced through much of the 1880s.
Each Transactions reproduced Club lectures delivered
during the previous year. More importantly, they includ-
ed annual reports of various committees highlighting
the field discoveries of members. The Transactions
thus provided the first documentation of a variety of
comprehensive lists of Ottawa area flora and fauna,
such as birds (White and Scott 1882), vascular plants
(Fletcher 1880), and fish (Small 1883). Against these,
individual members could compare and direct their own
field investigations and discoveries. Fletcher’s serial-
ized, annotated revision of the 1880 list of vascular flora
was produced over many years thereafter, providing a
continuing enumeration of new discoveries and poten-
tial exploration sites for OFNC members (Boivin and
Cody 1955).
10 THE CANADIAN FIELD-NATURALIST
After seven annual Transactions had been produced,
there were increasing calls for a more frequently
appearing publication. This was particularly important
for the description of new species (LaRocque 1931),
the first being a new fossil which had been described
in Transactions 2 by Sir James Grant (Grant 1881).
At the March 1887 Annual Meeting members agreed
to initiate a monthly publication series which could
move beyond the simple publication of Club lectures
and reports. This was over the objections of W. P.
Anderson, the current OLSS President, who had com-
plained the previous fall of OFNC “antagonism” to-
wards the old Society (see above); he wanted the
Transactions to stay as they were (LAC OFNC Collec-
tion, 14 March 1887).
The first issue of The Ottawa Naturalist was pub-
lished in April 1887 under the editorship of Will Har-
rington, who also had headed up the editorial com-
mittee which produced the last (1886) volume of the
Transactions (Brunton 1986a). The Ottawa Naturalist
was a small (21 x 14 cm), slim (16 page) publication
produced on a shoe-string budget (150 copies at $18.50
per issue) (LAC OFNC Collection, 10 March 1887).
Even then, such a cost was considered a financial dif-
ficulty for the Club (Harrington 1887) but was off-set
to some degree by the sale of advertising space on the
back cover. These advertisements included notices to
such “critical” products and services for the attention
and consideration of Ottawa naturalists as G. W.
McCullough’s Anthracite and Bituminous Coal, C.
Ross & Co.’s “Beautiful selection of Dress Silks being
offered at 75¢ per yard”, and Miss Harmon’s Board-
ing and Day School for Young Ladies.
Not only the advertisements may have met with
amusement or disapproval in the eyes of some. In 1888
the always feisty John Macoun expressed the opinion
that “too much trash was now published”, and that
“the majority of papers were of little or no value ...”;
that the accounts of Excursions were “all but worth-
less”. It is not recorded what Editor Will Harrington
might have thought upon hearing this (he undoubtedly
was present), but OFNC president R. B. Whyte was
not amused by Macoun’s intemperance. Whyte stated
that he “ ... wished to record his expression as direct-
ly opposite [Macoun’s] and thought the publication
was of much interest to the members” (LAC OFNC
Collection, 9 March 1888).
Regardless of the reservations of people such as
William Anderson and John Macoun, The Ottawa
Naturalist established a new standard for the timely
presentation of technically sound, original scientific
information which has continued seamlessly to the
present day. Its launch, however, was also far from the
last time controversy and disagreement would charac-
terize discussion and debate about OFNC publications!
Both the growth in local capacity for natural envi-
ronment research and the evolving vision of the Club’s
Vol. 118
role are indicated by Council’s November 1887 rejec-
tion of a gift of biological specimens from Corres-
ponding Member and American entomologist Henry
Edwards (1830-1891) (Fletcher 1891). The Council
(with both John Macoun and James Fletcher present)
suggested that the potential donor should offer the
plant specimens to the herbarium of the Central Exper-
imental Farm (DAO) which had recently been started
by Fletcher and is now the largest collection in Canada
(Rothfels 2003); they further suggested that Edwards’s
insect specimens be offered to the Geological Survey
Museum (LAC OFNC Collection, 18 November
1887). There was no discussion of a donation to the
OLSS collection, nor of initiating an OFNC museum
or cabinet. Neither, it appears, was deemed appropri-
ate in light of the existence of these growing, pro-
fessionally based research collections.
By the end of the 19" century, the personality of
the Club had also evolved considerably. The OFNC
was now administratively well established and boasted
a program of regular meetings and excursions. It en-
joyed a strong reputation for community involvement,
produced a steady stream of field-based scientific find-
ings, and even demonstrated a measure of political
prominence with Laurier government cabinet minis-
ters and future provincial Lieutenant-Governors as
members. The parent organization from which it had
split off, on the other hand, was in serious decline and
only a few years from dissolution. The young turks who
had rescued the OFNC from the moribund OLSS
Natural History Branch were middle aged and well
established now, a number having become respected
senior scientists and policy makers. The Ottawa Nat-
uralist remained a monthly publication but had grown
in size and enjoyed much improved printing quality.
Articles often now were accompanied by illustrations,
these sometimes being photographic. The Ottawa Nat-
uralist was gaining a wider readership too, with articles
addressing subjects considerably further afield than
the Ottawa Valley, such as the review of the status of
bird species in King’s County, Nova Scotia (Tufts
1898; 1899a; 1899b).
But portents of future conflicts and a growing diver-
gence of visions could be sensed. Founder and Past-
president R. B. Whyte, for example, complained about
the Nova Scotia bird articles. He felt The Ottawa Nat-
uralist should not be publishing material so far removed
from the Ottawa area. Botanist James M. Macoun
(1862-1920) and geologist Henry Ami (1858-1931)
disagreed, suggesting that the Club publication fulfilled
an important role here. Other new members support-
ed Macoun and Ami and called for a greater number
of rigorously scientific, more broadly based articles to
be included in the publication (LAC OFNC Collection,
14 March 1899).
In other words, a new group of younger, more vig-
orous, field-oriented naturalists — including a number
2004 BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 1]
Number of Members
assis ctor ieee
Ficure 6. Ottawa Field-Naturalists’ Club membership trend, 1879/1880 to 1974. Membership lists until 1971 (published in
The Canadian Field-Naturalist until the early 1950s and/or reported in published Annual Reports) included all
addressees to which The Canadian Field-Naturalist was sent. After 1971, however, the membership totals exclude
non-voting subscribers and thus are no longer directly comparable to earlier numbers. Where gaps on the membership
data occurred, such as when no lists or Annual Reports were published in some years in the 1920s, an intermediate
estimate was entered.
FiGureE 7. A geological field trip of The Ottawa Field-Naturalists’ Club along a railway rock cut north of Chelsea Grove in the
Gatineau region of Quebec, north of Ottawa. The area’s oldest and youngest deposits are in direct contact here. The trip
leader was Dr. Henry Ami. From Trail & Landscape 13(3): 94; prepared from a lantern slide original by Dr. Ami,
now in the Library and Archives of Canada, Ottawa.
12 THE CANADIAN FIELD-NATURALIST
4879.
OTTAWA
Pe ‘
FIELD- NATURALISTS’ CLUB. |
TRANSACTIONS No. 14.
OTTAWA, CANADA:
CITIZEN PRINTING AND PUBLISHING COMPANY, SPARKS STREET.
1880.
FiGureE 8. The initial issue of The Ottawa Field-Naturalists’
Club Transactions, the initial annual publication series
of The Ottawa Field-Naturalists’ Club.
of the first wave of trained professional biologists to
work in the federal government — were becoming
prominent in the organization, changing things, and
arguing for a more national perspective. This was not
entirely to the liking of at least some of the long-
established Club leadership. The situation must have
had ironic echos for the elders of the Club like Whyte,
Harrington, Small, and Fletcher, for in the days
leading up to the founding of the Club they were the
“young turks” eager for change!
Memorials and the Great War (1900-1915)
Despite the economic trials of much of the late Vic-
torian era, it was a positive period of establishment,
growth and achievement for the OFNC. By the turn of
the 20" century, it had become one of the largest and
most prominent such organizations in Canada. Events
of the next decade and a half would sorely test that
status, however.
Symbolic of the coming of age of the OFNC and
the end of its establishment period was the death of
Vol. 118
Queen Victoria in 1901. The OFNC pioneers, after all,
were either originally emigrants from Great Britain or
were locally-born in colonial times. The black-edge,
memorial issue of The Ottawa Naturalist in February
1901 (Figure 9) expressed in its frontispiece tribute
the heart-felt distress at the passing of an era: “In com-
mon with all the sorrowing subjects of His Imperial
Majesty King Edward the Seventh the members of
The Ottawa Field-Naturalists’ Club desire to record
their deep sense of sorrow and loss at the demise of
their beloved Sovereign Lady, Queen Victoria, during
whose glorious reign of sixty-four years, scientific work
and original research, such as our Club aims to accom-
plish, have received unprecedented impetus”. Quite so!
But Victoria was not the only recent loss mourned
by the Club in the new days of the new century. In the
Victoria Memorial edition, in fact, President Henry
Ami laments the February 1899 “early demise of our
friend and fellow member, the sweet poet of Ottawa,
Archibald Lampman ....[whose] ardent love of Nature
and all she teaches in lake, forest, in autumn, in winter,
in sorrow, in comfort, led him into those numberless
nooks and sequestered spots which enchant the eye,
please the mind and entrance the soul” (Ami 1901).
Just to be sure that the readers not think the Club
had become overwhelmed by anthropocentric concerns,
Ami went on in his address to eulogize a major
scientific personality ... the aforementioned Elkanah
Billings who had played such an important role in
the founding of scientific natural environment investi-
gation in the Ottawa Valley in the first place. Ami
further announced that the Club has commissioned a
portrait of the late Mr. Billings and was donating it to
the Geological Survey Museum (Figure 1).’ Shortly
after Ami’s address, the Council established a com-
mittee to co-ordinate with “different societies affiliated
with the Royal Society of Canada” lobbying of the
federal government for the construction of a National
Museum (LAC OFNC Collection, 13 February 1900).
Was this the genesis of the undertaking which resulted
in the completion and occupation of the magnificent
Victoria Memorial Museum building in 1910-1911?
In any event, the Club officers were clearly aiming for
a balance between the scientific investigation of the
natural environment and the encouragement/enhance-
ment of public awareness of the importance of such
concerns.
A growing OFNC interest in and emphasis on en-
couraging public awareness and appreciation of natural
sciences is shown by the active promotion of involve-
ment by the students and staff of the Ottawa Normal
School (teachers college) during the early years of the
20" century. This was the dawning of “environmental
education” in North America and the Club seemed
enthusiastically involved, particularly through the
school. At least five members of the OFNC Council
worked at the school in this time, including Vice-
Principal S. B. Sinclair. Sinclair served in various Club
2004
capacities during this period, including OFNC 1905-
1906 President (Appendix 1).
Not everyone shared this positive view of environ-
mental education within the Normal School and Ottawa
public schools. A lengthy debate was held amongst
key Club members early in 1905 on the difficulties and
obstacles of this undertaking. In his characteristically
direct way John Macoun declared “it to be his con-
viction that Nature Study would soon be consigned
to the limbo of exploded educational fads” (Attwood
1905). Nonetheless, the Club remained formally in-
volved in such school programs for years thereafter.
OFNC excursions also remained popular public
events, with over 200 people attending each of the
general excursions into the Gatineau Hills in May
and September 1902; tickets were 30¢ for adults, i5¢
for children, including the cost of the day-long, char-
tered train trip (LAC OFNC Collection, 13 May 1902).
Among the participants of the 6 September 1902 ex-
cursion was Normal School Vice-Principal Sinclair
“who was accompanied by about 100 Normal School
students” (LAC OFNC Collection, 6 September 1902).
One might cynically question if all 100 would have
been willing participants in their principal’s venture.
By the early 1900s, however, the Club was not
nearly so involved in original field-oriented research
in the Ottawa Valley as it had been one to two decades
before. There seemed to be a sense that “we pretty
much know it all now” as research reported in the
pages of The Ottawa Naturalist grew increasingly more
national in scope. A greater sense of conservation con-
cern was developing, however, with the first formal
conservation action being initiated when the Council
approved a motion by the Ornithology Committee for
an OFNC petition calling upon the federal government
to promote the preservation of shorebird-breeding wet-
land habitat in the newly established prairie provinces
(LAC OFNC Collection, 7 April 1908). It was a tenta-
tive step (an article in that month’s issue of The
Ottawa Naturalist also provided a prescription for a
“better” Timber Wolf poison [Anonymous 1908}]).
Nonetheless, it initiated a long history of conserva-
tion action and achievement for which the Club has
been widely honoured and of which the Club can be
justifiably proud.
Since its founding, the OFNC had elected a Librarian
and maintained a natural history library. There were
regular reports in Council minutes of titles of the in-
coming scientific literature received in exchange for
The Ottawa Naturalist or as a professional courtesy
to individual OFNC members. By 1904, however, it
was becoming a problem due to the logistical challenge
of housing and caring for the collection in donated
space (LAC OFNC Collection, 15 March 1904). In 1906
the library consisted of “some 350 bound volumes
occupying about 70 feet of shelf space” as well as
many unbound volumes (LAC OFNC Collection, 26
February 1906). The collection seemed to be little
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 13
FEBRUARY, 1901. J
VOL, XIV, No. 11
THE
{| OTTAWA
NATURALIST.
Published by the Ottawa Field-Naturalists’ Club.
CONTENTS.
x. Annual Address of the President of the Ottawa Ficld-
Naturalists’ Club selete BHO eipiate
2. Powers of Adaptation in Fishes, by Professor Edward E.
Prince
m 3. Notes of the Acadian Owl (Nyctala Acadica) in captivity,
by F, Norman Beattie eles steric 4 cows
(ISSUED JANUARY 23,
er anne |
1901.)
OTTAWA, CANADA,
Orraws PRintinG Company (Ltwitep).
3% 5 Moscnrovi Sr.
FiGuRE 9. The Queen Victoria Memorial issue of The Ottawa
Naturalist.
used, however, as the members with significant sci-
entific questions typically had access to the growing
institutional libraries at the Museum or “The Farm”
(as the research centre at the Central Experimental
Farm was — and still is — known). Arrangements were
made in 1909 to move the library into the Ottawa Public
Library where it would be maintained as a stand-alone
collection (LAC OFNC Collection, 22 June 1909). Pre-
dictably, the Ottawa Public Library eventually tired of
the cost and effort of such an arrangement. Faced with
no other realistic options for its maintenance, in 1917
the OFNC donated the collection to the OPL, asking
only that such material be labelled as a Club gift (LAC
OFNC Collection, 8 March 1917).° Curiously, the posi-
tion of OFNC Librarian lasted longer than the library,
being eliminated only in a constitutional change two
years later (LAC OFNC Collection, 15 January 1919).
James Fletcher retired from the Council in the spring
of 1905, after having filled almost every conceivable
position in the Club and working for it in so many
other ways throughout its first quarter century. The
event passed with remarkably little fanfare. Such a
low-key exit for such a pivotal figure was likely Flet-
cher’s own doing, however, as indicated by the very
14 THE CANADIAN FIELD-NATURALIST
different reaction to his sudden and unexpected death
on 8 November 1908.
Although moving along well with an active publi-
cation, excursions, and environmental education pro-
gram, the Club was clearly devastated by the loss of
Fletcher on both an organizational and, for many key
Club people, a personal level. A number of Club
founders and luminaries had died earlier, such as
OFNC 1892-1895 President George Dawson (1849-
1901), but no one personified the enthusiasm, idealism,
and commitment of the Club as did James Fletcher. A
memorial number of The Ottawa Naturalist was pro-
duced in January 1909, reproducing the many insight-
ful and heart-felt tributes delivered by professional
and personal colleagues alike at a special memorial
event held on | December 1908. The presentations of
Club co-founders R. B. Whyte and Will Harrington
were remarkably emotional presentations under such
stiff, proper Edwardian circumstances. Will Harring-
ton’s tribute in particular (Harrington 1909) is quite
capable of tugging heart strings for contemporary
readers a century removed from that time. With the
exception of an unfortunately self-promoting speech
by John Macoun, all contributors that night were clear-
ly bursting to express their appreciation for the man,
for his contribution to the Club and for his contribu-
tion to his chosen country.
Individual Club members were encouraged to con-
tribute to a Fletcher Memorial Fund for the construc-
tion of a memorial drinking fountain to be placed
near Fletcher’s former work site at The Farm. It was
quickly oversubscribed, having accumulated over
$1800 by early 1910 when construction of the memo-
rial began (LAC OFNC Collection, 15 March 1910).
A bronze likeness of Fletcher was created by famous
sculptor (and athletic community associate?) R. Tait
McKenzie and affixed to the fountain. The fountain,
with a descriptive plaque attached, was installed in
1911. It remains along the south side of the NCC
Scenic Drive in the Central Experiment Farm imme-
diately east of the Canada Agriculture Museum.
A memorial painting of James Fletcher was also
commissioned with surplus funds from the Memorial
Fund and hung in the Ottawa Public Library? early the
following spring (LAC OFNC Collection, 12 March
1912). It was officially unveiled by the federal Minis-
ter of Agriculture, Sydney Fisher, who “specially dwelt
on [Fletcher’s] loveable qualities which had endeared
him so much to all who came in contact with him”
(LAC OFNC Collection, 19 March 1912).
It is likely no coincidence that a malaise seemed to
settle over Club affairs in the following years. Few meet-
ings of Council or Club excursions were conducted in
the 1909-1911 period and discussions were held about
reducing the workload associated with The Ottawa
Naturalist, including publishing the journal only quar-
terly.!° The Club operated at a deficit for the first time
in 1910/1911 (LAC OFNC Collection, 21 March 1911).
In late 1911 Editor James Macoun reported that the
Vol. 118
Club could no longer afford to publish monthly (LAC
OFNC Collection, 18 December 1911).
There were calls for — and a dire need of — new
blood in the organization and President Alexander
McNeill suggested establishment of “ ... a junior
branch for the boys. He referred to the success of the
boy scouts but objected to the military spirit associated
with it” (LAC OFNC Collection, 12 March 1912).
Ironic words less than two years before the outbreak
of World War I. Nothing came of this for many years,
however, until the founding of the Macoun Field Club
(see “Post-war Boom (late 1940s-1965)”, below).
The Ottawa Naturalist seemed similarly to be some-
what unfocussed, publishing a relatively large number
of paleontological papers and natural environment
investigations and reports from afar but with the few
local contributions increasingly confined to popular
topics. A review article on the horrors of Poison-ivy
allergic reactions provides an example, reminding
any potentially afflicted reader that “ ... nothing is
better than the old-fashioned lead and opium lotion
...” to relieve the itching (Macnamara 1912).
The notable exception to this was the effort to devel-
op an active environmental protection and bird con-
servation program, led by Gordon Hewitt (1885-1920).
Hewitt was Fletcher’s replacement as Dominion Ento-
mologist (in 1909) and like him, was a dynamic, per-
sonable English immigrant (Criddle 1920). During
his few years in Canada he played an important role
in North American natural sciences and conservation
matters, including being the lead Canadian official in
the development of the 1916 Migratory Birds Con-
vention, before dying at a tragically young age in the
post-war influenza epidemic (Foster 1978). Likely be-
ing assisted by his socially prominent position as the
husband of Prime Minister Bordon’s niece, he suc-
cessfully lobbied both the Ottawa Improvement Com-
mission (forerunner of the National Capital Commis-
sion) and the Boy Scouts of Canada to become in-
volved in enhancement of migratory bird habitat (LAC
OFNC Collection, 17 February 1914). His crushing
load of professional responsibilities, however, limited
the amount of time he was able to put into re-ener-
gizing the Club, even during his tenure as President
in the difficult war-time period of 1918-1919.
As with so many cultural, social, and technical insti-
tutions in Canada, the OFNC was devastated by events
surrounding Canadian involvement in World War I.
On top of their post-Fletcher era struggles, the burden
of war-time logistics, costs, and priorities came close to
destroying the OFNC. The Club ran deficits through
the war years and for the first time in Club history, the
steady rate of membership growth virtually stopped
(Figure 7). A new focus and a new source of energy
were desperately needed. They came in the form of
another recent arrival in Ottawa, this one being a tall,
quiet, bearded architect turned ornithologist from
southwestern Ontario who would turn the OFNC into
a national institution.
2004
A National Role (1918-early 1940s)
Percy Taverner (1875-1947) didn’t think much of
Ottawa or Ottawa naturalists when he arrived in 1911
as the National Museum’s first ornithologist (Cranmer-
Byng 1996). Shortly after arriving he complained to a
Detroit friend, “we have a club here, the Ottawa Nat-
uralists, who are much on a par with the Detroit bunch.
They have nice picnics every week but they are no
place for you and me. The worst of it is that they
have all kinds of direction with good men. Fletcher,
Macoun, Gibson and the whole Geological Survey and
that of the Experimental Farm, but they haven’t evolved
a single naturalist in their twenty-five years of existence.
The only thing they have got is a publication that has a
government grant and appears regularly and in which
we can get publication any time. If not for that, the
real students here would have let the whole organiza-
tion die a natural death long ago”. (LAC Taverner Col-
lection, 29 April 1912).
Taverner’s criticism was brutal and a bit unfair —
but not by much. And to both his eternal credit and
the benefit of Canadian natural sciences, he set about
working with other like-minded rebels to shake the old
outfit up and to make it — or at least, its publication —
better serve the needs and opportunities of the contem-
porary naturalist and public communities. Fletcher,
Martin, Henry B. Small, Whyte, and Harrington would
have been proud.
Like Fletcher before him, Taverner maintained an
extensive network of correspondents across Canada
and the United States. Although allied on the OFNC
Council with the likes of botanist James Macoun, long-
time editor of The Ottawa Naturalist, entomologist
Arthur Gibson (1875-1959), and herpetologist Clyde
Patch (1887-1952), Taverner was inspired by his field-
naturalist colleagues across the country to broaden
the reach of the Club’s publication. Early in 1918 he
argued to the Council that “... it does not seem pos-
sible to support a worthy publication in a purely local
field. Any such endeavours to be successful must en-
large its field. I therefore suggest that the pure local
character of the periodical be removed by a change
of name and propose The Field Naturalist” (LAC
OFNC Collection, 26 March 1918).
Taverner, Macoun, and associates made the skepti-
cal Council an offer they could not refuse. They prom-
ised it would mean no substantive change for local
naturalists and would still accommodate more popu-
lar general public issues. Most importantly, they per-
sonally guaranteed to underwrite a huge expansion in
membership in order to establish a secure, long-term
financial base for the program. James Macoun, for ex-
ample, immediately pledged to underwrite 100 new
memberships; Taverner, Patch and anthropologist F.
W. Waugh each took on 25 and archaeologist W. J.
Wintemberg accepted responsibility for a further 15
(LAC OFNC Collection, 1 May 1918; 17 March 1919).
How could the Council refuse such an offer?
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 15
Vor. XXXII, No. 1. APRIL, 1916.
aS
|
second ebzss malice.
FiGure 10. An issue of the last volume of The Ottawa Nat-
uralist in 1918.
Taverner described the manoeuver to his mentor J.
H. Fleming in August 1918 as something of a coup,
“ .. a few of us got in control and overrode the con-
servatives ... ” (Cranmer-Byng 1986). He went on in
the Fleming letter to say, “we hope to make it the sci-
entific and nature study periodical of Canada” (LAC
Taverner Collection, 10 August 1918). And indeed,
by the following spring the mailing list had virtually
doubled to over 540 names (LAC OFNC Collection,
17 March 1919). Taverner reported back to a skepti-
cal Fleming in Toronto that “you are mistaken in
believing that the change in name will not help The
Ottawa Naturalist. It has helped already. The change
in form can only be supported by increased subscrip-
tions and we have to rely mostly on Canadians for this.
The jealousy of anything labeled Ottawa throughout
Canada is surprising” (LAC Taverner Collection, 10
April 1919).
The Canadian Field-Naturalist (CEN) was officially
established by a motion from James Macoun (sec-
onded by Taverner) at the OFNC Annual Meeting in
March 1919. A change had already been made in April
1918 with a larger format and better paper (Figure 10),
16 THE CANADIAN FIELD-NATURALIST
graced by the attractive, if pastoral, cover illustration
provided by Geological Survey of Canada artist C. E.
Johnson. The new journal name was first used on the
April 1919 issue. This cover illustration remained on
each regular issue of the CFN until volume 59 (1945)
when, without further explanation, it was removed in
favour of the Table of Contents (LAC OFNC Collec-
tion, 3 March 1945).
The care and maintenance of the CFN became the
primary issue and function of the Club. The under-
writing of new subscriptions by the small group of
‘friends’ of the journal had a dramatic effect on mem-
bership numbers, the new levels of which persisted
through the 1920s (Figure 6). This laid a strong, nation-
al foundation for the publication without which it seems
unlikely the publication (and the OFNC) would have
survived the dark days of the 1930s.
Another major publication initiative in that period
was the first OFNC Special Publication, occasioned
by the death of John Macoun. Upon the urging of his
son, horticulturist and OFNC 1903-1905 President
William T. Macoun (1869-1933), the Council agreed
to publish the elder Macoun’s autobiography (LAC
OFNC Collection, 9 April 1921). Curiously, not since
the Ottawa Natural History Society produced its occa-
sional Transactions more than 50 years earlier had
such a stand-alone publication been presented by the
Ottawa naturalist community.
While a Memorial Fund was established to cover
the $2500 costs of publication of the Macoun autobi-
ography as well as a memorial portrait (again as with
James Fletcher’s portrait, created by Franklin Brown-
ell), it apparently fell to William Macoun to make
most arrangements (LAC OFNC Collection, 9 April
1921). This he did enthusiastically and efficiently, lead-
ing to an initial run of 2000 copies of the autobiog-
raphy (Macoun 1922). Indeed, after the book was pub-
lished, the 1922 OFNC Annual Report was deliberately
altered to read that “the Club had co-operated with Mr.
W. T. Macoun in the publication of the Autobiography
of Professor John Macoun” (LAC OFNC Collection,
5 December 1922), suggesting that the Club may not
have played much of a role in its development."!
The Macoun portrait was formally presented to Na-
tional Museum of Canada Director William McInnis
during the 1921 OFNC Annual Meeting which was
held in the Victoria Memorial Museum, Macoun’s last
work place in Ottawa. It was accompanied by various
speeches praising his extraordinary contributions to
Canadian natural science (LAC OFNC Collection, 20
December 1921).
Other occasional publications appeared as Special
Issues of the CFN through the 1920s. One was a treat-
ment of the birds of Saskatchewan which included the
first colour illustration to appear in the journal (Mitch-
ell 1924) and another was a long essay on the natural
resource potential of northern Canada (Kindle 1928),
Vol. 118
copiously illustrated by high quality black-and-white
and half-tone plates. The latter, by paleontologist and
OFNC 1927-1928 President E. M. Kindle (1869-1940),
who had recently won a $1000 prize in a Canada-wide
competition established by Sir William Price for the
best article on this subject. This pattern of occasional
Special Issues for larger, particularly significant or
appropriate subjects has continued to the present day,
recent subjects including the Taverner biography
(Cranmer-Byng 1996) and a review of the orchid spe-
cies of the Ottawa District (Reddoch and Reddoch
1997). Earlier long articles, like Fletcher’s Flora
Ottawaensis (Boivin and Cody 1955) or Hoyes Lloyd’s
review of the birds of Ottawa (Lloyd 1923; 1924),
were often serialized over a number of issues.
Another special publication was called for in the
1920s. It was recommended to the Council by Geo-
logical Survey of Canada geologist J. B. Mawdsley
that the Club produce “ ... a local scientific guide book
of the region” (LAC OFNC Collection, 20 November
1929). The OFNC was indeed instrumental in seeing
such a naturalist’s guide produced, but that did not
happen until nearly 60 years later (Brunton 1988).
Local programming became little more than occa-
sional field outings and lectures during the late teens
and 1920s, although efforts were made to get the Boy
Scouts organization more involved during the early
1920s (LAC OFNC Collection, 26 March 1921).
Nonetheless, Taverner’s earlier unflattering portrayal
of the Club’s activity level was still more or less on
target a decade later. This apparent lack of new energy
and focus in the post-war years and early days of the
Roaring Twenties was underscored by the deaths of a
number of prominent OFNC pioneers and activists,
men who had emphasized the need for and impor-
tance of local field activity. These included founders
R. B. Whyte (1919) and Will Harrington (1918), as
well as Gordon Hewitt (1920), James Macoun (1920),
and John Macoun (1920).
National conservation issues, typically relating to
the protection of particular animal populations, con-
stituted the major non-publications subject of discus-
sion of the Council in the 1920s and 1930s. On a num-
ber of occasions the Council passed motions for the
Club to petition the federal government regarding such
issues as improved national museum support or the
protection of wildlife. This may have been awkward at
times, since many of the people receiving and dealing
with such pleas or critiques were Club members or
professional associates of Club members. Senior gov-
ernment eyebrows may have been raised, for instance,
when Editor Harrison Lewis (1893-1974) published a
(prescient!) editorial in the CFN that was highly criti-
cal of apparent governmental support for increased
commercialization of Canadian national parks (Lewis
1922). It has never been, after all, particularly judi-
cious for active civil servants to publicly question
2004
stated government policies or intentions. “Awkward”,
however, does not adequately describe the “Buffalo
Crisis” of 1925.
The trouble arose when the Council directed that a
letter be sent to the Department of the Interior protest-
ing the proposed movement of Plains Bison of ques-
tionable health into the disease-free range of the last
known herd of Wood Bison (LAC OFNC Collection,
28 February 1925). The protest letter was signed by
OFNC President Hoyes Lloyd (1888-1978) and accom-
panied by a comparably critical Letter to the Editor
which had recently been published in The Canadian
Field-Naturalist (Harper 1925). Lloyd and the CFN
Editor Harrison Lewis, however, were both employees
of the Department of the Interior and their public crit-
icism of their professional superiors was clearly not
appreciated. Instructed to choose between continued
federal government employment and their OFNC
positions, both Lloyd and Lewis had little choice but
to resign their Club positions immediately — to the
apparent surprise and regret of the Council (LAC
OFNC Collection, 11 April 1925). Lloyd became the
first and only OFNC President forced to resign in mid-
term, although he served the Club in many ways for
decades thereafter and was awarded an Honorary Mem-
bership in 1965 in recognition of his contributions
(Munro 1979). Curiously, the taking of this laudable,
if perhaps somewhat naive position of principle, was
publicly unreported until 2002. It is not even hinted
at in The Canadian Field-Naturalist obituaries of either
gentleman (Solman 1974; Munro 1979). Lewis, Lloyd,
Harper and associates have been proven correct in their
concerns regarding herd contamination, as the issue of
appropriate Wood Bison population management in
Wood Buffalo National Park is once again being hot-
ly debated (Fuller 2002).
On a more positive note, the 50“ anniversary of
the OFNC was celebrated with an anniversary dinner
on 19 March 1929 (erroneously believed to be the
founding date — see “Founding Meeting”, above), in
which two of the few surviving founders (H. B. Small
Jr. and Roger Davy) were the guests of honour. Other
founders (participants in the 25 March 1879 found-
ing meeting) still alive in March 1929 were L. H.
Chrysler, W. Chesterton, and P. B. Symes (who died
later that year).!* The Club was doing reasonably well
in early 1929, however, with a substantial surplus and
a stable, adequate number of members to support its
programs. If local activities were not undertaken at
anything like the keen levels of years and decades
before, the publication program seemed solidly and
comfortably established and seemed to have achieved
the national scope that Taverner, James Macoun, Lewis,
and their associates had worked so hard a decade ear-
lier to achieve.
The respite from difficult times was short-lived,
however, as the Great Depression of the 1930s pre-
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 17
sented another severe test of the Club’s staying power
and its officers’ mettle. Stripped down to basic func-
tions — publishing the CFN and little else — the Club
was enduring especially tough times, ushered in by
dramatically falling membership in 1930 and a sub-
stantial budget deficit. There was a $728 swing in net
revenues from the surplus of the previous year (LAC
OFNC Collection, 11 April 1930). Membership would
not again exceed the 1929 total of 549 until 1955 (
6).
By the December 1932 Annual Meeting the OFNC
was operating at a 20% deficit — and this only after
drawing upon the Club’s small Reserve Fund and
securing a 12% reduction in charges from the CFN
printer. The good news, though, was that excursion
attendance was way up, with four spring field trips
each averaging over 100 attendees. OFNC 1931-1933
President Charles Sternberg (1885-1981) concluded
cheerfully “we feel our organization has stood up as
well as others in the stormy times and we are, as a
Club, now looking forward and ready to face brighter
days as they dawn upon us” (LAC OFNC Collection,
6 December 1932).
It was not to be, of course. The Club officers were
creative and flexible in finding ways of keeping things
going despite the depletion of the Reserve Funds and
low membership numbers. They agreed, for instance,
to carry the 1934 membership of anyone who had been
with the Club for five years but could not afford the
$2.00 membership/subscription fee (LAC OFNC Col-
lection, 9 January 1934). Local excursions were em-
phasized again (e.g., 10 were held in 1935) and while
these did not appear to generate much in the way of
new biodiversity information, they did offer a benefit
and encouragement to local members. A re-emphasis
on conservation matters was also expressed, especially
by those working in National Parks and in federal
migratory bird conservation offices, but no particular
hands-on local initiatives were identified. The Council
even decided to defer joining the newly established
Federation of Ontario Naturalists which was dedicated
to the objective of protecting natural areas and “native
wildlife” (biodiversity) in Ontario (LAC OFNC Col-
lection, 7 May 1936).
Despite the difficult times and reduced level of local
activity, the 1936 Annual Business Meeting drew over
100 members, likely due to the attendance of Archie
Belaney, a.k.a. Grey Owl (Dickson 1973) “... Canada’s
famous Indian naturalist and conservationist who
spoke briefly on the need for immediate conservation
action in Canada” (LAC OFNC Collection, 1 Decem-
ber 1936).
What sustained the OFNC through all the ups and
downs of this difficult time was the special relation-
ship of the Club with the community of biologists
and scientists employed by the federal government,
especially with those at The Museum (Geological
18 THE CANADIAN FIELD-NATURALIST
Survey of Canada Museum, then National Museum
of Canada, now Canadian Museum of Nature) and
The Farm (Central Experimental Farm, now various
research initiatives within Agriculture Canada). Hall
(1986) notes that over 30 employees of The Farm —
the most notable being James Fletcher — served as
officers, editors, and/or Honorary Members of the
OFNC (Appendix 1). Twelve of those individuals had
been OFNC presidents. A comparable or possibly even
stronger commitment could be documented from The
Museum, with Department of the Interior (Canadian
Wildlife Service (CWS) and Parks Canada) personnel
making a similarly important contribution to the opera-
tion and support of the OFNC. These people saw the
Club in general and the CFN in particular as an im-
portant contribution to Canadian and North American
natural sciences and to the conservation of the natur-
al environment. They saw it (as many in such positions
still do) as virtually their duty to participate. In an
otherwise mundane 1937 debate on the question of
possible reduction in the honorarium given to the CFN
editor (from the princely of $90 established in 1928,
to $50) as yet another cost-cutting measure, Harrison
Lewis stated “... we are a scientific society and any
one of us would carry on the work without salary for
the good of the Club”, to which Percy Taverner
added ” ... the Editor works for the good of his
science and not for wages ...”. The motion for a
reduction in the editor’s honorarium passed, by the
way (LAC OFNC Collection, 10 April 1937), and was
not increased again until 1947 (LAC OFNC Collec-
tion, 25 January 1947).
There remained a small group of Club officers
throughout the 1930s and early 1940s who argued for
more emphasis on a strong local program of lectures,
excursions, and public education. This group was led
by irrepressible biology teacher and priest F. E, Banim
(1902-1979), statistician W. H. Lanceley (1893-1958),
and technical editor Pauline Snure. These Club offi-
cials, also supported by botanist and OFNC 1935-1937
President Herb Groh (1883-1971), argued for the re-
establishment of monthly lectures and a return to old
time soirées as means of generating renewed interest
and membership in the Club. They were successful in
the establishment of a Flora and Fauna Committee to
co-ordinate a renewal in the investigation and docu-
mentation of local biodiversity (LAC OFNC Collec-
tion, 28 October 1936). This latter committee ultimate-
ly had few results, although J. R. Dymond, selected as
leader of the fish working group, presumably conduct-
ed at least a part the research which was the basis for
his later The Fishes of the Ottawa region (Dymond 1939)
in response to this initiative.
Snure was particularly forceful in the mid-1940s
in taking on long-established, senior Council members
like Hoyes Lloyd and, to a lesser extent, Harrison
Lewis and Percy Taverner, and pushing successfully
for such things as the establishment of an Excursions
and Lectures Committee to co-ordinate services for
Vol. 118
local members (LAC OFNC Collection, 22 January
1944). The latter three — now old guard members —
were the most vocal on Council in arguing for contin-
ued priority being placed on the important “national
publication society” elements they had worked so
hard to sustain through the difficult 1930s and into
the early 1940s. Although their efforts only slowly
bore fruit, Banim, Lanceley, and Snure (who served
consecutively as OFNC President between 1944 and
1950)!°, were able to shepherd a measure of renewal
of local naturalist activities in this period.
The at-times conflicting perspectives of local natur-
alist club and national scientific publication society
simmered along, unresolved as national and world
events (the latter years of the Great Depression, the
commencement of World War II) effectively limited
the ability of the Club to generate substantial new
membership or financial resources. Despite the war-
time limitation on materials and human resources,
some Club local field investigations were initiated
and the CFN continued to appear, albeit with many
issues in 1941 and 1942 delayed by the printer’s war
work priorities. Not oblivious to patriotic opportuni-
ties themselves, in 1942 the Council responded to a
request for the exchange of scientific literature from
the Lenin Library in Moscow by offering a free set of
The CFN from 1935 “until the close of hostilities ...
as a mark of our good will” (LAC OFNC Collection,
5 October 1942). For OFNC functions and programs,
the World War II period was essentially an extension of
the publications and membership subsistence efforts
of the 1930s. Only as the war in Europe was winding
down did the first signs of renewal and new potentials
— such as increased membership — begin to appear
(LAC OFNC Collection, 5 December 1944).
Post-war Boom (late 1940s-1965)
One of the first signs of the rebirth of local area
activity within the OFNC came with publication of
review articles on the birds and mammals of the
Ottawa District in the latter years of World War II
(Lloyd 1944 and Rand 1945, respectively), at least in
part at the urging of local naturalist advocates like
Banim, Snure and Lanceley. Although based largely on
historic Museum data and/or the authors’ observations,
these review papers gave local naturalists the first com-
prehensive treatments of popular Ottawa District flora
or fauna since Fletcher’s 19" century vascular plant
list (Fletcher 1888) and Lloyd’s bird list from the
1920s (Lloyd 1923; 1924).
Almost coincident with, but much more important
than this, was the tremendous post-war growth in the
professional civil service in response to the needs of
an expanding, prosperous post-war national economy.
A new wave of young, energetic, natural scientists
from all across Canada was arriving in Ottawa in the
late 1940s and early 1950s, many soon joining and be-
coming involved with the programs and workings of
the OFNC. Following the dark days of the Depression
2004
and then the war, many of these individuals were keen
to contribute both to the improvement of their recover-
ing local and national communities and to the explor-
ation and protection of Canadian natural biodiversity.
In November 1946, for example, future Honorary
members and important Club contributors Clarence
Frankton (1906-2000) (Brunton 2003) and Jack Gillett
joined the Club, followed the next month by long-time
Business Manager of the CFN and future Honorary
Member Bill Cody. Indeed, almost 150 new members
joined the OFNC in 1948 alone (Snure 1978). Newly
arrived natural science specialists were pressed by
their OFNC veteran associates to join the Club; in-
volvement in Club programs was almost an expected
part of the job in those years (C. Frankton, personal
communication).
This new wave of naturalists demonstrated some-
thing not seen since the early years of the Club’s his-
tory — a keen enthusiasm for field exploration and
discovery, and a desire to share that new-found know-
ledge with the naturalist community and the general
public. Accordingly, the late 1940s and early 1950s
were productive years for the documentation of Ottawa
area biodiversity, as indicated by the richness of the
specimen records from that time in the collections of
The Museum and The Farm (personal observation).
Another major initiative of this period was the
formation of the Macoun Field Club (MFC), a junior
naturalists club sponsored jointly by the OFNC and
the National Museum of Canada (Snure 1978; Baldwin
1978). Such an organization had been talked about
since before the First World War, but nothing had
come of it. Due to dedicated work by a large number of
Club and Museum people, however, it was success-
fully established in 1948. The first MFC Committee
Chairman was OFNC 1954-1955 President W. K. W.
(Bill) Baldwin (1910-1979) (Figure 11) who set the
initial tone and procedures which have stood up ever
since (Soper and Bousfield 1982; Francis Cook, per-
sonal communication). The MFC has supported and
encouraged the investigation and documentation of nat-
ural biodiversity by elementary and secondary school
children in the Ottawa area through a remarkably rich
program of lectures, workshops and most importantly,
field studies, for over 50 years (Lee 1998). The work of
Bill, Herb Groh (Figure 12) and David Maddox was
particularly critical to this success in the formative years
of the MFC. Many OFNC club members contributed
time and even, in the case of Mary Stuart, access to their
property for field trips (Figure 13).
The OFNC also undertook to generate greater pub-
lic awareness of natural environment matters and to
develop an additional stream of funding for the Club
by arranging local sponsorship of Audubon Screen
Tour presentations in Ottawa. These were profession-
ally produced and well-attended illustrated lectures
by speakers of the calibre of Roger T. Peterson and
George M. Sutton (personal observation). They pro-
vided an important source of general public education
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 19
on a wide range of natural environment topics in the
days before specialty television channels or, indeed,
television of any kind was available for most Ottawa
households. It’s not entirely clear who was the Club’s
lead on this program; Humphreys (1979a) suggests it
resulted from Oliver Hewitt’s circulation of an Audu-
bon Screen Tour brochure in December 1947. The rec-
ords of the minutes books, however, state that former
Treasurer and future Honorary Member Ibra Connors
(1894-1989) brought the issue before the Council for
approval later that winter (LAC OFNC Collection, 21
February 1948). Regardless, until it was cancelled in
1959, the Audubon Screen Tours program was enjoyed
by many thousands of Ottawans and generated con-
siderable revenue for the Club (Humphreys 197%a).
A significant amount of Club revenue also resulted
from the clearance of a mass of The CFN back issue
orders which had built up during the 1941-1955 edi-
torship of Harold Senn (1912-1997). Bill Cody and
Clarrie Frankton spent weeks ferreting out and follow-
ing up on years-old orders for The CFN back issues
(C. Frankton, personal communications). The resulting
revenue formed the seed funding which has grown into
what now constitute very substantial OFNC reserve
funds.
In the late 1940s and for the first time in OFNC
history, the Club had its own field station. In 1949 A.
E. (Fred) Bourguignon (1893-1968) arranged for a
10-year lease of a property at Beatty Point along the
Ottawa River off what is now Grandview Road in
Nepean. For a cost of $300 (assisted by a substantial
donation of building materials), various Club members
(most particularly, Fred Bourguignon) worked to
construct a small wooden building which would serve
as a base for OFNC field studies in the area. Beatty
Point Lodge, as it was called, was officially opened
on 24 May 1949 and served as a field investigation
centre for almost 10 years. Encroaching urban growth,
expanding road networks, and the proliferation of per-
sonal automobiles eventually made a single base of
operations less useful for contemporary field explor-
ations and the building was sold in the late 1950s
(Humphreys 1979b).
Some members in the early 1950s wished to delve
more deeply into particularly popular natural history
subject areas in the Ottawa District. From this interest
arose informal study groups such as the Fern Group,
the Bog Group, the Trail Group, the Bird Group, etc.
(Dill 1979; 1982), and later, the Native Orchid Loca-
tion Survey. Consistent with the science-based approach
of OFNC field investigation throughout its history,
these study group participants did more than just ex-
plore interesting natural landscapes and share identi-
fication information amongst themselves. They docu-
mented significant findings in writing and/or with spec-
imens. The records of the Fern Group, for example,
were heavily relied upon for the production of a
treatment of the ferns of the Ottawa District (Cody
1956). The Native Orchid Location Survey was estab-
20 THE CANADIAN FIELD-NATURALIST Vol. 118
Ficure 11. Bill Baldwin, botanist at the National Museum of Canada and the first chair of the Macoun Field Club, at the meet-
ing room provided by co-sponsor National Museum of Canada in the basement of the Victoria Memorial Museum
Building together with early members Cynthia Millman and Nancy Fergusson, November 1950 (Macoun Club files,
courtesy of Rob Lee).
FiGurE 12. Herb Groh, then just retired weed specialist at the Canada Department of Agriculture and a Past President of The
Ottawa Field-Naturalists’ Club, with Macoun Field Club member Nick Wickenden, November 1950. (Macoun Club
files, courtesy of Rob Lee).
2004
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB aM
FiGurE 13. One of many Macoun Field Club trips to OFNC Honorary Member and long-time Macoun volunteer Mary
Stuart’s property near Packenham: Intermediate and junior groups, March 1969. Photograph courtesy of Rob Lee.
lished by E. W. Greenwood in 1966 and soon grew in
scope beyond the Ottawa District, gathering a consid-
erable body of orchid location data from volunteer
contributors across Canada until the mid-1970s (Red-
doch and Reddoch 1997).
With local natural history activities reaching levels
not seen since the early days of the century, OFNC
members felt the need for more timely and topical
information through a forum which would help to
“tie the members together” (LAC OFNC Collection,
28 February 1949). Appropriately enough, that initia-
tive was approved by the Council at the same meeting
authorizing the construction of the Beatty Point Lodge,
underscoring the new-found enthusiasm for local activ-
ity. The first issue of the Ottawa Field-Naturalists’
Club Newsletter was published in April 1949 under
the editorship of Verna (Ross) McGiffin. It ran until
1967, providing timely notices of meetings and events
and offering a forum for the speedy exchange of in-
formation and opinions on a wide variety of issues of
interest to the local membership.
The Club reached its 75" Anniversary in 1954,
though due to program delays, the occasion was actu-
ally celebrated in 1955 (Dill 1979). It was much more
of a party affair than the low-key Founders’ Tea and
Club dinner held for the 50" anniversary back in 1929.
The Club was profiled in the print media and a local
department store provided a display window for an
exhibit on the Club. The attention paid to the event
generated the first formal demonstration of historical
interest in the organization. Herb Groh, whose OFNC
involvement dated back to the pioneer days of the
Club and who had worked with both John Macoun
and James Fletcher (Taschereau 1972), provided an
anecdotal history of Club Presidents (Groh 1955).
After all, he’d known almost all of them! Although
some historical documentation of technical matters
pertaining to the CFN’s publication history had been
produced (LaRocque 1931; Boivin and Cody 1955),
this was the first public documentation of the person-
alities and events that had highlighted the Club’s
history.'*
The CFN produced increasingly larger issues
through this period, reflecting the greater volume and
quality of original field work being conducted both
locally and farther afield in the early to mid-1950s.
This increased production, however, posed financial
problems as publication costs increased 400% from
the mid-1940s to 1953; Club income not quite dou-
bled in the same period. Since it was felt that mem-
bership fees ($2.00) were as high as could be sustained,
costs had to be reduced. Accordingly, after decades
22 THE CANADIAN FIELD-NATURALIST
TRAIL, &
wi ye
A PUBLICATION CONCERNED WITH
NATURAL HISTORY AND CONSERVATION
TRAIL & LANDSCAPE Vol.1.No.1 p. 1-28 Ottawa, March-April, 1967
FiGure 14. The first issue of Trail & Landscape, March-April
1967, a journal for regional observations and outings
and Club events. The cover was designed by the first
editor, Anne Hanes.
of debate on the matter, the journal was reduced to
quarterly publication (from six issues per year) ef-
fective with volume 67 (1953) (LAC OFNC Collection,
20 November 1952). Publication production problems
were seriously exacerbated by lengthy delays in getting
into press, leading Publications Chairman and OFNC
1950-1952 President Walton Groves (1906-1970) to
“express his deep regret at his inability to command
the support and co-operation” of just retired editor
Harold Senn (who had served 13 % years) in order to
pass on the editorship to incoming editor R. A. Ham-
ilton (LAC OFNC Collection, 4 May 1956). By the
end of 1956 the last issue of the 1955 volume had still
not been produced. The Council decided not to pay out
the editor’s honorarium for that year until the volume
was completed (LAC OFNC Collection, 13 December
1956). The crisis was resolved by a flurry of publica-
tion activity under the efficient new editor, however,
with seven issues being published between February
and September 1957 (LAC OFNC Collection, 30
September 1957)!'>
The Club continued to struggle financially despite
the generally rosy economic picture in the country, as
it also had, ironically, during the “Roaring Twenties”.
Vol. 118
In the mid-1950s, for example, Treasurer R. J. Moore
advised the Council “to go easy, especially keep
Excursions & Lectures Committee under control”
(LAC OFNC Collection, 29 February 1956). Walton
Groves’ assessment was even more brutal, stating that
“many of the Club’s activities have been crippled by
the delay in publication” and by the need to publish
sO many issues in such a short time (LAC OFNC
Collection, 30 September 1956). Despite the return to
timely publication of the CFN, at the end of the decade
Groves still reported that “the financial position of
the Club continues to be very grave” at (LAC OFNC
Collection, 1 December 1960).
Still, the OFNC managed a Special Issue of The
CEN, Alice Wilson’s Geology of Ottawa (Wilson
1956). It was likely only possible because Carleton
University placed a pre-publication order for 1000
reprints (LAC OFNC Collection, 13 April 1956).
Before environmental conservation and the protec-
tion of natural biodiversity became major social and
cultural phenomena in the Western World in the 1960s,
the locally-focused elements within the OFNC had
been gradually increasing the organization’s level of
involvement in such directions. In the early 1950s,
for example, Harrison Lewis met with the Federal
District Commission (FDC) to discuss how the OFNC
could (and would) provide wildlife protection and
enhancement consultation during Gatineau Park dev-
elopment. They also explored the idea of an OFNC
field station space being provided in an expropriated
Gatineau Park building (LAC OFNC Collection, 7
April 1951). An ORNC Gatineau Park Committee was
formed under the chairmanship of OFNC 1960-1961
President Winston Mair and made various recom-
mendations for wildlife habitat enhancement there.
The Federal District Commission also asked the Club
to be involved in the establishment of a Brewery Creek
bird sanctuary in Hull (Gatineau), presumably in res-
ponse to the high profile that site had received from
former British High Commissioner Malcolm Mac-
Donald’s war time reminiscences in Birds of Brewery
Creek (MacDonald 1947) (LAC OFNC Collection,
13 March 1952). Nothing came of that and neither
FDC consultation was mentioned again after 1954
(LAC OFNC Collection, 15 December 1954).
Conservation priorities (late 1960s-early 1980s)
A forerunner of the OFNC Conservation Commit-
tee, called the Preservation of Natural History Sites
Committee, was established in 1960 with Bill Baldwin
as its chair and with locally-active members including
biology professor Donald A. Smith, CWS biologist
Vic Solman, geologist D. D. Hogarth and botanist W.
G. Dore (1912-1996) (LAC OFNC Collection, 15
December 1960). One of its first ventures — opposing
the proposed destruction of the vast Mer Bleue peat-
land in eastern Ottawa (it was to be used as a regional
landfill!) — was highly successful. It led not only to
2004
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 23
FIGURE 15. Members of the Traill Group near Pinks Lake 29. May 1965, one of the last outings before disbanding as a
formal group. From left to right are Winifred Anderson, Ruth Resenel, Alice Frith, Sheila Thomson, Bill Thomson,
Rowley Frith, Hue McKenzie, Elva MacKenzie, Anne Hanes and unknown. Photograph by Charlotte Dill. Trail &
Landscape 16(2): 95 [1982].
protection of that magnificent natural area, but also
to a series of ecological and biodiversity investigations
of the wetland (Baldwin and Mosquin 1969). Donald
Smith played a pivotal role in generating the neces-
sary awareness amongst both the naturalist commu-
nity and National Capital Commission (NCC) officials
of the significance of the bog (Dorais et al. 1974).
The protected area — now some 3 500 ha in size — is
managed by the NCC for the benefit of its ecological
functions and has been declared an internationally
significant wetland under the Ramsar Convention on
Wetlands (National Capital Commission 1996).
In this period local Club members and the general
public benefitted from two birding columns in Ottawa
newspapers, one in The Ottawa Citizen by Wilfred
Bell and the other in The Ottawa Journal by the ap-
propriately named John Bird. The latter weekly column,
“Bird’s-eye View”, was particularly beautifully written,
accurate and insightful. It emphasized the growing
level of birding activity in the Ottawa Valley and
offered a timely (unofficial) bulletin board of OFNC
and conservation events (McNicholl 1994).
Certainly the most important single occurrence for
the local Club element in this period was the estab-
lishment of Trail & Landscape (T&L) (Figure 14).
As expressed by the then CFN editor Theodore Mos-
quin, it was to be “a newsletter as well as contain[ing]
articles of wide appeal in the conservation field” (LAC
OFNC Collection, 5 January 1967). The existing OFNC
Newsletter wasn’t offering sufficiently comprehensive
local coverage, nor could it satisfactorily accommodate
the documentation of local conservation-oriented nat-
ural environment investigations which were increas-
ingly being undertaken by Club members. T&L was
an immediate and astonishing hit, not only satisfying
a need of active local Club members but generating a
huge, unprecedented increase in membership (Figure
6). Anne Hanes (1925-1981) was appointed as the first
editor and exercised these duties superbly through 13
volumes (1967 to 1979), always encouraging environ-
mental conservation themes wherever possible (Green-
wood 1980).
Two subsequent editors, Joyce Reddoch (from 1980
to 1989) and Fenja Brodo (from 1991 to 1992 and 1993
to 2001) expertly supervised and directed the develop-
ment of long runs of the publication. Reddoch’s term
was distinguished by the production of a number of
large review articles which she solicited for both their
intrinsic natural history value and their importance as
reliable references for various conservation applications
thereafter. A number of these, such as the reviews of
Ottawa District amphibian and reptile species (Cook
24 THE CANADIAN FIELD-NATURALIST
1981, a revision of an earlier series in 1967 solicited by
first editor Anne Hanes) and butterfly species (Layberry
et al. 1982), continue to be locally referenced, as do
all of the natural areas documentation published in
T&L. The Club and its members have also been well
served by other editors of Trail & Landscape, Elizabeth
Morton (1990), Bill Gummer (from 1992 to 1993) and
Karen McLachlan/Hamilton (from 2001 to the present).
Trail & Landscape quickly became the contempo-
rary source for information on local natural environ-
ment issues. It has provided an ideal bridge between
the recording of natural environment information for
its own sake and in directing and assessing conserva-
tion priorities (Brunton 1986b). To some, the timeliness
and thus effectiveness appears to have suffered, how-
ever, after a decision to reduce the publication sched-
ule, for manpower and economic reasons, from five
issues/year to four, starting with the 1988 volume.
The subsequently reduced publication frequency and
fewer total pages have coincided with a substantial
reduction (by almost half) in the number of articles
with direct conservation applications.
The huge increase in membership and higher profile
of conservation and field-oriented activities in the late
1960s may have set too hectic a pace for some long-
time Club stalwarts who had been more concerned with
the national publication role. Hoyes Lloyd resigned
from the Council at the end of 1967, stating that he
felt it inappropriate as an OFNC Honorary Member
to also serve as a Club director (LAC OFNC Collec-
tion, 6 June 1967). There is no such limitation on Hon-
orary Members, however, and a number have contin-
ued to serve on Council with distinction for many years.
Notable in this regard is 1979 Honorary Member Bill
Cody, who has served continuously on Council since
December 1947, shortly after becoming The CFN
Business Manager earlier that year (LAC OFNC Col-
lection, 21 May 1947). And similarly impressive is the
contribution of Frank Pope, who has served on Council
continuously since 1980 and has occupied the positions
of Corresponding Secretary (three years), Treasurer
(six years), Vice-President (one year) and President
(an unprecedented six years) (Appendix 1).
The Canadian Field-Naturalist underwent a signif-
icant reconfiguration in January 1970, introducing a
new size, format and appearance not just to improve
its look but “to [make] its content as relevant as pos-
sible to the natural history needs of our time” (Mosquin
1970). And by “relevant”, Editor Ted Mosquin meant
strongly conservation oriented. That first issue was
graced by a photo with a Timber Wolf — the contem-
porary symbol of wilderness protection — crossing a
snowy landscape. The issue contained both a variety
of articles on Canadian endangered species and a direc-
tory of conservation organizations in Canada. Conser-
vation applications of carefully-researched ecological
and natural diversity investigations have been a hall-
mark of The CEFN ever since.
Vol. 118
Both as OFNC 1969-1971 President and editor of
the CFN from 1967 to 1972, Mosquin was at the fore-
front of efforts to enhance the level of OFNC conser-
vation action and to engage both the membership and
the general public in this. OFNC 1971-1972 President
Sheila Thomson and OFNC 1972-1975 President
Irwin Brodo were similarly motivated conservation
voices in the OFNC, the three of them working togeth-
er to persuasively direct Club environmental protection
initiatives. Mosquin initiated a series of at times hard-
hitting and at times controversial editorials (not the
last we were to see in the CFN!), challenging Club
members, the larger naturalist community, and public
decision-makers to be more effective in protecting
natural environments in Canada. In 1972 he resigned
the CFN editorship to take on the challenge of found-
ing editor of the Canadian Nature Federation’s Nature
Canada.
The infectious enthusiasm, environmental passion
and unquestioned technical expertise of these three
activists in concert with other Club leaders of the day
such as OFNC 1963-1966 President George McGee
(1909-1991) and OFNC 1967-1969 President Hue
McKenzie, were an inspiration to a whole generation
of new Ottawa-area naturalists (personal observation).
For us newcomers, they transformed the understand-
ing of the study of the natural environment from a
seemingly slightly idiosyncratic, individual endeavour
undertaken for personal entertainment to a meaning-
ful — even important — and highly integrated calling.
What a revelation!
The growing commitment to natural environment
conservation in the late 1960s and early 1970s saw
the re-energizing of OFNC Council and membership
support in this area. At the urging of Ted Mosquin and
Ed Greenwood and recognizing that the Preservation
of Natural History Sites Committee was not broad
enough in its mandate, in early 1967 the OFNC estab-
lished the Natural Areas Committee to coordinate
original field conservation research and to actively
search out potential natural reserve sites in the Ottawa
Valley (LAC OFNC Collection, 10 April 1967). By
1970, the committee was undertaking a broad program
of local field investigations and had provided a basis
for the identification of significant natural areas in
the Regional Municipality of Ottawa-Carleton’s 1974
Official Plan. So significant was the role and mandate
of this group that the Natural Areas Committee was
soon being promoted as the most significant of Club
committees (LAC OFNC Collection, 8 December
1970). Increasing demand for input into various con-
servation issues both locally and beyond, resulted in
the establishment of the Research and Briefs Commit-
tee (1972-1973), which in 1974 was combined with the
Natural Areas Committee to form the Conservation
Committee. This committee continues to play an inte-
gral role in OFNC and community affairs to the
present day.
2004
The OFNC Centennial in 1979 understandably
brought forth a great deal of interest in the history of
the Club in particular and of the naturalist commu-
nity of Ottawa in general. Trail & Landscape provided
the major vehicle for sharing this information amongst
the local membership. Events culminated with a ban-
quet intended to be on the exact 100" anniversary,
but as with previous celebrations, it was erroneously
held on 19 March (Reddoch 1979a), not the actual
centennial date of 25 March.
The increased interest in the historical record gen-
erated by the Centennial year encouraged a new appre-
ciation of the designation of OFNC Honorary Mem-
bers. These had been given out only irregularly over
the years to honour lengthy, significant service to the
OFNC or Canadian natural sciences. Although honor-
ary memberships have been awarded more regularly
since 1971, the Centennial Year saw a new focus on
this acknowledgment of such exceptional contributions
(Brunton and Gummer 1987).
The conservation initiatives of the 1970s and early
1980s saw a resurgence of more systematic field
examinations of uncommon and ecologically significant
habitats in the Ottawa Valley such as fens, rivershore
communities, and relict woodlands (Dugal 1978;
Reddoch 1979b; White 1979). Publication of the first
complete, annotated checklist of the vascular plants
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 25
of the Ottawa District also reflected this knowledge
(Gillett and White 1978) and contained many of the
records newly discovered by Club members.
That burst of new knowledge and energy demon-
strated that suggestions in the early years of the 20"
century that our knowledge of the natural environ-
ment of the Ottawa area was all but complete, were
badly incorrect. Our understanding of native biodi-
versity and of the ecological systems supporting it
requires continual inventory and evaluation to enable
effective protection and maintenance of this natural
heritage.
The Club’s conservation activities in this era, led
by activist presidents Roger Foxall and Roger Taylor
between 1978 and 1982 and by such energetic mem-
bers as Loney Dickson, Allan Reddoch, Joyce Red-
doch, Albert Dugal, Stephen Darbyshire, and David
White, covered an amazing spectrum and exhausting
number of subjects. These ranged from a campaign for
a conservation area system in the Region of Ottawa-
Carleton (now city of Ottawa) to prevention of the
importation of Raccoon-dogs into Canada, and from
the prevention of 1988 Winter Olympic facility devel-
opment within Banff National Parks to consultations
with federal government officials on ecological re-
quirements in Gatineau Park and National Capital
Greenbelt planning.
Ficure 16. Excursion of Ottawa Field-Naturalists to the Rideau Trail in October 1979 (photograph by C. Beddoe). Contrast
with Figure 9. Long-time member Mary Stuart is second from left.
26 THE CANADIAN FIELD-NATURALIST
The Club hosted the annual meeting of the Feder-
ation of Ontario Naturalists in 1983, establishing a
successful program format that was followed by sub-
sequent provincial gatherings for years to come. The
OFNC again successfully hosted the provincial orga-
nization’s annual conference in 1993 (Pope 1993).
A more whimsical contribution is to wildlife con-
servation initiated in this period was the ““Seed-a-thon’”’,
a fund-raising effort whereby sponsors pledge a par-
ticular amount for every species observed on a par-
ticular day by a particular birding team, to be applied
towards the cost of supporting a network of OFNC
public bird feeder stations. Initiated by the Birds Com-
mittee on the suggestion of long-time OFNC member
Violet Humphries in 1981 (personal communication),
this was one of the first of what now are commonplace
fund-raising events across Canada (Brunton 1981).
There was a human cost to all this activity, how-
ever, and many of the lead Club personnel in these
matters eventually were called away by the mundane
but critical matters of family and careers, moving on
to other things and/or were simply exhausted by it all.
This was exacerbated in the later years of the 1970s
and into the 1980s by new pressures on the time and
resources of professional research staff within the
federal public service, reducing their availability and
energy for involvement in such initiatives as local
conservation and research. Only three OFNC presidents
since the mid 1970s (D. F. Brunton, R. John and E.
Zurbrigg), for example, were professionally involved
in natural environment investigation or management
(Appendix 1).
One of the most satisfying conservation ventures
of recent decades has to be the effort begun in the
early 1980s to save the massive, Provincially Signifi-
cant Alfred Bog east of Ottawa (Cuddy 1983) from
destruction by agri-business interests. This battle saw
the Club purchase conservation land for the first time
(in 1982) so as to have legal standing in the fight to
secure proper protective zoning. It was a long and
difficult effort but with the effective leadership of
OFNC President Frank Pope, considerable financial
and material contributions from numerous individual
members, and the critical involvement of the Nature
Conservancy of Canada, the entire wetland was saved
and is now either in protective public ownership or
zoned as parkland (Pope 2002).
The primary national contribution of the OFNC
continued to be led by the publication of the CEFN, al-
though as noted, direct involvement in national-scale
conservation issues was common enough in this peri-
od. Despite a continuing and perhaps even enhanced
national/international status and production standard,
however, the seemingly unanswerable question of how
national or local the journal should be was raised again
in a series of editorials in the late 1970s. The appro-
priateness and credentials of a citizen-based (‘‘ama-
teur”) organization directing the affairs of the journal
was severely criticized by Lorraine Smith, Editor 1972-
Vol. 118
1981, who suggested that “the burden of being account-
able to the scientific natural history community for a
national journal ... may now be more than this local
club should retain.” [The days of calling the OFNC a
“scientific society” were truly gone!] “Therefore... if
the journal’s reputation is not maintained and there is
no move for a change in publisher, I challenge those
who want a top-quality Canadian natural history jour-
nal, such as The Canadian Field-Naturalist is now, to
initiate a new journal” (Smith 1981). These comments
do not explain, however, how the OFNC managed to
maintain and enhance such a fine journal for so many
years.
After much discussion, consultation and review by
an Ad Hoc Committee on OFNC Publications com-
posed primarily of scientific specialists, the OFNC
Council approved (8 December 1982) a new Publica-
tions Policy to guide the CEN and other Club publi-
cations (Bedford 1983). The Policy reiterated the Club’s
continuing, century-long commitment to the scientific
integrity and high technical standards of the CFN, as
well as the Club’s intention to have the journal remain
the official publication of the OFNC.
Francis Cook assumed editorship of the CFN from
1962 to 1966, and again in 1981, and has guided the
journal to the present day with a steady and depend-
able hand, introducing important innovations such as
the publication of Canadian status reports for candidate
endangered species. There has been a great increase
in the amount of material published in each volume
during Cook’s tenure (volumes averaged 756 pages
over the five years ending in 2002). In the face of the
many complications in the publication process, the
timely publication of some issues has not occurred.
Scientific and technical quality has never been sacri-
ficed, however. The 28 volumes edited by Cook repre-
sent by far the longest and most prolific service of any
CEN editor in the 124-year history of the publication,
exceeding by more than a decade the tenure of the
next longest-serving editors, Harold Senn and Arthur
Gibson (Brunton 1986a).
Contemporary Times and the Future (mid-
1980s to date)
James Macoun, Percy Taverner and other “nation-
als” who worked so hard to enhance the mandate,
effectiveness, and reach of The Canadian Field-
Naturalist would be relieved to see that the publica-
tion has achieved the solid reputation, steady produc-
tion, and high scientific standards they hoped to see.
An interesting expression of that long-term contribu-
tion and durability is demonstrated in the number of
original descriptions (diagnoses of new taxa) which
have occurred in the pages of the CFN. Over 730 have
been published in the first 100 volumes (Brunton
1987).
The level of field-oriented investigation of the Otta-
wa Valley natural environment that was so productive
in the 1970s and early 1980s, however, has been dras-
2004
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB
Number of Members
| SS ES SSS CY MSY ET |
TS
prerereeco
FiGureE 17. Ottawa Field-Naturalists’ Club membership trend 1975-2003. Numbers of institutional subscribers to The Canadian
Field-Naturalist were not calculated within membership totals nor reported separately in Annual Reports after 1971.
A 1975 reorganization offered individual members (reported to total 1371 that year) the opportunity to be only non-
voting subscribers to the The Canadian Field-Naturalist, dramatically reducing the OFNC membership total reported
for 1976 (Erskine 1977) [Individual and institutional subscribers were reported separately in the Annual and Editor’s
Reports for The Canadian Field-Naturalist in each volume]. Absolute membership numbers prior to 1976, therefore,
are not directly comparable to these of subsequent years (from OFNC Annual Reports, 1975-2002).
tically reduced. The appearance of substantially fewer
area inventories and record documentation articles in
Trail & Landscape reflects that trend. This may be part
of an unfortunately strong North American perception
in recent decades that continuing, original field in-
vestigations are of less importance than in previous
times. T&L remains, however, an important and highly
relevant source of environmental news and natural
environment documentation.
Programs intended to actively involve the partici-
pation of local members have remained an important
part of the OFNC. Dozens of field outings, lectures
and special events are undertaken each year involving
a diversity of well-informed leaders and speakers.
For decades the Club’s Excursions and Lectures Com-
mittee has crafted an interesting and instructive program
that contributes greatly to the enhancement of members’
skills and to their enjoyment in the field. While field
investigations focus on both familiar and exotic local-
ities throughout the Ottawa District and the Ottawa
Valley, the Club does not confine itself to this area.
The spring “migration” of a bus load of OFNC mem-
bers to Point Pelee National Park, for example, has
become a popular biennial birding event since the 1980s.
This is important stuff. The majority of Club mem-
bers are locally based and most of us are involved,
first and foremost, because we enjoy exploring and
learning about our natural world. Providing support
for scientifically important undertakings such as the
publication of the CFN and the protection and preser-
vation of important natural landscapes, is a valuable
additional membership benefit. Membership in the
OFNC remains an easy and enjoyable way for indi-
vidual citizens to support greater understanding of,
and protection for, important natural landscapes and
features in the Ottawa Valley and beyond.
A noticeable change in the role of the local Club in
regards to its community has occurred in recent years.
The OFNC is much more integrated into environmen-
tal decision-making at a municipal and provincial
level than it has been at any time in its past. It has
become, in an sense, an ecological consultant to that
community. While such a role requires seemingly end-
less attendance at meetings and reduced time for core
field work, it has provided many excellent opportunities
for Club representatives to bring accurate ecological
information into the discussion of an issue at an early
and effective stage of the decision-making process. A
28 THE CANADIAN FIELD-NATURALIST
cynic might say that the Club has become somewhat
bureaucratized; an optimist would suggest that the Club
now more frequently has a seat at decision-making
tables across the National Capital Region. It is impor-
tant to note, for example, that it was through this per-
iod that the final protection of the important Alfred
Bog natural area was achieved.
Another very positive achievement of the last decade
was the establishment of the Louise de Kiriline Law-
rence Conservation Action Fund in 1994, founded with
a generous bequest from the estate of that outstanding
and eloquent field naturalist, Louise de Kiriline Law-
rence (1894-1992) (Ainley 1994). It is sustained by
further donations and by the profit from the sale of
particular OFNC products such as the “Natural Areas”
book (Brunton 1988). The fund provides for “stra-
tegic and timely expenditures towards the conservation
of natural areas” in the Ottawa Valley (Anonymous
1994).
A continuing interest for many Club members is
the Fletcher Wildlife Garden (FWG), established in
1987 in degraded woodland and regenerating agricul-
tural land on National Arboretum property near the
Rideau Canal. With the active cooperation and assis-
tance of Central Experimental Farm (Agriculture
Canada) personnel who are responsible for land man-
agement here, the Fletcher Wildlife Garden volun-
teers have transformed the site with native plantings,
the creation of a pond and through public interpre-
tation. The objective is not only to produce on-going,
evolving habitat restoration but to demonstrate suita-
ble wildlife-friendly landscaping and gardening prac-
tices for National Capital residents and visitors alike
— to be “a model for urban gardeners” (Conservation
Committee 1987).
These are all positive features. A disturbing trend in
Club affairs, however, has been declining membership
over the last two decades (Figure 17). Perhaps not
coincidentally, Club membership peaked ca. 1982 to
1985, at the end of the period of greatest conservation-
oriented activity. The local membership decline is
seemingly in tandem with the decline of original field-
based investigations. Nonetheless, the number of
OFNC members remains substantial — the Club is still
probably the largest regional natural history organi-
zation in Canada — but the downward membership
trend needs reversing (Figure 17).
The reasons for this decline in participation are un-
clear. It seems unlikely to be attributable to the ready
availability of up-to-date, comprehensive natural en-
vironment data on the World Wide Web since the mem-
bership decline began well before such technology
was widely available. It may, in part, be a function of
some wider, societal disinterest in hands-on involve-
ment with citizen-based, research-oriented groups.
Whatever the reason(s), the decline has been substan-
tial and if it continues, will undermine the financial
security and effectiveness of the OFNC.
Vol. 118
Since the 1990s the digital world has had as dra-
matic an impact on the OFNC as it has on so many
facets of contemporary Canadian life. We are only
just coming to terms with its potential benefits and
challenges. The OFNC’s impressive web page (http://
www.ofnc.ca) has allowed for rapid internal commu-
nications amongst Club officials, committee members
and conservation partners, and for the posting of
information and timely news items. Digital commu-
nication is only the latest expression of the Club’s
commitment to education of our membership and of
the general public in regard to important natural envi-
ronment features, needs and opportunities. The impor-
tance of the Club’s educational programs has been a
major theme throughout OFNC history and is ex-
pressed in the mission statement of the organization
(see frontispiece of this issue). There is every indica-
tion that it will remain so into the future.
It is not yet clear how the Club will move forward
from this foundation of established programs and re-
sources in order to stay informed, relevant — and sol-
vent — into the future. That’s not a new challenge but
is one that must be answered by each generation in
response to the circumstances and opportunities of
their day.
Some things are clear. For one, the Club needs to
re-establish a higher level of field-oriented investigation
amongst its membership. This will not only maintain
and develop the skills and interests of present mem-
bers but also inspire and generate new members. Ac-
curate and timely field investigation and documen-
tation are essential foundations for the maintenance
of the high level of technical credibility that the Club
has earned over the years. Continuing to do our home-
work, getting the facts straight, and presenting such
information in a defensible, objective manner are the
keys to maintaining and enhancing the OFNC’s impre-
ssive record of conservation achievement.
As with any organization, regardless of how vener-
able, the OFNC must also continue to re-examine what
it provides for the individual member. This is perhaps
even more critical in an era with an unprecedented
number of electronic diversions competing for the
attention of both members and partners alike. Will the
traditional superb program of excursions, lectures, and
publications be enough to inspire and encourage a
growing, involved membership? Do the new technol-
ogies of our time offer the same manner of new op-
portunities that technologies like the railway train,
electric lighting, the automobile, and the airplane
offered earlier OFNC members? They surely do.
What I hope is a clear message from this review of
the long, remarkably productive journey of Ottawa
naturalists is that the OFNC is not a static, hard-and-
fast “thing”. It is a community, an association of like
minds that aims to explore and celebrate the magnifi-
cent natural world of the Ottawa Valley and of Canada.
And as with any community, we in the OFNC have
2004
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB 29
tos
FIGURE 18. Record service to The Canadian Field-Naturalist: Left: Francis R. Cook, Editor 1962-1966; Associate Editor
(Herpetology) 1972-1981; Editor 1981-present; right: William J. Cody, Business Manager 1948-present. 25 August
2004. Photo courtesy Ron Bedford.
and have had the benefit of the skills, insight, and
inspirational leadership of numerous individuals and
groups over the years.
In weak times and strong, the common thread that
has bound Ottawa naturalists since 1879 — indeed, since
1863 — is an overwhelming desire to contribute to the
protection and enhancement of the natural features
and values that make this place so special. At the end
of the day it comes down to the fact that James Fletcher,
Frank Pope, Percy Taverner, Sheila Thomson, Edward
Van Cortlandt, Herb Groh, Gordon Hewitt, and the rest
of us are not that different ... we’re all just Ottawa
field naturalists.
Acknowledgments
The daunting challenge of reviewing a manuscript
of this nature was undertaken in a timely and helpful
manner by a team of naturalists well familiar with the
OFNC and OFNC personalities. These reviewers were
Ron Bedford, Bill Cody, Francis Cook, Karen McIntosh,
Elizabeth Morton, Frank Pope and Joyce Reddoch.
They added much to the effort and I gratefully ack-
nowledge their input. I remain, however, fully respon-
sible for any errors or omissions which may have
escaped their sharp eyes. Frank Pope and Francis
Cook provided additional factual input throughout
the development of the manuscript. This review has
also benefitted from the innumerable discussions (and
debates!) I have enjoyed with Francis Cook over the
last 25 years on numerous subjects related to the his-
tory of the OFNC and to the study of Canadian natural
sciences. Ron Bedford, Frank Pope, Joyce Reddoch,
and Rob Lee (present chair of the Macoun Field Club)
were instrumental in obtaining many of the illustra-
tions employed in this article. Rob Lee and Joyce Cook
scanned several of these. I am happy too, to acknowl-
edge two other important players in this effort. First
is the late Herb Groh whose clipping file on OFNC
personalities and whose interest in the Club’s past
inspired my own curiosity. The other gratefully ack-
nowledged is the staff at the Library and Archives
Canada (formerly the National Archives of Canada)
who so efficiently and pleasantly facilitated my
research with the OFNC collection and related files
held within the walls of that national treasure.
Documents Cited (marked * in text)
Dorais, M., R. Bouffard, R. Chenier and K. Adamson.
1974. An examination of the past and present status of the
Mer Bleue Peat Bog near Ottawa, Ontario. [Unpublished
report], Faculty of Science and Engineering, University
of Ottawa. 105 pages.
LAC OFNC Collection. Ottawa Field-Naturalists’ Club
Collection (MG 28 I 31), Library and Archives Canada,
Ottawa.
LAC Taverner Collection. Percy A. Taverner collection,
Library and Archives Canada, Ottawa.
30 THE CANADIAN FIELD-NATURALIST
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32. THE CANADIAN FIELD-NATURALIST
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Received 22 June 2004
Accepted 10 August 2004
END NOTES:
' Number 1 (un-numbered), Braddish Billings’ Ottawa
vascular plant list (Billings 1868) was published between
March and November 1868; Number 2 (numbered), 500
copies of Sir J. A. Grant’s examination of the surficial
geology of the Ottawa Valley (Grant 1868) were published
December 1868; Number 3 (numbered), Thomas Wily’s
discussions of swallows (Wily 1869) was published De-
cember 1869 (LAC OFNC Collection, 10 December 1869;
Dore 1968).
Much later, Henry Ami reminiscing about events leading
up to the formation of the Club described *... how the
Ottawa Club originated from the Epping Forest and Field
Club, and later Ottawa Naturalists Club ...” (LAC OFNC
Collection, 2 February 1924). Ami may, however, have
been referring to names applied to informal groupings of
field associates, such as the Fletcher, Harrington et al.
group which conducted field work together in the Billings
Bridge area in the late 1870s (Harrington 1909). There is
no further mention of these groups in OFNC records by
any of the individuals who, unlike Ami, were actively
involved in the formation of the Club.
Later, R. B. Whyte erroneously reported this as occurring on
19 March 1879 (Whyte 1880). He may have been referring
to an earlier preliminary meeting or to the date of the
OLSS Council meeting where Fletcher and Henry Small Jr.
obtained an expression of the co-operation and assistance
from the parent organization, rather than the formal orga-
nizational gathering. Being documented only one year after
the fact and by a Club founder and the originator of the
idea of the OFNC, this error would quite understandably
be accepted as fact and was repeated for over 100 years
as the formal starting date of the OFNC (e.g. Groh 1955;
Taylor 1979).
+ Relations between The Ottawa Field-Naturalists’ Club and
The Ottawa Literary and Scientific Society appear to have
been strained on at least several occasions in the following
years. In his 30 November 1886 Inaugural Address, for
example, OLSS President W. P. Anderson complained
nN
Vol. 118
that the OFNC (of which he was a founding member and
had been the Treasurer for the previous three years!) was
“antagonistic to the Ottawa Literary and Scientific Soci-
ety” (LAC OFNC Collection, 3 December 1886). The
OFNC and OLSS councils individually discussed the prob-
lem, the OLSS Council subsequently stating that they
would consider “ ... any proposition which the field Club
may wish to make looking for a change in the relations
between the Club and the Society but that a joint meeting
of the two Councils cannot conveniently be arranged ...”
(LAC OFNC Collection, 14 January 1887). Although no
such joint meeting or other formal Club action resulted,
the OFNC Council continued to meet in the OLSS
museum until March 1890. That was despite another
minor dust-up in 1889 concerning the OFNC’s offer to
cover some of the public lecture programming required
of the OLSS in order to maintain its Ontario government
grant (LAC OFNC Collection, 6 November 1889).
The involvement of women in the OFNC was very much
promoted in these early years — in a patronizing if sincere
way. The launch of The Ottawa Naturalist was accompa-
nied by a special plea for the involvement of women ...
“especially will be ladies welcomed to our ranks, and every
effort will be put forward to make the excursions and
soirees pleasant as well as instructive” (Harrington 1887).
At the March 1888 Annual Meeting “... a discussion en-
sued as to the eligibility of ladies as officers, and the
desireability of having some on the Council. Professor
Macoun gave notice that he would at the next General
meeting of the Club move that the executive Committee
consist of six members, three of whom shall be ladies”
(LAC OFNC Collection, 20 March 1888). This was accom-
plished by a Constitutional amendment in March 1890.
Margaret A. Mills became the first female OFNC Officer
when “Miss Mills” was elected Second Vice-President in
1892 (LAC OFNC Collection, 15 March 1892). She was
not present at the meeting, however, and was apparently
not agreeable to her election, as she resigned effective the
next Council meeting 9 days later (LAC OFNC Collection,
24 March 1892), but stayed on as a Club member for
several more years.
“This [Ottawa] District was then [1880] understood to
mean a radius of about twelve miles from the City of
Ottawa ... latterly, however, with the general consent of
the botanists of the club, this radius has been extended to
about 30 miles ...” (Fletcher 1888). The Ottawa District
boundary was metricated in 1981 to a 50 km radius circle
centred on the Peace Tower of the Parliament Buildings
(Anonymous 1981), including landscape within both south-
eastern Ontario and southwestern Quebec.
The portrait hung for many years in the Geological Survey
Museum (later, National Museum of Canada). It now can
be seen on display in the Logan Gallery of the Geological
Survey of Canada headquarters on Booth Street in Ottawa.
The saga of the OFNC library does not end there, however.
In 1948 the Ottawa Public Library (OPL) reported to the
Club that they had discovered “... the old library of the
Club, now deposited in a storeroom adjacent to the main
library” and that several hundred dollars worth of Canadian
Field-Naturalist (CFN) back numbers were recovered
(LAC OFNC Collection, 29 October 1948). The Council
agreed to thank the OPL for storing the collection (since
1917!) by donating a set of The CFN back to 1935.
Although the OPL apparently offered to continue to store
2004
a
oO
the 24 shelves worth of material at no cost to the Club,
Council determined that all of the natural history and
geology books should be sold (LAC OFNC Collection,
22 November 1948). No one was aware, apparently, that
the Club had given the library to the OPL back in 1917 and
thus was obviously in no legitimate position to sell the
material. Nonetheless, the library was sold to “Mr.
[Bernard] Amtmann, a dealer in second hand books ...”
who assured the Council that OFNC members “would be
given first choice before the [collection] catalogues were
sent out ... through his extensive mailing list” (LAC OFNC
Collection, 19 January 1950). The Club’s initial share of
sales before Amtmann moved to Montreal with the collec-
tion was $169 (LAC OFNC Collection, 20 November 1950);
the following year Amtmann offered the Club $200 for the
remaining volumes of the library which he had sold off
“on a poundage basis” and for which he claimed to have
incurred a considerable loss. The offer was accepted (LAC
OFNC Collection, 16 November 1951) ... a sad ending
to what must have been a magnificent collection with an
intriguing provenance.
The portrait by Franklin Brownell was commissioned in
late 1911 (LAC OFNC Collection, 18 December 1911)
and hung in “a suitable and prominent place” in the Ottawa
Public Library in the spring of 1912 (LAC OFNC Collec-
tion, 12 March 1912). In the 1920s it was transferred to
the National Museum of Canada “for safekeeping” (LAC
OFNC Collection, 14 December 1926) where it hung for
many years in the herbarium, its actual ownership and
the “temporary” nature of its placement at The Museum
eventually forgotten. When this history was discovered and
brought to the attention of National Museum of Natural
Sciences Assistant Director (and former OFNC Vice-Pres-
ident) C. G. Gruchy and Agriculture Canada staff in 1985
(personal communication), arrangements were made by
The Museum for cleaning and minor restorations to be
undertaken. The portrait, still technically owned by the
Club and on loan to The Museum, was officially donated to
The Farm on 2 June 1986 by OFNC 1986-1988 President
W. G. Gummer (1915-1999) as part of the celebrations of
100 years of agricultural research in Canada (Hall 1986).
The Museum and the Club had now fully honoured their
commitment to the memory of James Fletcher. The portrait
presently hangs, appropriately enough, in the William
Saunders Building, named after the Central Experimental
Farm Director who hired Fletcher as Canada’s first Domin-
ion Entomologist and Botanist.
The Ottawa Naturalist was published quarterly for a brief
period (1889/1890) as a cost-saving measure but reverted
to monthly publication (at the urging of Will Harrington)
because of reader preference for more frequent produc-
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB
w
15
33
tion. This was initiated despite the Club’s request for a
provincial publication assistance grant being denied. An
avowed Tory, John Macoun proclaimed that “‘politics had
intervened with the success of the application and that we
would have to learn to vote properly before we could hope
to succeed ...” (LAC OFNC Collection, 18 March 1890).
The none too subtle shot at the long serving Liberal govy-
ernment of Oliver Mowat was quite likely an accurate
observation of the politics of that day (Gywn 1984). The
Ottawa Naturalist did eventually receive a provincial gov-
ernment publication grant (of $300.00), beginning in 1897.
But presumably to Macoun’s chagrin, this occurred with
the Liberals still in power! Provincial financial assistance
was received thereafter until 1924 (LAC OFNC Collection,
3 November 1924), as was generous federal publication
support funding for The Canadian Field-Naturalist in the
1980s and 1990s.
The Macoun Autobiography was reprinted as an OFNC
Special Publication in the Club’s centennial year (Macoun
1979), with an new introduction by Richard Glover and
with both editorial notes and a biographical sketch by
historian William A. Waiser.
P. B. Symes presented his “nearly complete set” of The
Canadian Field-Naturalist and its predecessors to the
Club in 1923. It formed the basis for “the Club’s set of
original issues” (Patch 1923) which is maintained for the
purposes of the current CFN editor. The set is now complete
(Francis Cook, personal communication).
When Pauline Snure was elected in 1948, she was the first
woman president of the OFNC, despite the conspicuous
affirmative action efforts on behalf of women members by
James Fletcher and associates in the 1880s and again in
the first decade of the 20" century.
It was presumably this 75" anniversary that inspired Herb
Groh to develop a biographical clipping file on OFNC
Presidents and other officers. The file was presented to the
Club in the early 1980s by Pierre Taschereau on behalf of
Groh’s widow and is now preserved in the LAC OFNC
Collection.
The present editor has suggested (personal communication)
that this treatment might be overly critical of Senn’s edi-
torial tardiness in comparison to the at-times substantial
delay of issues of the CFN during his (Cook’s) tenure.
While recent delays sometimes approached (though
never matched) those of the 1950s, the critical difference
between the two was the impact on the Club in their res-
pective eras. The substantial publication delay in the early
1950s all but shut down Club productivity. While not to
suggest that contemporary publications delays are without
impact, they are clearly less threatening than those of 50
years ago.
34
THE CANADIAN FIELD-NATURALIST
APPENDIX 1: Ottawa Field-Naturalists’ Club officers (1879-2004)
(derived from (LAC OFNC Collection Minute Books (1879-1970) and The Canadian Field-Naturalist listings and contem-
porary OFNC Council Minutes)
1879/1880
1880/1881
1881/1882
1882/1883
1883/1884
1884/1885
1885/1886
1886/1887
1887/1888
1888/1889
1889/1890
1890/1891
1891/1892
1892/1893
1893/1894
1894/1895
1895/1896
1896/1897
1897/1898
1898/1899
1899/1900
1900/1901
1901/1902
1902/1903
1903/1904
1904/1905
1905/1906
1906/1907
President
W. White
J. Fletcher
W. R. Riddell*
J. Fletcher
J. Fletcher
H. B. Small Jr.
H. B. Small Jr.
W. H. Harrington
John Macoun
R. B. Whyte
R. B. Whyte
R. W. Ells
R. W. Ells
R. W. Ells
G. W. Dawson
G. W. Dawson
G. W. Dawson
F. Shutt
F. Shutt
EWE. Prince
BE Prince
H. M. Ami
H. M. Ami
R. Bell
R. Bell
W. T. Macoun
W. T. Macoun
S. B. Sinclair
W. J. Wilson
Vice-President(s)!
J. Fletcher
W. P. Riddell*
W. D. LeSueur*
R. B. Whyte
W. D. LeSueur
R. B. Whyte
H. B. Small Jr.
R. B. Whyte
J. F Whiteaves
R. B. Whyte
F. R. Latchford
R. B. Whyte
J. Fletcher
John Macoun
S. Woods
R. B. Whyte
S. Woods
John Macoun
S. Woods*
C. F. Marsan
R. W. Ells
H. M. Ami
J. Ballantyne
R. B. Whyte
J. Ballantyne
H. M. Ami
T. S. MacLaughlin
W. H. Harrington*
M. A. Mills*
F. Shutt
R. W. Ells
F. Shutt
J. Fletcher
F. Shutt
H. M. Ami
John Macoun
W. S. O'Dell
R. Bell
D. A. Campbell
W. T. Macoun
A. E. Attwood
W. T. Macoun
A. E. Attwood*
A. Halkett
W. J. Wilson
S. B. Sinclair
W. J. Wilson
F. Shutt
F. Shutt
Treasurer
R. B. Whyte?
W. H. Harrington?
W. H. Harrington?
W. P. Anderson
W. P. Anderson
W. P. Anderson
T. S. MacLaughlin
T. S. MacLaughlin
J. Fletcher
J. Fletcher
J. Fletcher
J. Fletcher
G. Harmer
A. G. Kingston
A. G. Kingston
.Am
"Harrington
ig*
J. Fletcher
J. Fletcher
J. Fletcher
J. Fletcher
A. Gibson
A. Gibson
A. Gibson
A. Gibson
A. Gibson
Vol. 118
Secretary(ies)”
R. B. Whyte?
W. H. Harrington?
W. H. Harrington?
W. H. Harrington
W. H. Harrington
W. H. Harrington
W. P. Anderson
W. H. Harrington
W. H. Harrington
T. S. MacLaughlin
T.S. MacLaughlin
T. S. MacLaughlin
W. H. Harrington
H. M. Ami
H. M. Ami
H. M. Ami
A. Halkett
A. Halkett
A. Halkett
W. J. Wilson
W. J. Wilson
W. J. Wilson
W. J. Wilson*
W. J. Wilson
W. J. Wilson*
T. E. Clarke
T. E. Clarke
T. E. Clarke
2004
1907/1908
1908/1909
1909/1910
1910/1911
1911/1912
1912/1913
1913/1914
1914/1915
1915/1916
1916/1917
1917/1918
1918/1919
19193
1920
1921
1922
1923
1924
1925
1926
1927
1928
1929
1930
1931
1932
1933
1934
1935
1936
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB
President
W. J. Wilson
A. E. Attwood
A. E. Attwood
A. Halkett*
A. G. Kingston*
A. McNeill
L. H. Newman
L. H. Newman
A. Gibson
A. Gibson
H. I. Smith
H. I. Smith
C. G. Hewitt
M. Y. Williams
M. Y. Williams
R. M. Anderson
R. M. Anderson
H. Lloyd
H. Lloyd
H. Lloyd*
G. A. Miller*
N. Criddle
N. Criddle
E. M. Kindle
E. EF. G. White
H. F. Lewis
H. F. Lewis
C. M. Sternberg
C. M. Sternberg
M. E. Wilson
M. E. Wilson
H. Groh
Vice-President(s)!
A. E. Attwood
A. E. Attwood
A. Halkett
A. Halkett
E. FG. Eifrig
A. Halkett
E. E.G. Eifrig
A. G. Kingston
L. H. Newman
A. Gibson
L. H. Newman
A. Gibson
J. W. Gibson
A. Gibson
H. I. Smith
C. G. Hewitt
H. I. Smith
C. G. Hewitt
H. I. Smith
C. G. Hewitt
E. D. Eddy
M. Y. Williams
C. G. Hewitt
L. D. Burling
M. Y. Williams
L. D. Burling
P. A. Taverner
L. D. Burling
R. M. Anderson
G. A. Miller
H. Lloyd
H. Lloyd
G. A. Miller
G. A. Miller
N. Criddle
G. A. Miller
N. Criddle
G. A. Miller*
N. Criddle
E. M. Kindle*
es}
=
a
5
M
Ib,
L
F
F
. M. Sternberg*
wiePatch=
. E. Wilson
. M. Sternberg
. E. Wilson
. M. Sternberg
. E. Wilson
erie fe) ea19 ke (Viel =" eafevol esli@l
Qt
=
fe)
=
P. A. Taverner
H. Groh
P. A. Taverner
P. A. Taverner
R. DeLury
Treasurer Secretary(ies)?
A. Gibson T. E. Clarke
A. Gibson T. E. Clarke
A. Gibson E. Clarke
H. Groh J. J. Carter
W. T. Macoun D. E. Blackader
W. T. Macoun D. E. Blackader
W. T. Macoun E. D. Eddy
G. LaLacheur
G. LaLacheur
J. R. Dymond
J. R. Dymond*
F. W. Waugh
E. B. Crampe*
C. B. Hutchings
C. B. Hutchings
C. B. Hutchings
B. A. Fauvel
B. A. Fauvel
B. A. Fauvel
B. A. Fauvel
B. A. Fauvel
W. Lloyd
W. Lloyd
W. Lloyd
W. Lloyd
W. Lloyd
W. Lloyd
W. Lloyd
W. Lloyd
J. F Watson E. D. Eddy
A. Halkett*
G. O. McMillan
L. D. Burling
L. D. Burling
C. L. Patch
C. L. Patch
C. L. Patch
C. L. Patch
C. L. Patch
C. L. Patch
J. FE. Wright
J. E. Wright
J. F Wright
J. F. Wright
J. F Wright
B. A. Fauvel
B. A. Fauvel
G. S. Postethwaite
G. S. Lewis
G. S. Lewis
G. S. Lewis
P. Whitehurst
P. Whitehurst
36
1937
1938
1939
1940
1941
1942
1943
1944
1945
1946
1947
1948
1949
1950
1951
1952
1953
1954
1955
1956
1957
1958
1959
1960
1961
1962
1963
1964
1965
1966
1967
THE CANADIAN FIELD-NATURALIST
President
H. Groh
P. A. Taverner
A. E. Porsild
A. E. Porsild
H. G. Crawford
H. G. Crawford
D. Leechman
D. Leechman
FE. Banim
F. E. Banim
W. H. Lanceley
W. H. Lanceley
P. Snure
P. Snure
J. W. Groves
J. W. Groves
R. Frith
R. Frith
W. K. W. Baldwin
W. K. W. Baldwin
L. S. Russell
L. S. Russell
E. L. Bousfield
E. L. Bousfield
W. W. Mair*
D. R. Beckett*
D. R. Beckett
D.R. Beckett
G. McGee
G. McGee
G. McGee
H. Mackenzie
Vice-President(s)!
P. A. Taverner
R. DeLury
R. DeLury*
H. G. Crawford*
A. E. Porsild
H. G. Crawford
D. Leechman
H. G. Crawford
D. Leechman
D. Leechman
D. Leechman
F. E. Banim
F. E. Banim
W. H. Lanceley
F. E. Banim
W. H. Lanceley
W. H. Lanceley
A. L. Rand
W. H. Lanceley
A. L. Rand
A. L. Rand
P. Snure
P. Snure
J. W. Groves
J. W. Groves
R. Frith
J. W. Groves
R. Frith
R. Frith
W. K. W. Baldwin
K. W. Baldwin
Senn
K. W. Baldwin
E. Bourguignon
Russell
Bousfield
Russell
Bousfield
B
B
IL,
E
Le
E ousfield
leakney
Bousfield
Bleakney
W. W. Mair
D. R. Beckett
W. W. Mair
D. R. Beckett
D. R. Beckett*
V. Solman*
E. Bousfield
W. W. Mair
D. A. Smith
W. W. Mair
G. McGee
W. W. Mair
G. R. Hanes
W. W. Mair
F. R. Cook
F. R. Cook
H. Mackenzie
J. C. Woolley
T. Mosquin
W.
H.
W.
A.
9.
a
Sy
Bas
Hf
MS
ae
ssh
J
E
J
Treasurer
W. Lloyd
W. Lloyd
W. Lloyd
W. Lloyd
W. Lloyd
C. H. D. Clarke
I. Conners
I. Conners
I. Conners
I. Conners
C. Frankton
C. Frankton
C. Frankton
C. Frankton
R. J. Moore
R. J. Moore
R. J. Moore
R. J. Moore
R. J. Moore
R. J. Moore
R. J. Moore
R. J. Moore
J. M. Gillett
J. M. Gillett
J. M. Gillett
A. Banning
A. Banning
A. Banning
A. Banning
R. D. Wainwright
L. G. Howden
Vol. 118
Secretary(ies)”
P. Whitehurst*
C. W. Lounsbury*
C. W. Lounsbury
C. W. Lounsbury
C. W. Lounsbury
C. W. Lounsbury
J. W. Groves
J. W. Groves
J. W. Groves
J. W. Groves
O. H. Hewitt
O. H. Hewitt
H. J. Scoggan
H. J. Scoggan
J. Scoggan
J. Scoggan
J. Scoggan
al
. Scoggan
J. Scoggan
. Scoggan
J. Scoggan
J. Scoggan
M. Banfield
M. Banfield
M. Banfield
ee ee eee
a
M. Banfield
A. M. Banfield
D. A. Smith
A. W. Rathwell
A. W. Rathwell
A. W. Rathwell
A. W. Rathwell
2004
1968
1969
1970
1971
1972
1973
1974
1975
1976
1977
1978
1979
1980
1981
1982
1983
1984
1985
1986
1987
1988
1989
1990
199]
1992
1993
1994
1995
BRUNTON: THE OTTAWA FIELD-NATURALISTS’ CLUB
President
H. Mackenzie
H. Mackenzie
T. Mosquin
T. Mosquin
S. Thomson
I. M. Brodo
I. M. Brodo
E. C. D. Todd
E. C. D. Todd
R. A. Foxall
R. A. Foxall
R. Taylor
R. Taylor
R. Taylor
D. F. Brunton
D. F. Brunton
E. F. Pope
E. F. Pope
W. Gummer
W. Gummer
J. Harrison
J. Harrison
J. Harrison
R. John*
E. F. Pope
ESE Pope
E. EF. Pope
E. F. Pope
Vice-President(s)!
T. Mosquin*
J. Tener*
G. McGee*
T. Mosquin
W. A. Holland
W. A. Holland
S. Thomson
S. Thomson
I. M. Brodo
I. M. Brodo
E. C. D. Todd
E. C. D. Todd
E. C. D. Todd
R. A. Foxall
R. A. Foxall
R. Taylor
R. Taylor
C. Gilliatt
H. L. Dickson
H. L. Dickson*
D. F. Brunton*
C. G. Gruchy
P. M. Catling
C. G. Gruchy*
ESE; Pope*
P. M. Catling
W. Gummer
W. P. Arthurs
W. Gummer
W. P. Arthurs*
B. A. Campbell
J. Harrison
D. F. Brunton
J. Harrison
D. F. Brunton*
K. Strang*
J. Harrison
R. John
K. Strang
R. John
D. Cuddy
E. Fox*
S. Blight*
vacant
M. Murphy
M. Murphy
D. Moore
M. Murphy
D. Moore
Treasurer
37
Secretary(ies)?
L. G. Howden
F. M. Brigham
F. M. Brigham
F. M. Brigham
P. Kevin
C. Gruchy
C. Gruchy
P. J. Sims
P. J. Sims
B. Henson
B. Henson
B. Henson
B. Henson
B. Henson
P. D. M. Ward
P. D. M. Ward
P. D. M. Ward
P. D. M. Ward
P. D. M. Ward
F. Valentine
F. Valentine*
J. Gehr
M. Scromeda
G. Marston
G. Marston
G. Marston
G. Marston
G. Marston
A. W. Rathwell
A. W. Rathwell
A. W. Rathwell
A. W. Rathwell
A. W. Rathwell
A. J. Erskine (RS)
A. H. Reddoch (CS)
A. J. Erskine (RS)
J. D. Lafontaine (CS)
A. J. Erskine (RS)
C. Gruchy (CS)
P. J. Narraway (CS)
A. J. Erskine (RS)
D. Laubitz (RS)
S. Armstrong (CS)
D. Laubitz (RS)
S. Armstrong (CS)
D. Laubitz (RS)
V. Hume (CS)
D. F. Brunton (RS)
E. F. Pope (CS)
E. F. Pope (RS)
W. Gummer (CS)
E. F. Pope (RS)
W. Gummer (CS)
E. F. Pope (RS)
W. Gummer (CS)
G. Hamre (RS)*
A. Martell (CS)*
B. Martin (RS & CS)*
A. Martell (CS)*
B. A. Campbell (CS)*
B. J. Martin (CS)
E. Bottomley (RS)
B. A. Campbell (CS)
M. Coleman (RS)
D. F. Brunton (RS)*
R. John (RS)*
B. A. Campbell (CS)
D. Duchesne (RS)
M. Aksim (CS)
E. Fox (RS)
E. Evans (CS)
E. Evans (CS)
D. Furlong (RS)*
C. Firth (RS)*
N. Stow (RS)*
E. Fox (RS)*
E. Evans (CS)
C. Clark (RS)
S. Gawn (RS)
E. Evans (CS)
S. Gawn (RS)
E. Evans (CS)
D. Smythe (RS)
E. Evans (CS)
38 THE CANADIAN FIELD-NATURALIST Vol. 118
President Vice-President(s)! Treasurer Secretary(ies)”
1996 D. Moore M. Murphy G. Marston D. Smythe (RS)
E. Evans (CS)
1997 D. Moore M. Murphy S. Shaw* D. Smythe (RS)
T. Reeve* L. Cairnie (CS)
1998 D. Moore E. Zurbrigg S. Shaw G. McNulty (RS)
D. Smythe vacant (CS)*
1999 D. Moore E. Zurbrigg ESE: Pope? G. McNulty (RS)
D. Smythe vacant (CS)*
2000 E. Zurbrigg R. John E. F. Pope J. Martens
2001 E. Zurbrigg R. John E. F. Pope K. Allison
2002 E. Zurbrigg R. John E. F. Pope K. Allison
2003 G. McNulty M. R. Murphy E. F. Pope S. L. Bourque
G. Marston
2004 M. R. Murphy G. Marston E. F. Pope S. L. Bourque
* served only a portion of this term; RS — Recording Secretary CS — Corresponding Secretary
' First and Second Vice-President positions existed in most but not all terms.
2 Secretary and Treasurer positions were combined until 1882;
> The OFNC “year” was rearranged in 1919 to coincide with the calendar year rather than the fiscal year, resulting in a
1918-1919 year ending in March 1919, a9 month “year” for the remainder of 1919, and normal calendar years thereafter.
* Corresponding Secretary position left vacant for two years then eliminated; Recording Secretary position continues.
Continuing Environmental Change — An Example from Nova Scotia
EDMUND S. TELFER
Scientist Emeritus, Canadian Wildlife Service, Environment Canada
Current address: 3582-42 Street, Edmonton, Alberta, T6L 5A1 Canada
Telfer, Edmund S. 2004. Continuing environmental change — an example from Nova Scotia. Canadian Field-Naturalist
118(1): 39-44.
Information from personal experience, from community elders and published literature served as a basis for evaluating envi-
ronmental changes in the District of North Queens and adjacent areas of Southwestern Nova Scotia over the past century. Major
events included disappearance of the Caribou (Rangifer tarandus), the arrival of White-tailed Deer (Odocoileus virginianus),
the severe reduction of Canada Yew (Taxus canadensis), disappearance of Lynx (Lynx canadensis), a major dieoff of Striped
Skunks (Mephitis mephitis), decline of American Beech (Fagus grandifolia), the loss of mature birch (Betula spp.), the severe
reduction of Moose (Alces alces), the arrival of the American Dog Tick (Dermacentor variabilis) and Coyotes (Canis latrans),
and the restoration of Beaver (Castor canadensis). The proximate cause of many of those changes were plant and animal
disease, while the ultimate causes were naturally occurring animal range expansion and human impacts. The warming of the
climate over the past 150 years probably played a role. The nature and timing of the events could not have been predicted.
Key Words: Nova Scotia, plant and animal diseases, change in biota, climate change, adaptive management.
Here, I present and discuss an example of long-term
environmental change. It is a narrative account of
changes in the occurrence of some mammals and plants
in my home area, the District of North Queens, and
surrounding portions of the interior of southwestern
Nova Scotia. I personally observed these changes or
heard about them from my father and other community
elders and further document them by reference to the
available literature. I discuss the changes in the light
of current resource management philosophy. Since my
father was born in 1882 and was a teenager in the 1890s,
the changes noted cover a century.
The District of North Queens lies in the interior of the
southwestern peninsula of Nova Scotia and is centred at
approximately 65°09'W and 44°18'N. It is an area of
scattered farms and homesteads where the population
has subsisted for 200 years on a mix of agriculture and
forestry. The district contains the western portion of a
swarm of glacially-formed drumlin hills that occur in
Lunenburg and Queens counties (Roland 1982). Drum-
lins provide arable land but comprise a small propor-
tion of the land area. Most of the district is rocky, for-
ested terrain that, even where cultivatable and produc-
tive, was difficult for early settlers to clear. The remain-
der of the interior of western Nova Scotia is a complex
of water bodies, bogs, fens, barrens and stony soils
supporting Acadian forests of mixed conifers and decid-
uous tree species (Rowe 1972). When my father was
born the area contained considerably more crop agri-
culture and improved pasture than today. For the County
of Queens as a whole, approximately 30 000 acres
(12 140 ha) were under agriculture in 1870 (Canada
1871). This area dropped to 7410 acres (2999 ha) by
1966 (Nova Scotia 1966). However, those were small
proportions of the total area, 4.4% in 1870 and 1.1%
in 1966. Because the terrain is very complex, and the
forest composed of many small stands, with the whole
divided into small private land parcels, timber harvest
has consisted of cutting small patches or individual trees
as a market or need for the wood occurred. However, in
recent years there have been larger clearcuts and some
conversion of mixed forest to conifer plantations on
industrial ownerships. The decline in the area of mixed-
wood has been counterbalanced to an unknown extent
by reversion of agricultural land to mixedwood forest
and by improved fire protection (Telfer 1971).
Mammals
In the 1880s Caribou Rangifer tarandus, were still
common in unsettled parts of Nova Scotia (Rand 1933;
Sheldon 1936). An old hunter (the late F. M. Forrest,
personal communication) told me of a trip he made
when he was 16 years old (that would have been in
1888) to find Caribou. Somewhere at the west side of
the present day Kejimkujik National Park he found a
herd on a large barren and had a good chance to ob-
serve them and to shoot a fat yearling to replenish his
provisions. Within 20 years Caribou appear to have been
gone from North Queens. Another old woodsman (the
late E. B. Smith, Sr., personal communication) told me
that when he began to guide sportsmen in the early
1900s there were still broad trails beaten though the
woods in all directions in the remote parts of the District
that had been made and kept open by Caribou. Sheldon
(1936) also commented on the Caribou trails. By my
time the Caribou were long gone and their trails had
faded away before the encroaching forest. Caribou
suffered from logging and burning on their winter
ranges and from poorly controlled hunting. However,
the probable final cause of Caribou extirpation was
39
40 THE CANADIAN FIELD-NATURALIST
meningeal worm, Parelaphostrongylus tenuis, intro-
duced by White-tailed Deer, Odocoileus virginianus
(Benson and Dodds 1977).
The loss of a large mammal like Caribou from the
regional fauna quite probably had at least minor im-
pacts on other plants and animals living in the area. I
have not been able to find any records of any obser-
vations of such impacts. However, Caribou move fast
and far and feed while moving so they spread their
use of vegetation out in time and space (Miller 1982).
The relatively small population of Caribou in Nova
Scotia would have had slight impact on other species.
Moose, Alces alces, were distributed throughout
Nova Scotia and were the common game animal in
my father’s youth. However, after 1926 they were
observed to be dying (Sheldon 1936; Benson 1958).
The sick Moose exhibited symptoms similar to those
later described by Anderson (1965) as resulting from
infestation by the meningeal worm (Parelaphostron-
gylus tenuis). This organism was later found in Nova
Scotia Moose by Smith et. al (1964). Parelaphostron-
gylus tenuis is relatively common in White-tailed Deer.
It does little harm to whitetails but may cause heavy
mortality among other species of the deer family
(Thomas and Dodds 1988). By the 1940s, Moose were
dying in large numbers from the condition which had
come to be called “Moose Sickness” (Benson and
Dodds 1977). The animals showed evidence of paral-
ysis, blindness and other neurological symptoms al-
though they were often in good physical condition
otherwise. Annual reports of the Nova Scotia Depart-
ment of Lands and Forests commented on the dead
Moose. The 1949 report was typical, “Nearly all
Rangers report moose as being in a healthier condi-
tion which is perhaps indicated by the decrease in the
number of moose which were found dead. This number
was 75, a decrease of 74 from last year” (Nova Scotia
1949: 65). Of course only a fraction of the dead Moose
would have come to the attention of the authorities.
Moose almost vanished from southwestern Nova Scotia
by the 1960s but recovered slightly following later
declines in deer numbers.
Although P. tenuis was found in some Nova Scotia
Moose in the 1960s and has been shown to cause a
“moose sickness” type of illness, that does not prove
that all the animals that perished in the dieoff of
Nova Scotia Moose in the 1930s and 1940s died of
meningeal worm infection. However, the similarity of
the symptoms displayed by the sick Moose suggests
that most died of the same cause. Moose have been
found to suffer from neurological symptoms where no
P. tenuis has been observed in autopsies (Tony Nette,
personal communication). Those symptoms have been
recently linked to deficiencies of cobalt and vitamin
B,, (Frank et al. 2004). However, it seems unlikely
that a nutritional deficiency would cause a catastrophic
dieoff like that reported in Moose in Nova Scotia in
the 1940s, and the coincidence of the dieoff with the
Vol. 118
post-introduction boom in White-tailed Deer num-
bers suggests that P. tenuis was the principal cause.
My father was an adult before deer showed up in
North Queens. They had been spreading across Nova
Scotia with the help of some introductions, and by the
late 1800s their numbers were increasing (Rand 1933).
There were many reasons for the increase. Possibly
the most decisive was the climatic warming that set in
about 1850 (Hawboldt 1952; Lamb 1982). The first
deer hunting season in Nova Scotia was in 1916 and by
the 1930s deer were common (Sheldon 1936; Benson
and Dodds 1977). Over 40 000 were reported killed in
Nova Scotia in one year in the early 1950s — more than
two for every square mile in the province (Benson and
Dodds 1977). Deer remained numerous until the unusu-
ally severe winter of 1955-1956 caused a major dieoff
of deer in western Nova Scotia. Since then they have
fluctuated with winter conditions.
Beavers, Castor canadensis, were not mentioned by
my father as a species that he encountered in North
Queens as a young man in the 1890s and the early
1900s. The animals had been trapped almost to extirpa-
tion in Nova Scotia during the preceding century. How-
ever, in 1907 Beavers were given complete protection
(Wood 1973) and the Department of Lands and For-
ests staff began live-trapping and transplanting them
from the few remaining populations to unoccupied
parts of the province.
One cold autumn dusk when I was about five years
old my father took me on a short walk to a small lake
where Beavers had been released. We saw a new dam
blocking the outlet stream and a new house with
fresh mud on it. The Beavers had made themselves at
home. They soon became abundant in North Queens
and remained so until after 1945. Limited trapping was
allowed after that time, reducing Beaver numbers and
the dense population of animals had reduced their food
supply along streams and lakes. However, Beavers have
continued to occur in substantial numbers in North
Queens (Wood 1973).
Hunting with hounds was a favourite activity of my
father and his friends. They hunted Red Foxes (Vulpes
vulpes) and what they referred to as “wildcats”. Most
of the cats were Bobcats (Lynx rufus) but my father
also described killing cats that were over six feet long
from rear toes to front toes when held up by their
hind legs. Those large, rangy animals were probably
Lynx. More (1873) stated that there were “lucifees”
(Loup cervier, Lynx) and “little lucifees” in Queens
County. However, the Lynx had become rare or extir-
pated by the 1930s (Rand 1933; Sheldon 1936) and
is now absent from the region (McCord and Cardoza
1982).
According to local tradition, there were no Striped
Skunks, Mephitis mephitis, in North Queens when the
area was first settled. The species is not mentioned by
More (1873) who, as a land surveyor, was very famil-
iar with the mammals of the region. It was said that
2004
sometime in the mid-1800s someone brought a dead,
frozen animal to a local blacksmith shop. None of the
farmers who happened to be there could identify it.
However, a few days later someone passed who had
worked in the United States and who identified it as a
skunk. By my father’s time skunks were common.
However, by the 1930s, skunks were gone, probably
due to an epidemic of distemper (Dodds 1969) but
the decline in agricultural land use may also have had
a negative impact on this animal of farms and forest
edge. They were found in Nova Scotia only along the
New Brunswick border but by the 1960s they had
once again begun to spread into central areas of the
province (Dodds 1969). None were present in Kejim-
kujik National Park in the early 1970s (Wood 1973).
However, in 2001 I observed a skunk near Ten Mile
Lake, in Queens County.
My father would have had difficulty in believing that
the howl of the Coyote (Canis latrans) could ever be
heard in North Queens. Yet in the 1970s Coyotes ar-
rived in Nova Scotia. In North Queens, the popula-
tion of White-tailed Deer in Kejimkujik National Park
was apparently reduced by Coyotes which were com-
monly seen along Park roads and heard on still nights
throughout the area (Patterson 1994). The impact of
Coyotes not only on deer but on competing Red Foxes,
on Snowshoe Hares (Lepus americanus), microtine
rodents, grouse (Bonasa umbellus and Canachites can-
adensis) and other ground-nesting birds must have
been considerable.
Plants
Before the arrival of White-tailed Deer, the forest
floor in mature spruce-hemlock stands was carpeted
with Canada Yew, Taxus canadensis. This evergreen
shrub is highly palatable to deer and by the 1940s it
had been eliminated from the forest. In the 1960s one
experienced biologist (the late Harrison F. Lewis,
personal communication) told me that the only sur-
viving yew bush that he knew of was growing beside
the outhouse at a warden cabin where one branch had
grown through the wall of the well-ventilated facility
and had thus escaped browsing.
One of the most important trees of North Queens is
the White Pine (Pinus strobus) (Rowe 1972). White
Pines were a major resource in North Queens histori-
cally (More 1873). However, in my father’s time re-
generating White Pine was increasingly attacked by
the White Pine Weevil (Pissodes strobi). That insect
kills the leaders on the top of the tree, creating crooked
stems or, at worst, “cabbage trees” whose lower branch-
es continually grow up to take the place of the weevil-
killed central stem. White Pine Weevil is a native North
American insect. However, the first official records of
its presence in the Maritimes date from about 1920
(Martineau 1984). The insect quickly spread throughout
the range of the White Pine including North Queens.
The spread of the weevil was facilitated by the exten-
TELFER: CONTINUING ENVIRONMENTAL CHANGE — AN EXAMPLE 4|
sive areas of regenerating forest created by logging, fire
and the invasion of old fields by White Pine (Belyea
and Sullivan 1956). By my time the value of the White
Pine resource in North Queens was greatly reduced
and crooked, multi-stemmed pine occupied much space
in the forest. White Pine remains an important tree in
the district but the weevil attacks have reduced the
value of many stems for lumber.
The American Beech, Fagus grandifolia, was com-
mon in North Queens when my father was a boy. Pure
beech stands occupied the ridge tops and beech trees
were also scattered throughout the hardwood and
mixedwood stands. Beech nuts were always an impor-
tant seasonal food source for wildlife. Black Bears
(Ursus americanus), especially, sought them out for
a high fat and protein food before hibernation. When
whitetails arrived in Nova Scotia they quickly became
the most important consumers of the dwindling supply
of nuts. Loucks (1962) cited evidence that beech was
formerly more common in southwestern Nova Scotia.
He believed that wildfire had reduced the occurrence
of the species. Early in the 1900s the Woolly Beech
Scale (Cryptococcus spp.), an insect that spreads Beech
Nectria Fungus (Nectria coecinea var. faginata), ar-
rived in Nova Scotia, probably an accidental intro-
duction from Europe (Boyce 1961). The fungus gains
entry to the tree through holes made by the Woolly
Beech Scale. Saunders (1970) stated that Woolly
Beech Scale entered Nova Scoria from Europe about
1890 and that the fungus also entered North America
through Nova Scotia in about 1929. Nectria disease
debilitates beech by invading the bark and cambium,
eventually killing the tree. Roland and Smith (1969:
page 341) noted that “All the beech in N.S. is severe-
ly affected by the Nectria beech canker.” Most beech
in North Queens was unthrifty and dying by the mid-
twentieth century and in all cases moribund stems were
thoroughly infested with Nectria cankers. Beech have
declined substantially (Telfer 1971). They have been
replaced by species like Sugar Maple (Acer saccha-
rum) and Red Maple (Acer rubrum), Hemlock (Tsuga
canadensis) and Red Spruce (Picea rubens).
White Birch (Betula papyrifera) and Yellow Birch
(Betula alleghaniensis) were prominent trees in the
North Queens forest when my father was a boy. In-
deed the old farmhouse in which he was born and died
was sheathed with bark of the white birch between the
wallboards and the shingles. In the mid-1930s a die-
back was observed in the birch (Hawboldt 1952.
Mature stands all died. This phenomenon occurred all
over northeastern North America.
Temperatures were high in the 1930s following a
steady rise from Little Ice Age conditions that existed
before the 1850s (Hawboldt 1952). One hypothetical
cause of birch mortality was that the warming climate
altered the species composition of the mycorrhizal
flora in the soil to the detriment of species that could
enter into symbiotic relationships with birch roots
42 THE CANADIAN FIELD-NATURALIST
(Hawboldt 1952). Birch would thus have suffered from
nutrient deficiencies. Although birch regeneration sur-
vived, live mature trees were very scarce by my time.
One would have had to travel a long way to collect
enough bark to sheath a house. In the 1960s I worked
on forest inventories in a remote part of the District
where the mature forest had formerly been dominated
by a mixture of birches, Red Spruce and Hemlock
(Fernow 1912), but by then the birches were rotten
snags and Red Spruce, White Pine, Balsam Fir (Abies
balsamifera) and Red Maple were sprouting in the
gaps created by their death.
Arachnids
An invading organism that caused excitement in
North Queens in the mid-twentieth century was the
American Dog Tick (Dermacentor variabilis). Opinion
is divided on whether the ticks were relict in a small
area in Western Nova Scotia or if they were introduced.
One woodsman told me of encountering ticks along a
small section of the Tusket River, near the western
end of Nova Scotia, during a canoe trip early in the
1900s (the late F. M. Forrest, personal communi-
cation). The distribution pattern shown by Dodds et
al. (1969) suggests dispersion from an epicentre of
infection. The Tusket River flows through the area of
earliest distribution. By the 1930s loggers working in
the western part of North Queens began to complain
of tick bites. Ticks advanced on a broad front across
the district in the late 1940s and the 1950s, causing
consternation among the people who were unused to
them. Since the 1960s, American Dog Ticks have con-
tinued to spread eastward in Nova Scotia (Andrew
Hebda, personal communication).
Weather
Nova Scotia is on the track of the equatorial Atlantic
hurricanes. North Queens has been occasionally lashed
by at least the fringes of those storms. In 1939, the area
was hit by a hurricane that blew down many trees but
did limited damage in closed stands. However, in 1954,
a powerful hurricane, code named “Edna”, struck North
Queens (Hawboldt and Bulmer 1958). Mature and old
forests suffered particularly. Hurricane Edna was fol-
lowed by a campaign of salvage logging as landown-
ers tried to recover as much of the blowdown as pos-
sible. The forest openings were invaded by regeneration
of Red Spruce, Red Maple, White Pine and particu-
larly by Balsam Fir in place of the dominant Hemlock
of the former stands.
Prediction and Management
Causes of some of the observed changes were nat-
ural, like birch dieback and distemper, while others
were due at least in part to human intervention. There
were some introductions of White-tailed Deer to Nova
Scotia that probably accelerated their spread. Logging,
small farming and attendant wildfires no doubt in-
Vol. 118
creased the amount of suitable habitat for deer and also
the area occupied by White Pine regeneration, the
habitat of the White Pine Weevil. Hunting probably
hastened the extirpation of Caribou and Lynx and the
near extirpation of beaver. Coyotes may have been
able to invade eastern North America partly because
European settlers extirpated Grey Wolves, Canis lupus,
from regions to the west of Nova Scotia. Ticks and
the insect vector and the fungus involved in the beech
Nectria disease may have been accidentally introduced.
Climatic warming over the past 150 years interacted in
a complex way with other causes of ecological change.
The most important factors causing change to the
terrestrial biota in North Queens operated haphazardly.
Most were outbreaks of plant and animal diseases
and parasites. Unpredictable outbreaks of disease are
sometimes not considered to be very important by re-
newable resource managers simply because they are
random and basically unforeseeable. Also, the educa-
tion of resource managers usually focuses on other
topics. However, Hurricane Edna represented another
kind of random event. There was sufficient evidence
of the occasional occurrence of such severe hurricanes
that shrewd ecosystem managers would probably have
allowed for their possible occurrence when preparing
management plans.
The observed ecological changes in North Queens
did not damage basic ecological functions like produc-
tion, herbivory and predation. However, the suite of
species involved changed. White-tailed Deer to some
extent replaced Moose and Caribou as consumers
while Coyotes became important predators as Lynx
had been previously. After decades of absence, Beavers
were brought back in numbers by deliberate manage-
ment. Energy flow through the ecosystem was unim-
paired but flowed through somewhat different chan-
nels. The observed changes exemplify the fluidity and
unpredictability of nature (Botkin 1990).
What might have happened if, beginning in the
1890s, the forests and wildlife of North Queens had
been under a modern regime of ecosystem manage-
ment? Foresters might have made management plans
aiming at production of a steady supply of birch logs.
All would have been well for the first fifty years, then
they would have found that the birch growing stock
was dying and that spruce and fir were taking its place.
As time went on the beech would also have been lost
as a commercial species. Forest management would
have had to be altered, as it indeed was following Hur-
ricane Edna when managers were forced to revise their
thinking about harvesting techniques (Johnson 1986)
and deal with storm-caused openings and changes in
forest composition. Conversely, the patchy nature of the
storm-damaged forests provided improved habitat for
White-tailed Deer and Moose.
Wildlife managers would have found a major ungu-
late species, the Caribou, suddenly declining. Even if
the meningeal worm problem had been known, would
<2
2004
managers have tried solve it by exterminating the
White-tailed Deer population? Whitetails were by then
spread thinly over the entire province. By the time
Moose also declined there were so many deer that erad-
ication would have been impossible. Even without par-
asites, how would biodiversity managers have viewed
the invasion of exotic whitetails especially since they
were also the culprits in the extirpation of the Canada
Yew? Managers would have been largely helpless to
protect the yew except possibly by fencing small res-
erved patches. Although “ecosystem” preservation is
often a suitable management approach to maintain
threatened species, it would have been counterproduc-
tive in this case because old hemlock/spruce forest is
preferred winter habitat for whitetails as well as the
site of best yew growth (Schierbeck 1931). Lynx still
remain on Cape Breton Island so protection from hunt-
ing might have been adequate to recover the species
on the mainland of Nova Scotia as it did for the
Beaver. Because skunks appear to have died from dis-
temper, reintroduction of healthy animals following
the dieoff might also have re-established viable popu-
lations and prevented local extirpation.
Our hypothetical ecosystem managers would have
emerged from the hundred-year period somewhat bat-
tered. They would have lost a member of the charis-
matic megafauna, the Caribou. They would no doubt
have been chagrined by the fact that the district had
been overrun by the exotic White-tailed Deer and Coy-
otes, not to mention the obnoxious dog ticks. Some
major tree species would also have been drastically
reduced. However, a major understorey shrub and two
mammal species might have been rescued and one
mammal species, the Beaver, was indeed returned to
the area by management. Would the public consider
that money spent trying to maintain the ecosystems
as they were in the 1890s to have been well spent as
part of a worthwhile effort to “preserve” “nature” in
the region? Or would managers simply be seen as
having cast themselves in front of the juggernaut of
inevitable ecological change?
In the 1890s the coming changes and their impact
could not have been foreseen. If managers at that time
had set goals like doubling the sustainable harvest of
White Birch and developing an industry to use it, or
if they had set out to double the Caribou population to
satisfy outfitters, they would have been in for a rough
time. Yet, such factory-type production goals are often
set in resource management.
This example highlights the significance of scale
in biodiversity conservation. Would it have been worth-
while to try to keep species that are still common else-
where in North America, like Caribou, Lynx, Striped
Skunks, and Canada Yew, in the district or even in Nova
Scotia? At what price should we try to keep everything
that was present historically in a local or regional biota?
Or should the waxing and waning of species’ ranges
be accepted as inevitable?
TELFER: CONTINUING ENVIRONMENTAL CHANGE — AN EXAMPLE 43
Although such a comprehensive management ap-
proach would have been unthinkable in the 1890s, a
program of adaptive management (Walters 1986) would
have been appropriate. With the adaptive model in
mind, managers might have been aware of the likeli-
hood of natural variability and therefore cautious in
goal setting. They could have initiated a program of
monitoring that might have picked up changes in spe-
cies status in their early stages when some prediction
of the magnitude of upcoming impacts could have been
made. While little could have been done to change the
course of events in the short term, a more comprehen-
sive and quantitative understanding of the operation of
nature might have led to effective interventions later
on.
The haphazard nature of the changes in the ecology
of North Queens during the past hundred years under-
lines the difficulty of predicting what will happen next
in nature. One is reminded of the soldier’s axiom re-
garding shellfire, “You won’t hear the one that gets
you”. The example of North Queens demonstrates the
inevitability of environmental change and emphasizes
the value of a flexible approach to forest and wildlife
management.
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al Park. Proceedings of the Nova Scotia Institute of Sci-
ence 27: 43-58 (1971-1973).
Received 15 February 2002
Accepted 24 June 2004
Habitat Segregation Among Songbirds in Old-Growth Boreal
Mixedwood Forest
ENID E. CUMMING
1542 Empress Ave., Saskatoon, Saskatchewan S7K 3G3 Canada
Cumming, Enid E. 2004. Habitat segregation among songbirds in old-growth boreal mixedwood forest. Canadian Field-
Naturalist 118(1): 45-55.
The foraging behaviour of ten species of insectivorous songbirds — Boreal Chickadee (Poecille hudsonicus), Golden-crowned
Kinglet (Regulus satrapa), Ruby-crowned Kinglet (R. calendula), Blue-headed Vireo (Vireo solitarius), Tennessee (Vermivora
peregrina), Blackburnian (Dendroica fusca), Magnolia (D. magnolia), Yellow-rumped [Myrtle] (D. coronata), Black-throated
Green (D. virens), and Bay-breasted (D. castanea) warblers — was observed in the boreal mixedwood forest of Prince Albert
National Park in central Saskatchewan. Birds segregated their habitat use by preferentially foraging in different tree species,
and through preferential use of different foraging locations (height and position) within trees.
White Spruce (Picea glauca) was used more than expected by Yellow-rumped Warblers, and Golden-crowned and Ruby-crowned
kinglets. Tennessee and Magnolia warblers used White Birch (Betula papyrifera), more than expected and Boreal Chickadees
and Blue-headed Vireos used Balsam Fir (Abies balsamea) more than expected. Boreal Chickadees, Ruby-crowned Kinglets,
and Tennessee, Blackburnian and Yellow-rumped warblers all used the bottom part of trees less than expected, while Blue-
headed Vireos foraged near the top of trees less than expected. Large inner branches were avoided by Tennessee, Blackburnian
and Yellow-rumped warblers, while Bay-breasted Warblers and Blue-headed Vireos avoided small outer twigs. In conifers,
Blackburnian Warblers foraged significantly higher in the trees than all other species except Black-throated Green and Bay-
breasted warblers. Blackburnian Warblers also foraged significantly higher than Blue-headed Vireos and Magnolia Warblers
in deciduous trees.
Key Words: Songbirds, behaviour, foraging, boreal forest, old-growth, Prince Albert National Park, Saskatchewan.
Behavioural interactions and niche partitioning in
songbirds have received much attention in the literature
(MacArthur 1958; Sabo 1980; Maurer and Whitmore
1981). For many boreal songbirds, however, much on
their basic biology remains poorly understood (Sodhi
and Paszkowski 1995). Many of the detailed behavioral
descriptions have come from studies conducted in the
New England States (Rabenold 1978; Robinson and
Holmes 1982; Hunt and Flaspohler 1998). This is like-
ly an incomplete description for some birds, as several
of the species discussed have their breeding ranges
almost entirely restricted to the Canadian boreal forest
(Ficken et al. 1996; Rimmer and McFarland 1998).
Studies on the southern fringes of the boreal forest, in
Maine or Minnesota, are not adequate on their own to
understand boreal ecology as many of the plant and ani-
mal species are not the same as further north (Rowe
1972; Acton et al. 1998). Even for wide-ranging species,
there is evidence that birds do not behave the same
way and do not use the same kind of habitat in all parts
of their range (Noon et al. 1980; Collins 1983; Robi-
chaud and Villard 1999).
Recent studies in the boreal forest have focused on
habitat associations, and habitat requirements of song-
birds (Schieck et al. 1995; Kirk et al. 1996). This infor-
mation is urgently needed in light of increased pressure
from large-scale forestry in this region (Cummings et
al. 1994). There is mounting evidence to show that
mature and old boreal mixedwood forest support an
entirely different suite of species not found in younger
age classes (Stelfox 1995; Cumming and Diamond
2002). These older age classes of forest are currently
under a harvesting intensity that is disproportionate to
their abundance in the landscape (Cummings et al.
1994; Weyerhaeuser 1998*).
The goal of this project was to investigate details of
within-stand habitat segregation among boreal song-
birds, focusing on the foliage-gleaning songbird guild
of old (>120 years) boreal mixedwood forest. This type
and age of forest was chosen as it was biologically the
most diverse and structurally the most heterogeneous
habitat in the region (Erskine 1977; Johnson et al. 1995:
Robichaud and Villard 1999). In addition, mature to old
(80+ years), mixedwood forest will become increas-
ingly rare at the landscape level if current land use
practices (i.e., logging, oil and gas exploration and agri-
culture) continue at their present rate (Cummings et
al. 1994: Hobson et al. 2002; Schneider et al. 2002*).
Study Area
This study was carried out in the boreal, mixedwood
forest of Saskatchewan (Kabzems et al. 1986; Acton
et al. 1998), in Prince Albert National Park (53°35'N,
106°00'W) during 1990 and 1991 (see Bayne and
Hobson 1997 for description). Three sites were chosen
in forest stands that were >40 ha in area and >120 years
old. Sites were as similar in topography and vegetative
cover as field conditions allowed. Stands were aged
by forest inventory maps, and by taking core samples
from six of the largest trees on each site. Each study
45
46 THE CANADIAN FIELD-NATURALIST
site was surrounded by continuous forest of similar
type, but younger age. None of the study sites had been
subjected to forest harvesting, and wildfire was the
driving force behind forest succession in this area
(Weir et al. 2000).
The study sites were structurally very heterogeneous,
with many tree-fall gaps and many standing dead trees.
These canopy gaps allowed for regeneration, which
resulted in a wide range of tree sizes and ages. Domi-
nant tree species were White Spruce, Picea glauca,
Balsam Fir, Abies balsamea, and Trembling Aspen,
Populus tremuloides, with scattered White Birch, Betula
papyrifera. Average canopy height was 21 metres with
a maximum height of 38 metres (Cumming 1995).
White Spruce was the only species that reached heights
of over 30 metres, with some specimens also having
diameters in excess of one metre. Understory trees (<12
metres), were mainly Balsam Fir, while the main
shrubby species were Balsam Fir, White Birch sap-
lings, and Alder, A/nus sp. Shrub distribution was
patchy, with dense patches occurring in tree-fall gaps,
and scattered shrubs in the rest of the study area. The
most abundant ground cover species were various
mosses, Bunchberry (Cornus canadensis), Wild Sarsa-
sparilla (Aralia nudicaulis), Ostrich Fern (Matteuccia
struthiopteris) and several horse-tail species (Equi-
setum Spp.).
Methods
Observations on bird behaviour took place from
late May to early August in 1990 and 1991, and birds
were observed between 04:00 (dawn) and 21:00
(dusk). Upon locating a focal bird, continuous obser-
vations were made using binoculars until the bird
was lost from sight (Altman 1974; Martin and Batson
1986). To avoid possible biases, observations that last-
ed less than five seconds or longer than two minutes
were not used in the analysis. Bird species, behaviour,
tree species and bird position in the tree were record-
ed. Bird height was estimated to within three metres.
Linear regression analysis (Zar 1996) was used to
ensure that estimates accurately reflected clinometer-
measured heights (Cumming 1995).
In addition to behavioural observation, unlimited
distance point counts (Bibby et al. 1982) were con-
ducted twice during the breeding season (June), in
order to estimate relative abundances of the various
bird species. The average number of individuals per
point count for each bird species was obtained by taking
the maximum number recorded for that species and
dividing by the number of point counts. Data from the
three sites were pooled and used as a relative index of
abundance for the study as a whole. For more details
on bird species abundances see Cumming and Diamond
(2002).
Following the method of MacArthur (1958), con-
ifers were divided into 15 zones; 5 vertical and 3 hori-
zontal, to determine in which part of the tree birds were
foraging (Figure 1). Vertical zones divided the tree into
Vol. 118
fifths, with zone | at the top and zone 5 at the bottom.
Horizontal zones corresponded to the outer part of the
branch with new growth, fresh needles and small twigs
(zone T), the middle layer of older needles and larger
branches (zone M), and the inner part of the branch,
largely devoid of needles with large diameter branches
(zone B). A similar system was used for deciduous
trees except they were divided into three vertical zones
due to their more globular shape (Figure 2).
Although many birds exhibit male-female foraging
differences (Holmes 1986), data for both sexes were
pooled since the focus of the study was on interspecific
differences in habitat use and because some species
in the study were not sexually dimorphic. Bird foraging
behaviour (tree zone use), did not differ significantly
between the two species of conifer or between the two
species of deciduous trees. Therefore, data for each
bird species was pooled based on either coniferous or
deciduous trees (Cumming 1995).
Vegetation in the study areas was measured using
a modified James and Shugart (1970) method. Ten
0.04 ha circles (22 m diameter) were established in
each study area, one centered on each of five point
count stations and one at 50 metres in a random direc-
tion from that point. Within each circle, species, height
in meters and diameter at breast height (dbh) in cm for
all trees larger than 7 cm dbh were recorded. Percent
basal area for each tree species was calculated using
dbh values. Basal area more accurately reflected tree
availability to birds than numbers of trees, due to
heterogeneity in tree size.
To check for possible visibility biases in the various
tree species, simultaneous confidence intervals (Chi-
squared with Bonferroni confidence intervals) were
constructed by pooling the number of seconds of ob-
servation for all bird species (Byers et al. 1984).
Simultaneous confidence intervals were also used to
assess whether birds preferred or avoided certain tree
species. Chi-squared test with Yates correction (Zar
1996) were used post priori to determine if birds had
a preferred foraging zone within trees. Foraging diver-
sity was analyzed using the Shannon Index (Shannon
and Weaver 1949). To assess niche overlap between
species, the proportion of observations each bird
species spent in each of the 15 possible tree zones (9
zones in deciduous trees) was compared between each
species pair using Morisita’s Index of overlap (see
Diamond 1983). With this index, potential niche over-
lap can vary from | (complete overlap) to 0 (no over-
lap). Foraging height data were analyzed using a 1-
way Anova (Proc GLM; SAS Institute 1988), and the
results subjected to a Tukey’s HSD pair-wise com-
parison test (with P=0.05).
Results
Tree Species Preference
By basal area, White Spruce, Balsam Fir, Trembling
Aspen and White Birch comprised 46%, 30%, 20%,
and 4%, respectively, of the available arboreal habitat.
2004 CUMMING: HABITAT SEGREGATION AMONG SONGBIRDS 47
BOCH
(N=128)
H=2.25
@ 10- 14.9% [ 5.9.9% LI 0- 4.9%
FiGuRE 1. Songbird use of zones in coniferous trees. Shadings indicate frequency of observations within a zone (see
legend). N= number of observations, H= Shannon diversity index. See Table 4 for species abbreviations.
48 THE CANADIAN FIELD-NATURALIST
White Spruce was used more than expected by
Yellow-rumped (Myrtle) Warblers, (Dendroica coro-
nata), Golden-crowned (Regulus satrapa) and Ruby-
crowned (R. calendula) kinglets and in proportion to
its availability by all other species (Table 1). Balsam
Fir was used more than expected by Boreal Chicka-
dees (Poecile hudsonicus) and Blue-headed Vireos
(Vireo solitarius) but less than expected by Tennessee
Warblers (Vermivora peregrina). White Birch was
used more than expected by Tennessee and Magnolia
(Dendroica magnolia) warblers, while Trembling Aspen
was used less than expected by Boreal Chickadees,
Golden-crowned and Ruby-crowned kinglets, Blue-
headed Vireos, Yellow-rumped and Magnolia war-
blers (Table 1). Bay-breasted Warblers (Dendroica
castanea) used all tree species in proportion to their
availability; however, they did exhibit a tendency to
prefer White Spruce and avoid White Birch that was
approaching significance. Blackburnian (D. fusca) and
Black-throated Green (D. virens) warblers were not
tested due to insufficient sample size (Brennan and
Morrison 1990).
Point counts
All ten species were found in all three study sites,
except Black-throated Green Warbler, which only oc-
curred in one of the three study sites. Average bird
abundance per point count from most to least abundant
was; Magnolia Warbler (1.2), Yellow-rumped Warbler
(0.8), Bay-breasted and Tennessee warblers (0.7),
Blackburnian Warbler and Ruby-crowned Kinglet (0.4),
Blue-headed Vireo (0.3), Boreal Chickadee and Gol-
den-crowned Kinglet (0.2) and Black-throated Green
Warbler (0.1).
Foraging Zones
In coniferous trees the most diversely foraging spe-
cies (in order) were Yellow-rumped Warblers, Ruby-
crowned Kinglets, Magnolia Warblers, and Boreal
Chickadees (Figure 1). These species were observed in
most tree zones and had the highest diversity indices
(Shannon and Weaver 1949). The least diversely forag-
ing species were Black-throated Green Warblers, Black-
burnian Warblers and Blue-headed Vireos (Figure 1).
Vol. 118
In the vertical zones, Ruby-crowned Kinglets, and
Tennessee and Yellow-rumped warblers used the
bottom of the tree, less than expected, while Boreal
Chickadees and Golden-crowned Kinglets used the
top and bottom less than expected (Table 2). Black-
burnian and Bay-breasted warblers used the bottom
two zones less than expected, while Blue-headed Vireos
used the top two zones less than expected (Table 2).
For the horizontal zones Bay-breasted Warblers and
Blue-headed Vireos both used small twigs on the
ends of branches (zone T) less than expected, while
Tennessee and Blackburnian warblers used small
twigs (zone T) more than expected (Table 2). Yellow-
rumped Warblers use large inner branches (zone B)
less than expected, while Boreal Chickadees, Golden-
crowned and Ruby-crowned kinglets and Magnolia
Warblers showed no significant difference in their use
of inner and outer branches. Black-throated Green
Warblers were not tested due to insufficient sample
size (Brennan and Morrison 1990). In deciduous trees,
only six of the ten species had a large enough sample
size to test foraging zone use (Figure 2). In deciduous
trees, Blackburnian Warblers used the top of the trees
more than expected. Yellow-rumped, Magnolia and
Blackburnian warblers used zone B less than expected,
and Tennessee Warblers used zone T more than ex-
pected (Table 2).
Niche Overlap
In conifers, niche overlap varied from 0% between
Blue-headed Vireos and Blackburnian Warblers to
95% between Yellow-rumped Warblers and both
Magnolia Warblers and Boreal Chickadees The four
most diversely foraging species, Boreal Chickadees,
Ruby-crowned Kinglets, and Yellow-rumped and Mag-
nolia warblers, all overlapped each other by >80%.
In deciduous trees, the most foraging overlap was
between Yellow-rumped and Blackburnian warblers
and between Magnolia and Tennessee warblers; both
species pairs overlapped by 88% (Table 3). The least
amount of overlap in deciduous trees (40%), was be-
tween Black-throated Green and Bay-breasted warblers.
TABLE |. Bird use of different tree species compared to the tree’s availability (y? test with Bonferroni confidence intervals,
DF=3 for all species).
Use
Bird Species
Boreal Chickadee
Golden-crowned Kinglet
> Expected
Balsam Fir
White Spruce
Ruby-crowned Kinglet White Spruce
Blue-headed Vireo Balsam Fir
Tennessee Warbler White Birch
Magnolia Warbler White Birch
Yellow-rumped Warbler White Spruce
Bay-breasted Warbler -
Significance: *< 0.05, **<0.01, ***<0.001
< Expected ye Pp
Trembling Aspen 43.3 ss
Trembling Aspen 10.1 A
Trembling Aspen 529 :
Trembling Aspen 6.3 ‘i
Balsam Fir 50.7 tte
Trembling Aspen 10.9
Trembling Aspen DAD Ee
= 5.0 n.s.
2004 CUMMING: HABITAT SEGREGATION AMONG SONGBIRDS 49
YRWA MAWA
(N=54) (N=64)
H=1.85 H=1.85 H=1.90
BLBW
(N=53)
H=1.91 H=1.35 H=1.25
FiGure 2. Songbird use of zones in deciduous trees. Shadings indicate frequency of observations
within a zone (see legend). N= number of observations, H= Shannon diversity index.
See Table 4 for species abbreviations.
Foraging Height average foraging height of Blackburnian Warblers was
In coniferous trees, the average foraging height of
Blackburnian Warblers was significantly higher than
all other species except Black-throated Green and Bay-
breasted warblers (Table 4). Black-throated Green
and Bay-breasted warblers both foraged significantly
higher than Magnolia Warblers and Blue-headed Vir-
eos. Foraging heights of all other species were not sig-
nificantly different (Table 4). In deciduous trees, the
significantly higher than that of Blue-headed Vireos
and Magnolia Warblers but not significantly different
from other species.
Canopy vs. Subcanopy Use
Blackburnian, Black-throated Green, and Tennessee
warblers were seen in canopy level trees (>12 metres)
in two-thirds or more of all observations (Table 5). At
the other extreme, two-thirds of the observations on
50
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 2. Bird use of tree zones where zone use was significantly more or less than expected (x? test with Yates’s correction;
DF=!1 for all species).
Species Horizontal Zones
T,M,B Use OG
In Coniferous Trees
Boreal Chickadee n.s
Golden-crowned Kinglet ns.
Ruby-crowned Kinglet ns.
Blue-headed Vireo at < 20.9
Tennessee Warbler al > 14.9
Blackburnian Warbler ay > 18.5
Magnolia Warbler ns.
Yellow-rumped Warbler B < 14.6
Bay-breasted Warbler at < 10.5
In Deciduous Trees
Tennessee Warbler T > 30.3
Blackburnian Warbler B < 24.9
Magnolia Warbler B < 155
Yellow-rumped Warbler B < 233)
Vertical Zones
IP 1 to5 Use Ye RB
sD) < 20.4 nce
We) < 14.5 cae
5 < 16.5 sats
a Ie) < 1h oe
Fata 5 < ig? “ook
nas 4,5 < 7.4 mee
3 > 13.7 ie
cates 3) < 10.1 ar
ae 4,5 < 7.5 ne
eae ns.
se I > 6.6 *
eae ns.
bt n.s.
Significance: *< 0.05, **<0.01, ***<0.001; T = outer part of branch with new growth, fresh needles and small twigs; M =
middle layer of older needles and larger branches; B = inner part of branch, largely devoid of needles with large diameter
branches; | to 5: vertical zones, 1 = top, 5 = bottom.
TABLE 3. Average (mean + SD) foraging height (metres) in
coniferous and deciduous trees. Species marked with * for-
aged significantly higher than other species (1-way Anova
with Tukey’s HSD test, P=0.05).
Bird Species Coniferous Deciduous
Boreal Chickadee 6.1 + 3.4 ONS: 2
Golden-crowned Kinglet TOE 229 ODES al
Ruby-crowned Kinglet 7.3+44.7 9.5+4.7
Blue-headed Vireo 6.1+2.0 6.3+3.8
Tennessee Warbler SiOFE SE 5S) aed]
Blackburnian Warbler esi Bel /a3) ay Thee Spoke
Magnolia Warbler DR) Baa 6.9 +5.0
Black-throated Green Warbler 12.7 + 7.8* 11.44+3.8
Yellow-rumped Warbler 7.0+4.2 NIMs Site)
Bay-breasted Warbler 10.3 + 4.8* loves Shs
Coniferous: Blackburnian Warbler foraged significantly high-
er than all but Black-throated Green Warbler and Bay-breasted
Warbler. Black-throated Green Warbler and Bay-breasted War-
bler foraged significantly higher than Blue-headed Vireo and
Magnolia Warbler.
Deciduous: Blackburnian Warbler foraged significantly high-
er than Blue-headed Vireo and Magnolia Warbler.
Magnolia Warblers and Boreal Chickadees were in
subcanopy trees (Table 5). Blue-headed Vireos and
Ruby-crowned Kinglets were approximately equal in
their use of canopy and subcanopy trees, while Golden-
crowned Kinglets and Yellow-rumped and Bay-breast-
ed warblers tended to be observed slightly more often
in canopy level trees (Table 5). Yellow-rumped Warblers
were observed in canopy level trees significantly more
than Magnolia Warblers (Z=5.2, P<0.001) and Boreal
Chickadees (Z=3.4, P<0.001).
Discussion
Tree Species Preference
The four main tree species in the study area (White
Spruce, Balsam Fir, Trembling Aspen, and White
Birch), were not equally abundant, nor equally large
(Cumming 1995). If abundance alone had been used
as the criteria for tree availability for foraging then
Balsam Fir would have appeared to comprise a larger
proportion of available habitat than it actually did.
Patches of old, White Spruce-dominated forest are
relatively rare in Saskatchewan (Kabzems et al. 1986;
Acton et al. 1998); therefore, it was expected that
birds which prefer White Spruce would selectively
occupy this habitat. The data appear to support this,
as all species in the study used White Spruce either in
proportion to, or greater than, its abundance. Yellow-
rumped Warblers and Golden-crowned and Ruby-
crowned kinglets all used White Spruce more than
expected. Boreal Chickadees and Blue-headed Vireos
used White Spruce in proportion to its abundance and
used Balsam Fir more than expected. All five species
used Trembling Aspen less than expected (Table 1).
This is similar to their behaviour elsewhere, as other
researchers have found these five species to be conifer
specialists (Keast and Saunders 1991; Ingold and
Wallace 1994; Ingold and Galati 1997).
Trembling Aspen was the least favored tree; it was
used less than expected by half the bird species in the
study. Previous research has suggested differences in
insect abundance may exist between aspen and other
tree species (Ives and Wong 1988). Holmes and Robin-
son (1981) suggested structural characteristics of aspen
trees and their leaves may impede foraging by insec-
tivorous birds. However, Greenburg (1979) felt that
Yellow-rumped and Bay-breasted warblers were phys-
5]
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2004
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Sy THE CANADIAN FIELD-NATURALIST
TABLE 5. Bird use of canopy versus subcanopy trees, from
most to least canopy using species.
Number of Observations
Bird Species Canopy Subcanopy
Blackburnian Warbler 62 ii
Black-throated Green Warbler iL) 5
Tennessee Warbler 80 41
Yellow-rumped Warbler 94 63
Bay-breasted Warbler 73 55
Golden-crowned Kinglet 16 12
Ruby-crowned Kinglet Dil, 25
Blue-headed Vireo 24 25
Boreal Chickadee 29 50
Magnolia Warbler 60 126
ically adapted to foraging in conifers and both their
body size and foraging habits impeded foraging in
deciduous trees.
Tennessee and Magnolia warblers both used White
Birch more than expected. Morse (1989) felt that
many songbirds preferred various Betula species for
mechanical reasons; they had smaller leaves than other
trees (especially Fagus, Acer and Populus) and were
easier for gleaning songbirds to reach. Other studies
have found various species of birch have higher den-
sities of lepidopteran larvae than other trees (Holmes
and Robinson 1981; Holmes and Shultz 1986). An
insufficient sample size prevented testing of Black-
throated Green Warbler’s tree species preference. It is
notable, however, that 50% of the foraging observa-
tions on this species were in White Birch, even though
these trees represented only 4% of the available habitat.
Other researchers (Holmes and Robinson 1981; Robi-
chaud and Villard 1999) have also found that Black-
throated Green Warblers are partial to birch and use
it greater than expected by chance alone.
Tennessee Warblers used Balsam Fir less than ex-
pected, while Blackburnian and Black-throated Green
warblers were never observed in this tree. Although
Blackburnian and Black-throated Green warbler use
of this tree could not be tested, the fact that Balsam
Fir comprised 30% of the available trees suggests
that both birds were avoiding it. Blackburnian and
Black-throated Green warblers were consistently ob-
served high in the canopy, so Balsam Fir with an
average height of 11 + 5.6 metres may have been too
short to attract these species (Cumming 1995). Branch
structure may also have played a role in some birds’
avoidance of fir. Differences in branch shape have been
attributed to several bird species’ preference of Red
Spruce (Picea rubens) over White Spruce (Morse
1989; Parrish 1995). Balsam Fir branches were less
ridged than those of White Spruce (personal observa-
tion). Birds which preferentially foraged on thin outer
twigs appeared to have more difficulty foraging on the
tips of Balsam Fir branches than they did in White
Vol. 118
Spruce (personal observation). This was particularly
noticeable in Tennessee Warblers because this species
focused most of its foraging activities on the outer
twigs and new growth in both coniferous and decid-
uous trees. In contrast, birds which foraged in many
tree zones (Yellow-rumped, Magnolia, and Bay-breast-
ed warblers) appeared to be less affected by branch
structure and they used Balsam Fir in proportion to
its availability.
Foraging
Boreal Chickadees were the only permanent resi-
dents in the study and one of the few passerines that
are resident in the boreal forest (Ficken et al. 1996). It
is considered an advantage for birds to be flexible in
their foraging habits when they live in an unpredic-
table environment, like the boreal forest (Hunt and
Flaspohler 1998). Boreal Chickadees were diverse
foragers, using most tree zones and overlapping more
than 80% with Ruby-crowned Kinglets and Yellow-
rumped, Magnolia, Bay-breasted and Tennessee warb-
lers. Other studies found Boreal Chickadees had an
average foraging height of five metres, and used all
parts of the tree branch (Sabo and Holmes 1983;
Ficken et al. 1996). Similarly, I found Boreal Chicka-
dees foraged at an average height of six metres and
showed no significant difference in their use of inner
and outer branches. They did however, use the top
and bottom of trees less than expected. Boreal Chick-
adees may have avoided the tops of trees because this
zone was heavily used by several other species. Boreal
Chickadees have been shown elsewhere to shift their
foraging activity lower in the trees due to competition
from Black-capped Chickadees (Vassallo and Rice
1981). Boreal Chickadees also tended to forage in
small subcanopy trees more than any other species
except Magnolia Warblers.
Ruby and Golden-Crowned kinglets were similar
in their behaviour; however, Ruby-Crowned Kinglets
were usually higher in the trees and were more diverse
foragers. Rabenold (1978) found that where Ruby-
crowned Kinglets and Golden-crowned Kinglets oc-
curred together, Ruby-crowned Kinglets were more
diverse in their foraging activity and occurred higher
in the canopy than Golden-crowned Kinglets. Franz-
reb (1984) felt this was due to social dominance of
Ruby-crowned over Golden-crowned kinglets. No
interspecific social interactions were observed in this
study; however, Ruby-crowned Kinglets were twice
as abundant as Golden-crowned Kinglets and may
have influenced the behaviour of the latter through
numerical dominance.
Large inner and middle branches were favoured by
both Blue-headed Vireos and Bay-breasted Warblers;
this was an area of the trees that was seldom used by
other species. There was only moderate foraging over-
lap (47%) between Blue-headed Vireos and Bay-
breasted Warblers, as they foraged at significantly dif-
ferent heights. Foraging on large inner and middle
2004
branches is similar to the behaviour these two species
have displayed elsewhere (Williams 1996; James 1998).
Both Blackburnian and Black-throated Green war-
blers foraged high in the trees (significantly higher than
most other species), and had larger foraging overlap
with each other (85%) than they did with any other
species. These warblers appeared to be specialized in
a tree-top niche, and have been identified in many stud-
ies as feeding, singing, and nesting high in conifer-
ous trees (Morse 1993, 1994). Indeed, Morse (1994)
found that Blackburnian Warblers were unlikely to
be found in forest without at least some conifers over
18 metres tall. Unlike MacArthur (1958) and Morse
(1989), I found no evidence that Black-throated Green
Warblers were socially dominant over any other spe-
cies in the study area. This may have been because
Black-throated Green Warblers were the least abundant
bird in the study and only occurred in one of three
study sites.
Similar to their behaviour elsewhere, Tennessee
Warblers were observed at a variety of heights in all
tree species, but foraged mainly on the terminal foli-
age (Rimmer and McFarland 1998). Foraging on the
tips of the branches and using many different trees
may help Tennessee Warblers (a Vermivora warbler)
fit into a community (spruce-fir forest) that already
has several coexisting species of Dendroica warblers
(Morse 1989). Tennessee Warblers also used White
Birch more than any other species except Magnolia
and Black-throated Green warblers. Greenburg (1979)
felt that small warblers were better able to forage on
deciduous foliage than larger warblers for the physical
reasons. Tennessee, Magnolia and Black-throated Green
warblers were smaller than most species, except for
the two kinglets, and Boreal Chickadees, which were
conifer specialists. Therefore, they may have been
using a food resource that the larger Yellow-rumped
and Bay-breasted warblers would have trouble
exploiting.
I found Magnolia Warblers used subcanopy trees
more than any other species and had the lowest aver-
age foraging height of all species observed. This was
similar to Hall (1994), who found Magnolia Warblers
used mainly young conifers and were seldom found
at any great height. Magnolia Warblers displayed no
significant difference in their use of inner, middle and
outer parts of branches. This was likely because they
most often foraged young trees; there was far less
difference in branch structure between inner and outer
parts of branches in young trees than there was in large
old trees (personal observations).
Yellow-rumped Warbler showed the greatest diver-
sity of foraging habits. They used almost every tree
zone in both coniferous and deciduous trees. Yellow-
rumped Warblers have been noted elsewhere as being
generalists and this flexibility is thought to help them
withstand adverse conditions better than their con-
geners (Rabenold 1978; Hunt and Flaspohler 1998).
Unlike their behaviour elsewhere (MacArthur 1958;
CUMMING: HABITAT SEGREGATION AMONG SONGBIRDS 53
Morse 1989), Yellow-rumped Warblers did not use
mainly the bottom and inner branches. Yellow-rumped
Warblers occurred most often in the middle and outer
branches at mid to upper heights in both conifers and
deciduous trees, the same zone frequented by Black-
throated Green Warblers in other studies (MacArthur
1958; Morse 1989). Morse (1971) and Howe (1979)
felt that the presence or absence of Black-throated
Green Warblers caused shifts in Yellow-rumped War-
bler foraging activity. I observed no social interactions
between Yellow-rumped and Black-throated Green
warblers, and as Yellow-rumped Warblers were eight
times more abundant, there was likely little interspe-
cific competition between these two species. Indeed,
Yellow-rumped Warblers experienced the most overlap,
and likely the most interspecific competition, from
Magnolia Warblers, Boreal Chickadees, and Ruby-
crowned Kinglets (Table 4 and Figure 1).
Niche Overlap
Northern regions, such as the boreal forest, are
thought to have such large pulses of seasonally avail-
able food that for songbirds food saturation occurs
(Rabenold 1983; Wiens 1989). This seasonal pulse of
food, combined with a high number of neo-tropical
migrants, allows greater niche overlap between song-
birds than occurs in other habitats (Rabenold 1978,
1983; Wiens 1989). Rabenold (1978) found that spruce-
fir forests in particular had a high number of songbirds
which were “...broadly overlapping congeners”.
Although the present study and Rabenold’s were not
directly comparable, many of the species were the same
between the two studies and results from this study
support his theory of generalist stacking. Species with
the most generalized foraging behaviour had the high-
est amount of niche overlap, while those with more
specialized foraging behaviour had little niche overlap.
Canopy vs. Subcanopy
Availabilty of canopy versus subcanopy trees was
not measured; therefore, I could not test whether birds
were significantly selecting one over the other. At the
two extremes, however, it was apparent that Black-
burnian Warblers were using very tall trees almost
exclusively, while Magnolia Warblers were using most-
ly young regenerating trees.
I tested Yellow-rumped Warblers’ use of canopy and
subcanopy trees against Magnolia Warblers’ and Boreal
Chickadees’ because they had a 95% foraging overlap
(in conifers) with both species (83% with Magnolia
Warbler in deciduous trees). A Z-test (in results) found
Yellow-rumped Warblers used tall (canopy) trees sig-
nificantly more than the other two species. I felt this
was a significant difference between these species, as
they used the available habitat in a similar way and
they did not forage at significantly different heights.
Magnolia and Yellow-rumped warblers were also the
two most abundant species in study.
Previous research has shown old-growth boreal
mixedwood forest such as those studied here to harbor
54 THE CANADIAN FIELD-NATURALIST
unique communities not seen in pre-rotation age forest
(Erskine 1977; Kirk et al. 1996: Cumming and Dia-
mond 2002). This diverse songbird community appears
to be caused by an interaction between a structurally
diverse habitat and a mixture of generalized and specil-
ized foraging behaviours of the bird species involved.
Although this study did not examine multiple age class-
es of forest, it would appear that the community dyna-
mics seen here may be fairly unique due to canopy gap
dynamics that tend to be associated with old-growth
forest (Hunter 1990). This type and age-class of forest
has not received the attention it deserves from either
environmental impact studies or long-term manage-
ment plans for the boreal forest. The scientific commu-
nity needs to pay greater attention to the contribution
old-growth boreal mixedwood forest makes to bio-
diversity on both a regional and national scale.
Acknowledgments
This study was carried out in partial fulfillment of
the requirements for a M.Sc. degree at the University
of Saskatchewan. Parks Canada allowed field work to
be carried out in Prince Albert National Park. Funding
was provided by the Canadian Wildlife Service, Prince
Albert National Park, Nature Saskatchewan, and the
Saskatchewan Wildlife Habitat Development Fund.
Office, laboratory and computer space was provided
by the Canadian Wildlife Service in Saskatoon. A spe-
cial thank you to my husband S. L. Van Wilgenburg
for help with tables and figures and to my supervisor
A. W. Diamond for advice and support during thesis
research and preparation. This manuscript was im-
proved by helpful comments from S. L. Van Wilgen-
burg, K. A. Hobson, and A. J. Erskine.
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Received 10 March 2001
Accepted 20 May 2004
Effects of Mid-winter Snow Depth on Stand Selection by Wolverines,
Gulo gulo luscus, in the Boreal Forest
JONATHAN D. WRIGHT! and JEssICA ERNST
Ernst Environmental Services, Box 753, Rosebud, Alberta TOJ 2T0 Canada
Present address: Box 648, East Coulee, Alberta TOJ 1BO Canada
Wright, Jonathan D., and Jessica Ernst. 2004. Effects of mid-winter snow depth on stand selection by Wolverines, Gulo gulo
luscus, in the boreal forest. Canadian Field-Naturalist 118(1): 56-60.
Wolverines (Gulo gulo luscus) in a study area in the boreal upland forests of northwestern Alberta and northeastern British
Columbia (approximately 57°N) were noted to be limited to upland landscapes, despite abundant food in adjacent lowland
landscapes. Snow-tracking suggested that the species was selecting for the densest climax conifer stands for travel in search of
food. It was hypothesized that snow depth was a limiting factor for Wolverines in the boreal forest during midwinter, and that
they selected for this stand-type because of the buffering effect of this type of canopy on ground snow-depths. A series of
snow-depth measurements were collected. Snow depths collected along Wolverine trails were very significantly lower than
random snow depths collected under upland canopy (F = 32.84, df = 1, P << 0.010). There was a significant buffering effect
on snow depth indicated for upland canopy (F = 11.1, df = 1, P < 0.010), while adjacent lowland canopy had no significant
buffering effect on snow depth (F = 3.45, df = 1, P > 0.05). Wolverines were hypothesized to be limited to upland landscapes
in the study area because of the buffering effect on snow-depth of the stand types found there, and not for reasons of food
availability. Climax conifer stands were interpreted as being of high importance to Wolverine survival during winter. Conser-
vation implications include the detrimental effect on Wolverine populations likely to result from current timber harvesting
practices in the boreal forest.
Key Words: Wolverine, Gulo gulo luscus, snow depth, boreal forest, stand, landscape, climax, buffering effect, timber harvest-
ing, Alberta, British Columbia.
The Wolverine, Gulo gulo luscus, remains among the
least understood of the world’s forest mesocarnivores.
Recent research focusing on the life history of the
species in cordilleran landscapes is beginning to fill
knowledge gaps. However, landscape features docu-
mented as being of high importance to Wolverines in
mountainous regions — for example, the alpine zone
(Eric Lofroth, personal communication [see Acknow-
ledgments section for affiliation]) — are unavailable to
forest populations.
In the boreal forest, Wolverines are believed to be
declining from densities that appear to be lower than
in any of the other landscapes in which they occur
(Banci 1994). As they are less observable in the forest
due to the unbroken forest canopy, Wolverine study in
the forest ecoprovinces is an even greater challenge
than in alpine habitats. It is therefore not surprising that
Banci (1994) has suggested that stand-level and land-
scape scale “habitat use by Wolverines in forests has
not been adequately investigated”, and that research
is needed to study the “habitat needs of Wolverine in
forests, because there is no sound basis for developing
habitat management prescriptions at the stand level”.
In forested areas of the northwest, the Wolverine is
the furbearer about which wildlife agencies have the
greatest concern (Bill Johnson, personal communica-
tion).
There has been agreement among researchers that
Wolverine “habitat is probably best defined in terms
of adequate year-round food supplies in large, sparsely
inhabited wilderness areas, rather than in terms of
particular types of topography or plant associations”
(Kelsall 1981)*. Seasonal shifts by Wolverine in cor-
dilleran landscapes from the alpine zone in the summer
to subalpine forest in the winter have been attributed
to the availability of food (Banci 1994), or are thought
to be related to avoidance of high temperatures or
humans (Hornocker and Hash 1981). While snow
depth has been investigated as a limiting factor for
Fishers, Martes pennanti (Krohn et al. 1995; Raine
1983), it has not been implicated as a factor affecting
habitat selection in the Wolverine.
This paper presents the hypothesis that Wolverines in
the boreal forest are limited by mid-winter snow con-
ditions, which in turn affects stand, and in this case,
landscape selection.
Methods
Snow tracking is being increasingly recognized as a
reputable scientific tool in wildlife studies, management
and conservation, with efforts being made to establish
standardized terminology, institute university courses
on the subject, and to establish networks of trackers
throughout the North American continent (Rezendes
1999; Zielinski and Kucera 1995). Snow tracking may
be the only practical way of learning details of Wol-
verine habits and habitat use, as such details are not
adequately provided by radio-telemetry studies (John
Krebs, personal communication; Eric Lofroth, per-
sonal communication).
56
2004
Wolverine and other furbearer activities were mon-
itored during three winter seasons (1997-2000) utiliz-
ing snow-tracking methods. Approximately 34 000 km
were traveled by truck, snowmobile, cross-country skis
and on foot, in search of furbearer tracks, with an
emphasis on locating Wolverines. The tracking efforts
covered approximately 1100 km/? in the region of the
border country of Alberta and British Columbia known
as “Chinchaga” (after the Chinchaga River), at approx-
imately 57° north latitude. The tracking area offered
conditions especially conducive to this type of study,
in that the landscape could be conveniently divided into
distinct upland and lowland components. These com-
ponents offered markedly different and readily divis-
ible stand characteristics as a result of the “Great Chin-
chaga Fire” which blanketed the area during the 1950s
(Don Williams, personal communication), burning
all but some upland ridges. Fifty years following the
fire, two distinct forest types predominate: early-to-mid
seral second-growth of predominantly aspen or pine
in the lowlands, with more limited late-seral, climax
or “over-mature” stands predominated by White and
Black spruce (Picea spp.), and mostly dead and dying
Populus spp. in the uplands. The lowland forest may
be further characterized as forming a mosaic broken
by broad expanses of relatively open Black spruce fen
and willow (Salix sp.) muskeg. The upland forest cover
is by comparison more continuous.
The area is thoroughly criss-crossed by open linear
corridors at varying stages of regeneration that were
cleared to conduct seismology work, and have been
implicated in possible predator/prey imbalances. Seis-
mology work and subsequent oil and gas exploration
and extraction activities have been traditional in the
area since the 1950s (Brody 1981). The area is expe-
riencing a surge of such activities at present, and there
was virtually no segment of the area covered in track-
ing Wolverines that was not impacted by these activ-
ities at some point during the three winter seasons.
Moose (Alces alces) reach some of their highest
densities in North America in the area (Brody 1981),
being most heavily distributed in the lowlands, and
frequent in the uplands. Groups of Woodland Caribou
(Rangifer tarandus caribou) are frequent at low den-
sities in the lowlands. These are the only two com-
mon ungulate species in the region, and they offer a
generous prey-base for the area’s healthy Grey Wolf
(Canis lupus) population, whose kills in turn offer a
ready food source for the infrequent Wolverines.
When Wolverine tracks were located, the individuals
were fore-tracked (older trails) or back-tracked (fresh
trails) in order to gain insights into important and
little-known details of the creature’s use of the boreal
forest, including landscape and stand use. Tracks were
accessed in the morning by snowmobile or truck, and
followed on foot as long as daylight permitted, with
the exception of one overnight excursion conducted in
order to assess advantages and disadvantages to the
WRIGHT AND ERNST: STAND SELECTION BY WOLVERINES 57
tracking process of remaining in situ. Pertinent details
of the Wolverine’s behavior were logged in field note-
books during the tracking event as well as being
photographically documented.
Snow depth measurements (in centimetres) were
taken over a time frame of approximately | week, char-
acterized by below-freezing temperatures, between
periods of snowfall. Snow depths were taken at loca-
tions determined using random numbers generated by
a portable computer (calculator). The number indicated
the number of paces to be taken on the ground, either
within a grid-square (random snow depths), or along a
Wolverine or Lynx (Lynx canadensis) trail, at which
point a snow-depth was taken.
Bes following snow-depth data were recorded:
Ten random depths on open upland sites (to quantify
“non-buffered” upland snow depth) with a grid-cell size
of 1 km?;
e 27 random depths in forested upland sites (“buffered”
upland depths) with a grid-cell size of 1 km;
e Ten random depths on open lowland sites (to quantify
non-buffered lowland snow depth) with a grid-cell size
of 1 km’;
e 25 random depths on forested lowland sites (buffered
lowland depths) with a grid-cell size of 1 km?;
e 46 random depths along documented Wolverine trails
at random paced intervals;
e 29 random depths along Lynx trails (for comparison
purposes) at random paced intervals.
The following comparisons were made utilizing
ANOVA tests of significance:
e Snow depths along Wolverine trails versus random for-
ested upland snow depths;
e Random forested upland snow depths versus random
open upland snow depths (= “buffering effect” of upland
canopy on snow depth);
e Random forested lowland snow depths versus random
open lowland snow depths (= buffering effect of lowland
canopy on snow depth):
e Snow depths along Lynx trails versus random forested
lowland snow depths (for comparison purposes).
Crusting of snow typically occurs in the area of this
study during late winter to early spring, and occasion-
ally in late fall, depending on temperatures. Crustless
(powder) conditions are the norm in this region for
the majority of the snow season. Snow conditions were
noted as being of a crustless nature during the collec-
tion of this data.
Wolverine reactions to linear corridors such as
access roads and seismic lines were documented as
encountered, with special attention being paid to the
effect that snow conditions on the corridors (compact-
ed versus undisturbed) had on Wolverine response.
Efforts were made to locate Wolf kills in both
representative landscapes in order to monitor such
important food sources for utilization by Wolverines.
Results
Wolverine tracks were located on ten occasions over
three winters (for a mean of one Wolverine track en-
58 THE CANADIAN FIELD-NATURALIST
countered per 3400 km of searching). Thirteen sepa-
rate tracking events resulted, totaling 20 linear km of
off-corridor (forest) tracking, or 26.6 total off-cor-
ridor km using Magoun’s (1985) estimate of adding
33% to arrive at non-linear distance traveled. Wolver-
ines were tracked for an additional 12.3 km on linear
corridors offering conditions of compacted snow, for
a total estimated tracking distance of 38.9 km.
Seven Wolf kills (Moose) were located, two in the
upland landscape and five in the lowland landscape.
These kills were monitored for Wolverine use. An
additional road-killed Moose in the lowland landscape
was monitored for Wolverine use. Of these, Wolver-
ine were documented as utilizing one of the upland
Wolf kills.
Despite frequent available food in the lowland land-
scape, Wolverine tracks were located only in the upland
landscape. Wolverines were revealed to have remained
in the uplands throughout the tracking events.
One Wolverine tracked was noted to have traveled
through a burned-over upland area regenerating to
Lodgepole Pine (Pinus contorta). The second-growth
pine formed a low (approximately three-metre), dense
canopy. Heavy use of the burn by Snowshoe Hares
(Lepus americanus), provided compacted trails on which
the Wolverine traveled through this second-growth.
Wolverines often encountered linear corridors during
their travels. Wolverine diverged from their line-of-
travel under the forest canopy to travel on 100% of the
linear corridors encountered that offered conditions of
compacted snow (n=17), for distances ranging from
3 — 3000 m. Wolverines did not travel on any of the
corridors encountered that had undisturbed snow cover
(n = 16), choosing instead the most direct route across
in 100% of instances noted.
There were two instances where an individual Wol-
verine paralleled an undisturbed east-west corridor
from just within the south-facing edge of the canopy.
The individual crossed the respective corridors in-
volved to select the south-facing aspect for travels of
470 m and 30 m, before diverging deeper into forest.
Exposure to the sun had acted in concert with the
buffering effect of the canopy to reduce snow depth
from 32 cm on the corridor, to 4 — 11 cm under the
canopy’s edge.
Snow depths along routes selected for travel by
Wolverines were significantly less than random snow
depths under the upland canopy (F = 32.84, df = 1, P
<< 0.010).
TABLE 1: Comparison of random snow depths
Wolverine Trails
Range 13-47 cm
Mean 31 cm
Standard Deviation 9.03
Vol. 118
Random upland snow depths under the canopy were
significantly less than snow depths in open upland areas
(F = 11.1, df = 1, P< 0.010), whereas random lowland
snow depths under canopy were not significantly dif-
ferent from snow depths in open lowland sites (F =
3.45, df = 1, P > 0.05).
Snow-depths along routes selected for travel by Lynx
were not significantly different from random snow
depths under the lowland canopy, where Lynx data
were collected (F = 2.86, df = 1, P > 0.05).
When Wolverine tracks were discovered exiting the
forest onto access routes, the Wolverines involved had
invariably been traveling through dense to extremely
dense coniferous cover. While subsequent travel on
compacted linear corridors would frequently take a
Wolverine through a variety of stand types, the Wol-
verines invariably selected similarly dense coniferous
cover for re-entry into the forest. Within the forest,
Wolverines were frequently, even continuously, ob-
served to alter their direction of travel (n = 29) to select
for routes that offered an even slightly denser canopy
cover (increased buffering effect on snow). Of the ran-
dom upland sites, 70% were estimated to represent a
similar cover type to that selected by Wolverines for
travel, as compared to 20% of random lowland sites.
Discussion
Popular and even scientific literature of past decades
reflected the level of misconception surrounding the
Wolverine. The Wolverine was seen as unique among
wildlife in being best adapted to survive during the
harshest months, to the point of finding winter a sea-
son of ease (Rausch and Pearson 1972). The animal’s
adaptations to a winter landscape were provided as
evidence of this: the dense, luxurious coat (which may
give the illusion of good underlying physical condition
in winter); the enormous, well-haired “snowshoe”
feet cited as enabling the animal to coast effortlessly
on top of deep snow; the preference for the harshest
wilderness areas. In fact, in an ongoing study in the
foothills of northern British Columbia, Wolverines in
winter were often found upon examination to be in a
state of energetic stress approaching thresholds of star-
vation (Don Reid, personal communication); a large
percentage of dissected Wolverines have empty gastro-
intestinal tracts (Banci 1994). Unlike such sympatric
predators as Martens (Martes americana), and col-
oured foxes (Vulpes vulpes), Wolverines are too large
to survive on small prey (Banci 1994), and must there-
fore wander widely, as indicated in all studies, in search
Random Lowland Locations Lynx Trails
23 — 52 cm 17-54 cm
40 cm 36 cm
Wes) 8.2
2004
of less reliable yet more bountiful sources of food
such as large ungulate carrion.
While recent research is presenting a different pic-
ture of Wolverines and their habits, apparent contra-
dictions still abound. One of the more notable of the
apparent contradictions in Wolverine behavior is ad-
dressed by this paper: Why do Wolverines select for
wide-open landscapes in some parts of their range and
the densest of cover in other areas such as the boreal
forest? During the tracking of Wolverines in the boreal
forest at Chinchaga, patterns of behavior became ap-
parent. The species limited itself to the upland land-
scape despite abundant food in the lowlands, con-
tradicting literature which suggested that wilderness
conditions and a ready supply of food governed the
Wolverine’s presence or absence, rather than specific
landscape and stand features (Kelsall 1981*; Banci
1994). The observation that Wolverines in the study
area were limiting themselves to a specific landscape
(at least during winter) was supported by conversa-
tions with the area’s fur trappers and wildlife agents,
who noted that:
(1) over many decades of trapper experience in the Chin-
chaga area, Wolverines were encountered in heavily
timbered upland terrain (Les Sharp, personal com-
munication);
(2) in a winter trapper’s experience over 13 years on a
lowland landscape trapline adjacent to uplands where
Wolverines were tracked during this study, not a single
Wolverine was caught, nor tracks ever detected (Larry
Smith, personal communication).
(3) in other lowland traplines in the area with long tra-
ditions of use none were recalled to have ever yielded
Wolverine pelts (Bill Johnson, personal communi-
cation).
During the tracking efforts, it became quickly appar-
ent to me that the Wolverines were continuously sel-
ecting, where feasible, for the path of least snow cover.
When faced with even a slight thinning of the forest
canopy (= deeper snow conditions), the animals were
observed to have paused, selected the densest alter-
native timber, and altered their route to follow this
“path of least resistance” in terms of snow depth. The
Wolverines would only cross such openings if:
(1) a compacted Showshoe Hare trail crossed the deeper
snow, which they would then select;
(2) alternative routes were not available without extensive
detour, in which case the Wolverine would cross the
deeper snow over the shortest straight-line path, usually
at a walking gait.
Wolverines in the area seemed to favor a “2x” or
“3x” lope (Zielinski and Kucera 1995) when less
impeded by snow, suggesting that this was their most
efficient gait in terms of energy expenditure versus
distance traveled. They would immediately switch to a
less efficient walk, however, when faced with unavoid-
able stretches of deeper snow.
In comparison, Lynx were observed not to avoid
deeper snow, readily crossing open areas of the deepest
snow conditions, as encountered. This is supported
WRIGHT AND ERNST: STAND SELECTION BY WOLVERINES 59
not only by the snow depth data, which showed Lynx
(in direct contrast with Wolverine) to have selected
paths of insignificantly less snow depth, but also by the
fact that Lynx were abundantly found in the lowland
landscape where the buffering effect of the forest
canopy was demonstrated to be insignificant.
Wolverines traveling together did so single-file for
an estimated 95% of the distance traveled, traveling in
tandem only along ridges where snow cover was neg-
ligible. It would be interesting to discover if social travel
in this species represents a survival strategy, and if the
individuals involved alternate as lead-individual.
That Wolverines at Chinchaga were not selecting the
densest canopy conditions in order to avoid detection by
man or predators is obvious for the following reasons:
(1) In 100% of cases, they followed open linear corridors
offering compacted snow conditions when encountered
(including winter roads up to 18 m wide; freshly
opened seismic lines; snowmobile trails; all-terrain
vehicle tire tracks; wind-swept ice on creek-beds bisect-
ing open muskeg; compacted otter runways on open
creek beds) for travel of distances up to 3 km;
(2) Wolverines are more abundant on the open tundra
(characterized by hard-crusted snow conditions) than
they are in the forest (Don Reid, personal communi-
cation; Banci 1994);
(3) Wolverines seem to prefer the open alpine zones during
snow-free seasons in cordilleran landscapes (Whitman
et al. 1986; Banci 1994; Don Reid, personal com-
munication; Eric Lofroth, personal communication).
The hypothesis presented by this paper is that Wol-
verines in the mid-winter boreal forest are limited by
snow conditions. Conifer-dominated climax stand types
offer the highest buffering effect on snow conditions
underfoot. In this study area, such stand-types are
only found extensively in upland landscapes, which
accounts for the absence of Wolverines in the lowlands,
despite abundant food there. Wolverines travel great
distances in search of unpredictable food (Banci 1994)
while under conditions of energetic stress, necessi-
tating that they pay the strictest attention to energy
expenditure while traveling. To travel in conditions
of deep powder (unbuffered) snow is to increase risk
of starvation, and so such conditions are avoided where
alternatives exist. While the relatively enormous feet of
the Wolverine, providing low foot loads of 22 g/cm?
(Knorre 1959) are of great advantage when crusts begin
to form (Eric Lofroth, personal communication), they
have little effect in the midwinter powder snows of
the northwest characterizing this study, as indicated by
shifts to an inefficient walking gait in deep, midwin-
ter snow. It is further suggested here that the size of
the Wolverine’s feet, rather than being an indication
of their level of mastery of winter conditions, is in-
stead just the opposite, an adaptation indicative of their
extreme level of sensitivity to snow depths as a result
of specialized foraging strategies combined with rela-
tively large body size leading to conditions of energetic
stress. While one could argue that Lynx, with their
equally large feet and specialized foraging strategies,
60 THE CANADIAN FIELD-NATURALIST
should therefore show a similar sensitivity to snow
depths not indicated in this study, it should be remem-
bered that the Lynx data herein were collected during
years of high hare numbers. Perhaps during the low
hare cycle, Lynx must also become more sensitive to
snow depths.
Conclusions
During midwinter, Wolverines in the boreal upland
forests of northwestern Alberta and northeastern British
Columbia demonstrate preferences at the stand level
and landscape scale that are apparently unrelated to
food availability, consistently selecting for stand types
that offer the greatest available buffering effect on
ground snow depth.
Wolverines require the type of boreal forest habitat
considered optimum for Martens, the species with
which they may be considered most highly sympa-
tric. However, Wolverines appear to be even more
dependent on climax conifer forests during winter than
are Martens. Climax conifer cover appears to be of
high importance to Wolverines in the boreal forest
because of the buffering effect this stand type has on
snow depth.
Forest practices that remove climax growth may
create conditions that are not conducive to Wolverine
conservation. As current logging practices in the boreal
forest are geared towards precisely this type of stand
removal, timber harvesting may be a key factor in appa-
rent population declines. Conditions following removal
of climax cover may not become favorable again for
Wolverine habitation for many decades (Don Williams,
personal communication). The situation may be im-
proved in the case of immediate regeneration to Pinus
spp., however, with a minimum estimated lapse of 20
years (several Wolverine generations) before conditions
become again conducive to Wolverine travel, if not
other life history components of this species. Efforts
should be made to preserve linkages of climax conifer
cover between more extensive areas of intact climax
forest habitat.
Acknowledgments
Funding, accommodations, and ongoing support for
this project were provided by Pioneer Natural Res-
ources Canada Inc., to whom the authors are very
deeply grateful. We would also like to thank the fol-
lowing (in order they appear in text) for their per-
sonal communications: Eric Lofroth, British Columbia
Ministry of Environment, Lands and Parks, Victoria,
British Columbia; Bill Johnson, Alberta Environment,
Peace River, Alberta; John Krebs, Columbia Basin
Vol. 118
Fish & Wildlife Compensation Program, Nelson, Bri-
tish Columbia; Don Williams, Alberta Environment,
Manning, Alberta; Don Reid, British Columbia Minis-
try of Environment, Lands and Parks, Smithers, British
Columbia; and the late Les Sharp, as well as Larry
Smith, fur-trappers in the Chinchaga region of Alberta.
Documents Cited (marked with * in text)
Kelsall, J. P. 1981. Status report on the Wolverine, Gulo
gulo, in Canada in 1981. (Committee on the Status of
Endangered Wildlife in Canada (COSEWIC), Ottawa,
Ontario. 47 pages.
Literature Cited
Banci, V. 1994. Wolverine. Pages 99-127 in American marten,
Fisher, Lynx and Wolverine in the western United States.
Edited by L. F. Ruggiero, K. B. Aubry, S. W. Buskirk, L.
J. Lyon and W. J. Zielinski. USDA Forest Service General
Technical Report RM-254.
Brody, H. 1981. Maps and dreams; Indians and the British
Columbia frontier. Douglas & McIntyre. Vancouver, British
Columbia, and Toronto, Ontario.
Hornocker, M. G., and H. S. Hash. 1981. Ecology of the
Wolverine in northwestern Montana. Canadian Journal
of Zoology 59: 1286 — 1301.
Knorre, E. P. 1959. Ecology of the elk. Jn Transactions of
the Pechora-Ilych State Game Preserve by G. A. Novikov.
Translated by The Canadian Wildlife Service 1966. 3895.
(7): 324 pages.
Krohn, W. B., K. D. Elowe, and R. B. Boone. 1995. Relations
among Fishers, snow and martens: development and eval-
uation of two hypotheses. The Forestry Chronicle 71(1):
97-105.
Magoun, A. J. 1985. Population characteristics, ecology, and
management of Wolverines in northwestern Alaska. Ph. D.
thesis, University of Alaska, Fairbanks, Alaska. 197 pages.
Raine, R. M. 1983. Winter habitat use and responses to
snow-cover of Fisher (Martes pennanti) and marten (Martes
americana) in southeastern Manitoba. Canadian Journal
of Zoology 61: 25-34.
Rausch, R. L., and A. M. Pearson. 1972. Notes on the
Wolverine in Alaska and the Yukon Territory. Journal of
Wildlife Management 36: 249-268.
Rezendes, P. 1999. Tracking & the art of seeing; how to
read animal tracks and sign. Firefly Books, Willowdale,
Ontario. 336 pages.
Whitman, J. S., W. B Ballard, and C. L. Gardner. 1986.
Home range and habitat use by Wolverines in south-
central Alaska. Journal of Wildlife Management 50: 460-
462.
Zielinski, W. J., and T. E. Kucera. 1995. American Marten,
Fisher, Lynx, and Wolverine: survey methods for their
detection. USDA General Technical Report PSW-GTR-
lsyie
Received 19 July 2001
Accepted 26 May 2004
Wolverine, Gulo gulo luscus, Resting Sites and Caching Behavior in
the Boreal Forest
JONATHAN D. WRIGHT and JESSICA ERNST
Ernst Environmental Services, Box 753, Rosebud, Alberta TOJ 2T0 Canada
'Present address: Box 648, East Coulee, Alberta TOJ 1B0 Canada
Wright, Jonathan D., and Jessica Ernst. 2004. Wolverine, Gulo gulo luscus, resting sites and caching behavior in the boreal
forest. Canadian Field-Naturalist 118(1): 61-64.
Wolverine (Gulo gulo luscus) caches and resting sites were examined in a study area in the boreal upland forests of northwestern
Alberta and northeastern British Columbia (approximately 57°N). Cache sites were in climax, or ““overmature” stands of Black
Spruce (Picea mariana) or mixed-wood of high complexity, dominated by conifers, and in which the Trembling Aspen (Populus
tremuloides) and Balsam Poplar (Populus balsamifera) component consisted of mostly dead or dying trees characteristic of
such old growth in the boreal uplands. Sites offered relatively good visibility of the surrounding stand. Sites were never
located in the dense to extremely dense homogenous spruce stands documented as being favored for travel by Wolverines in the
study area. The better used cache complexes were accessed by numerous weil-used trails made by the Wolverines themselves.
Caches consisted of the bones, hide and hair of Moose (Alces alces) believed to have been killed by Grey Wolves (Canis
lupus). Caches were classified as “simple caches” composed of a single feeding site and/or excavation and “cache complexes”
involving one or more feeding “stations”, latrines, resting sites, and climbing trees that may have been used as avenues of escape
from competitors/predators. Resting sites were located atop the snow in relatively open locations that offered good visibility
of the surroundings. Climax stands were implicated as being of importance to Wolverine caching behavior. Conservation
implications include the detrimental effect on Wolverine populations likely to result from current timber harvesting practices
|
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in the boreal forest.
Key words: Wolverine, Gulo gulo luscus, cache, resting site, climax, boreal forest, stand, Alberta, British Columbia.
Knowledge gaps exist involving many aspects of
Wolverine life history in forests, including caching
behavior and selection of resting sites (Banci 1994).
This paper presents observations of these aspects of
Wolverine activities as documented over three winters
(1997-2000) of snow-tracking efforts in the boreal
upland forests of the border between northwestern
Alberta and northeastern British Columbia, at approxi-
mately 57°N.
Methods
Wolverine and other furbearer activities were moni-
tored during three winter seasons (1997-2000) utilizing
snow-tracking methods. The tracking efforts covered
approximately 1100 km? in the region of the border
country of Alberta and British Columbia known as
“Chinchaga” (after the Chinchaga River). Tracking is
being increasingly recognized as a useful scientific tool
in wildlife studies, management and conservation, with
efforts being made to establish standardized termi-
nology, to institute university courses on the subject,
and to establish networks of trackers throughout the
North American continent (Rezendes 1999; Zielinski
and Kucera 1995). Snow tracking may be the only
practical way of learning details of Wolverine habits
and habitat use, as such details are not adequately pro-
vided by radio-telemetry studies (Eric Lofroth, personal
communication).
Approximately 34 000 km were traveled by truck,
snowmobile, cross-country skis and on foot, in search
of furbearer tracks over the course of the three winters,
with an emphasis on locating Wolverines. Markedly
different and readily divisible stand characteristics are
a feature of the area as a result of the “Great Chinchaga
Fire” which blanketed the region during the 1950s
(Don Williams, personal communication), burning all
but the upland ridges. Fifty years following the fire,
two distinct forest types predominate: early-to-mid seral
second growth of predominantly aspen or pine in the
lowlands, with more limited late-seral, climax or “over-
mature” stands predominated by White Spruce and
Black Spruce (Picea spp.), and mostly dead and dying
Populus spp. in the uplands. The lowland forest may
be further characterized as forming a mosaic broken by
broad expanses of relatively open Black Spruce fen and
open Willow (Salix spp.) muskeg. The upland forest
cover is by comparison more continuous.
Moose (Alces alces) reach some of their highest
densities in North America in the area (Brody 1981),
being most heavily distributed in the lowlands, and
frequent in the uplands. Groups of Woodland Caribou
(Rangifer tarandus caribou) are frequent at low densi-
ties in the lowlands. These ungulates offer a generous
prey base for the area’s healthy Grey Wolf (Canis lupus)
population, whose kills in turn offer a ready food
source for the infrequent Wolverines.
When Wolverine tracks were located, the individ-
uals were fore-tracked (older trails) or back-tracked
(fresh trails) in order to gain insights into important
and little-known details of the creatures’ use of the
61
62 THE CANADIAN FIELD-NATURALIST
boreal forest, including landscape and stand use. Tracks
were accessed in the morning by snowmobile or truck,
and followed on foot as long as daylight permitted,
with the exception of one overnight excursion con-
ducted in order to assess advantages and disadvan-
tages to the tracking process of remaining in situ.
Pertinent details of the Wolverines’ behavior were
logged in field notebooks during the tracking event
as well as being photographed.
Results
Wolverine tracks were located on ten occasions over
three winters (for a mean of one Wolverine track en-
countered per 3400 km of searching). Thirteen sep-
arate tracking events resulted, each lasting approxi-
mately six hours, and totaling 20 linear km of off-
corridor (forest) tracking, or 26.6 total off-corridor
km using Magoun’s (1985) estimate of adding 33% to
arrive at non-linear distance traveled. Wolverines were
tracked for an additional 12.3 km on linear corridors
offering conditions of compacted snow, for a total
estimated tracking distance of 38.9 km. Five cache sites
and three resting sites were encountered and docu-
mented using a GPS unit, camera, and sketches in
field notebooks.
Despite frequent available food in the lowland land-
scape, Wolverine tracks were located only in the up-
land landscape. Wolverine were revealed to have re-
mained in the uplands throughout the tracking events.
Wolverine often encountered linear corridors during
their travels. Wolverine diverged from their line of
travel under the forest canopy to travel on 100% of the
linear corridors encountered that offered conditions of
compacted snow (n=17), for distances ranging from 3
to 3000 m. In one instance, two Wolverines traveling
together followed a compacted (snowmobile) trail on a
linear corridor for 1270 m to bring them within 150 m
of a cache site, at which point they exited the trail at
right angles to follow the shortest linear distance
directly to the cache.
All five caches observed consisted of bones and/or
sections of the hides of Moose (Alces alces), all of
which were believed to have stemmed from the Wol-
verine’s scavenging of Grey Wolf (Canis lupus) kills.
Bones and hide are believed to be a very important
component of the Wolverine’s winter economy (Banci
1994; Haynes 1982). Cache-sites appear to be closely
frequented until the nutritive value is exhausted, judg-
ing from the well-used system of trails and tracks of
varying ages in the vicinity of such sites.
Cache sites encountered ranged from those consist-
ing of a single bone process or an excavation (n = 2),
to those better described as “cache complexes” (n = 3).
Such complexes were believed to stem from the scay-
enging of a single kill, resulting in a series of smaller
caches spread over areas which ranged from highly
localized to widely radiating. Cache sites were in cli-
max, or “overmature” stands of Black Spruce (Picea
mariana) or mixed-wood of high complexity, domi-
Vol. 118
nated by conifers in which the Trembling Aspen
(Populus tremuloides) and Balsam Poplar (Populus
balsamifera) component consisted of mostly dead or
dying individuals characteristic of such old growth in
the boreal uplands. Sites offered relatively good visi-
bility of the surrounding stand. Sites were never locat-
ed in the dense to extremely dense homogenous spruce
stands documented as being favored for travel by
Wolverines in the study area, perhaps because of the
limited field of vision in such stands. The better-used
cache complexes were accessed by numerous well-used
trails made by the Wolverines themselves, and had
certain features in common, including:
e areadily accessible spruce tree (Picea spp.) of rela-
tively large dbh (diameter at breast height) selected
and well-used for climbing (perhaps as refuge from
Wolves, or a safe area to digest between feedings);
° aresting site characterized as a depression in the snow
formed by the Wolverine’s body and with a good view
of surroundings;
e one or more latrines — specific off-trail sites the Wol-
verine visited to eliminate wastes;
e aradiating series of “feeding areas” characterized by
areas approximately 1.5 m* of well-compacted snow,
on which bones and bone fragments or sections of
Moose-hide were found, but not both, and distinguish-
able from a kill site by the lack of Moose stomach-
content remains;
e excavations [often in the snow, but on more than one
occasion (n = 3) in the earth beneath the overhanging
boughs of a very large spruce tree], that likely had
contained fragments of cached food.
A detailed description of the cache and resting sites
presented on a site-by-site basis follows, in order as
encountered.
Cache #1
Cache # I was a widely radiating cache complex.
The original Wolf kill site was believed to have oc-
curred on a linear corridor regenerating to Lodgepole
Pine (Pinus contorta) located at 57° 27° 20” N and
120° 08° 26” W. Old Wolf tracks lead to and from
this central location, and Wolverine trails of varying
ages, all apparently more recent than the Wolf tracks,
were present. Shards of Moose bone were located at
a feeding area here.
Three additional caches connected by Wolverine
trails and radiating from the kill site combined to
comprise the cache complex.
(1) At 57° 27° 20” N and 120° 08’ 18” W a cache con-
sisting of Moose hide remains and an abundance of
Moose hair was located.
(2) At 57° 27’ 17” N and 120° 08’ 18” W a fresh excava-
tion in the earth under the boughs of a very large spruce
tree was located. This cache was believed to have been
visited by a Wolverine within several hours prior of
its discovery.
(3) At 57° 27° 22” N and 120° 08’ 06” W a cache consist-
ing of bone shards and fragments was located. The
shards were larger than those examined at the kill site.
Further components of this cache included an excava-
tion in the snow down to the sphagnum ground-cover
and a latrine.
2004
This cache complex was not characterized by a
climbing tree, which was a notable component of some
other cache sites. The Wolverine tracked to this cache
complex was dragging what was believed to be a trap
by one of its left feet. This hindrance apparently ren-
dered it incapable of climbing, as nowhere during the
tracking event was it observed to have done so,
whereas other Wolverines tracked climbed regularly.
The trap appeared to affect the individual’s locomo-
tion as well; unlike other Wolverines tracked, this in-
dividual never varied its gait from a “2x lope”
(Zielinski and Kucera 1995).
Cache # IT
Cache # II was located 150 m from a linear corridor
with compacted access (snowmobile trail) that was
followed by two Wolverines traveling together, as
mentioned, for 1270 m, before exiting the corridor at
a right-angle to head directly to the cache.
This cache is best described as a localized complex,
and appeared to represent the richest of the observed
caches as evidenced by heavy use. It was located in a
climax stand of somewhat stunted Black Spruce. Four
feeding stations were located here, characterized by
the existence of bone shards and larger fragments and
processes of bone. There were three latrines, two con-
taining white scats and one containing brown scats.
Resting Site # 1
A resting site, slightly elevated, was located at the
north edge of the complex. The resting site consisted
of a 43 x 35 cm oval depression atop the snow, at the
base of the remains of a short (30 cm), well-wea-
thered spruce stump. Snow in the depression was well-
compacted. The resting site was relatively open, away
from the boles of living trees, and offered a good
view of the cache complex and its approaches. It was
accessed by four well-used trails, at approximately the
four points of the compass. A few guard hairs were
present in the depression, along with a few dribbles
of urine at the edge of the east access.
A climbing tree (Black Spruce) of approximately
14 m was located in a dense clump of smaller spruce
at the southeast edge of the cache complex. The tree
was larger than the stand’s average and heavily used,
as evidenced by claw-marks on the trunk, heavy debris
of bark atop the snow at the tree’s base, and the degree
of trampling of snow within the spruce clump. Climb-
ing on the tree appeared to terminate at a point near its
apex where there was a “witches’ broom” formation
estimated to be large enough to support a resting Wol-
verine; it may have been an additional resting site. No
additional trees in the area of the cache complex bore
any evidence of having been climbed by a Wolverine.
Resting Site # 2
A second resting site was discovered by following
the trail of the two Wolverines after leaving Cache # 2.
Approximately 200 m from the cache, this resting site
again consisted of an oval depression (58 x 43 cm)
WRIGHT AND ERNST: WOLVERINE RESTING SITES AND CACHING 63
atop the snow at the base of a relatively large Tama-
rack (Larix laricina) tree. Snow in the depression was
well-compacted. This resting site was characterized
by having more canopy cover than the previous site,
although the cover was by no means dense. There
was no cache in the immediate vicinity of this resting
site, and no apparent climbing tree.
Cache # III
Cache # III was located at 57° 26’ 84” N and
120° 07° 69” W and is best termed a “simple cache”,
rather than a cache-complex. This cache consisted of a
single large bone-process and a well-gnawed Moose’s
hoof. The cache was located by following the previ-
ous two Wolverines, which evidently were aware of,
or scented, this cache, as evidenced by their diverting
their course of travel by approximately 50 m to reach
the cache. There were no other features characteristic
of other caches present at Cache # III.
Cache # IV
Cache # IV located at 57° 27’ 25” N and 120° 06’
81” W is best termed a cache-complex, although not
extensive. Certain features lacking at the last (simple)
cache were present at this one. This cache consisted
of a collection of bone fragments located on a single
feeding platform under a relatively open canopy in a
high-complexity climax mixed-wood stand. The cache
was accessed by numerous well-used Wolverine trails.
No latrines were discovered at this cache.
Approximately 10 m from the main cache was an
excavation in the earth under the overhanging boughs
of a very large spruce tree, accessed by a Wolverine
trail, and virtually identical to the excavation discoy-
ered at Cache # I. This excavation, too, was deemed
to have contained cached food that had been recently
recovered by a Wolverine.
Cache # IV was further characterized by a well-used
climbing tree (spruce) of larger than average dbh,
located approximately 4 m from the feeding-station.
This cache was located approximately 10 m from a
linear corridor with compacted access (snowmobile
trail) that was used as a conduit for 700 m in a nor-
therly direction by the Wolverine pair upon exiting
the cache. This cache had been visited recently by a
Marten (Martes americana).
Cache #V
Cache # V was located in very large, climax mixed-
wood dominated by spruce, near the base of a ridge
adjacent to Resting Site # III. This was a simple cache,
consisting of a single fresh excavation in the earth
beneath the overhanging boughs of a large spruce,
much as described for caches I and IV. The excava-
tion was also believed to be for the purpose of recov-
ering cached food.
Resting Site # 3
Resting Site # 3 was located along the Wolverine
pair’s trail at 57° 27° 72” N and 120° 05’ 11” W. As
in the case of the other resting sites observed, this
64 THE CANADIAN FIELD-NATURALIST
one consisted of an oval depression atop the snow
approximately the same dimensions as the last pre-
vious two sites (measurements not taken due to this
similarity). The site was mid-slope on a prominent
ridge covered by a stand of very large mixed-wood
dominated by spruce. The site was relatively open,
and offered good view down and along-slope, and only
slightly less so upslope. Within 1 m of the resting site
was a medium-sized pine tree which had been well-
climbed to a height of approximately 4 m.
Tracks indicated that this resting site may have
been utilized by a third Wolverine which was travel-
ing down slope. It appeared as though this third
Wolverine left the resting site to travel approximately
15 m along-slope to meet the Wolverine pair as they
traveled upslope. The single Wolverine may have util-
ized the climbing-tree to observe the approaching
pair. A confusion of tracks resulted where the three
Wolverines apparently met. It is believed that all
three animals subsequently traveled upslope together.
Discussion
Caches were located in climax stands of less density
than those apparently favored for travel by Wolverines
in the study area. Visibility of approaching competi-
tors/predators (Wolves) may be the deciding factor in
both cache-site and above-snow resting-site selection.
That the caches were all located in climax timber re-
inforces the importance of this stand-type to Wolver-
ine. Present forest practices that result in the harvest-
Vol. 118
ing of climax stands may negatively impact Wolver-
ine populations.
Acknowledgments
Funding, accommodations and ongoing support for
this project were provided by Pioneer Natural Res-
ources Canada Inc., to whom the authors are deeply
grateful.
Literature Cited
Banci, V. 1994. Wolverine. Pages 99-127 in American marten,
Fisher, Lynx and Wolverine in the western United States.
Edited by L. F. Ruggiero, K. B. Aubry, S. W. Buskirk, L.
J. Lyon and W. J. Zielinski. USDA Forest Service Gen-
eral Technical Report RM-254.
Brody, H. 1981. Maps and dreams; Indians and the British
Columbia frontier. Douglas & McIntyre. Vancouver, Bri-
tish Columbia; Toronto, Ontario.
Haynes, G. 1982. Utilization and skeletal disturbances of
North American prey carcasses. Arctic 35: 266-281.
Magoun, A. J. 1985. Population characteristics, ecology, and
management of Wolverines in northwestern Alaska. Ph.D.
thesis. University of Alaska, Fairbanks, Alaska, 197 pages.
Rezendes, P. 1999. Tracking & the art of seeing; how to read
animal tracks and sign. Firefly Books, Willowdale, Ontario.
336 pages.
Zielinski, W. J. and T. E. Kucera. 1995. American marten,
Fisher, Lynx, and Wolverine: survey methods for their
detection. USDA General Technical Report PSW-GTR-
ilyt/s
Received 19 July 2001
Accepted 26 May 2004
Seasonal Home Ranges of Raccoons, Procyon lotor, Using a Common
Feeding Site in Rural Eastern Ontario: Rabies Management Implications
SARAH C. ToTTon,! RICHARD C. ROSATTE,? ROWLAND R. TINLINE,? and LAURA L. BIGLER‘
'340 Second Avenue West, Owen Sound, Ontario N4K 4L7 Canada
? Ontario Ministry of Natural Resources, P.O. Box 4840, Peterborough, Ontario K9J 8N8 Canada
> Geographic Information Systems Laboratory, Queen’s University, Kingston, Ontario K7L 3N6 Canada
+ Zoonotic Disease Section, Diagnostic Laboratory, College of Veterinary Medicine at Cornell University, P.O. Box 5786,
Upper Tower Road, Ithaca, New York 14852-5786 USA
Totton, Sarah C., Richard C. Rosatte, Roland R. Tinline, and Laura L. Bigler. 2004. Seasonal home ranges of Raccoons,
Procyon lotor, using a common feeding site in rural eastern Ontario: Rabies management implications. Canadian
Field-Naturalist 118(1): 65-71.
Thirteen adult Raccoons (Procyon lotor) (six females, seven males) that fed at a garbage dump north of Kingston, Ontario
were radio-tracked from 21 June to 16 October 1995 to assess their seasonal home ranges and movements. Average
Minimum Convex Polygon (MCP) summer and fall home ranges for the collared Raccoons were 78.4 ha (SD=46.2 ha) and
45.6 ha (SD=29.7 ha), respectively. Average grid cell summer and fall home ranges for the collared Raccoons were 143.3 ha
(SD=40.0 ha) and 116.9 ha (SD=24.9 ha), respectively. Summer ranges of the Raccoons were significantly larger than fall
ranges using both the MCP method (P=0.05) and the grid cell method (P=0.073). Yearling Raccoons travelled an average
summer maximum distance from the dump of 2608 m (SD=1964, n=3), more than double the distance of adults (22 yr) at
1239 m (SD=547, n=10). The population density for the study area in late August 1995 was estimated at | Raccoon/12 ha
based on an effective area surrounding the dump of 234 ha. Home range and movement data may be useful to design a
strategy to control Raccoon rabies in Ontario.
Key Words: Raccoon, Procyon lotor, rabies, communal feeding, disease transmission, field study, home range, telemetry, Ontario.
Raccoon (Procyon lotor) rabies was first reported
in Ontario, Canada, during July 1999 (Wandeler and
Salsberg 1999; Rosatte et al. 2001). Point infection
control methodologies are currently being used (since
1999) in Ontario to contain the outbreak to a small
area (Rosatte et al. 2001). As well, a Raccoon rabies
model is being developed in Ontario to assist with the
control of the disease by predicting the rate of spread of
Raccoon rabies both temporally and spatially. Know-
ledge on Raccoon home ranges, movements and popu-
lation dynamics in Ontario is needed to develop and
validate the rabies model so that it reflects the actual
sequence of events that occur during a Raccoon
rabies epizootic/enzootic (Broadfoot et al. 2001).
The spatial distribution of food is known to influ-
ence contact rates in Raccoons (Procyon lotor) (Sei-
densticker et al., 1988). Clumped food resources such
as garbage dumps may increase potential contact rates
of Raccoons as these resources cause members of a
population to congregate from a wide area. This in
turn may influence rabies transmission in the popula-
tion (Seidensticker et al. 1988). Range of movements
of Raccoons using common feeding sites may be a
useful indicator of potential rabies spread. Such infor-
mation can be used to design effective baiting strate-
gies to vaccinate these animals against rabies as well
as provide input for the development of rabies models.
Home ranges of Raccoons tend to shift due to sea-
sonal changes in behavior and therefore must be calcu-
lated separately for each season (Kauffmann 1982).
Summer is the family rearing period when lactating
mothers and their offspring travel together and it is also
the main dispersal period for yearling males (Mech et
al. 1968; Fritzell 1978). Fall is a time when the juve-
niles may disperse and Raccoons prepare for the com-
ing winter dormancy period (Shirer and Fitch 1970).
In this study, home range was defined using criteria
of White and Garrott (1990) as the area within which
the animal normally moved in a specified time frame,
in this case the summer and fall of 1995.
In this study, movements of Raccoons using a com-
mon feeding site in rural eastern Ontario, Canada, were
determined by radio-telemetry to assess the size of their
summer and fall home ranges. The same Raccoons on
which contact data were obtained in the Totton et al.
(2002) study were used. In addition, two Raccoons,
caught at a smaller feeding site (compost heap) were
tracked periodically to determine their daytime rest-
ing sites. The population density of Raccoons in this
study was also measured as it influences home range
and contact rate.
Study Area and Methods
Trapping took place at a private garbage dump
(44°34’N, 76°20’W) and at a compost bin on the
grounds of the Queen’s University Biological Station
40 km north of Kingston, Ontario (44° 35’N, 76° 19° W).
The area surrounding the dump consisted of farm land
(livestock), forest, marsh, and cottages (most of which
were only occupied during the summer). The entire
65
66 THE CANADIAN FIELD-NATURALIST
study area was about 460 ha. Fifteen Raccoons (eight
females and seven males) were collared between 20
May and 27 June 1995. Raccoons were captured us-
ing Tomahawk #106 (Tomahawk Live-trap Company,
Tomahawk, Wisconsin, USA), and Havahart #1079
(Havahart Live Trap Company, Niagara Falls, Ontario,
Canada) live-traps. All Raccoons were ear-tagged
(numbered size | and 2, National Band and Tag Com-
pany, Newport, Kentucky), vaccinated against rabies
(Imrab® inactivated rabies vaccine, Merieux, Inc.,
Athens, Georgia, USA) and canine distemper (Fromm
D, modified live virus, SOLVAY animal health, Inc.,
Mendota Heights, Minnesota, USA). They were im-
mobilized by intramuscular injection of ketamine hy-
drochloride (Rogar/STB Inc., London, Ontario, Can-
ada) and xylazine hydrochloride [Rompun] (Bayvet,
Rexdale, Ontario, Canada) [30 mg/kg body weight
ketamine, 10:1 ratio ketamine:rompun]. We deter-
mined their sex and extracted a first premolar tooth for
age determination by cementum analysis (Johnston
et al. 1987). Each animal was then fitted with an adjus-
table radio-collar [151 to 152-Mhz] (Lotek Engi-
neering Inc., Newmarket, Ontario, Canada) and rel-
eased at its point of capture.
The radio-tracking system consisted of a four-
element Yagi antenna, 151 MHz (FM) transmitters
mounted on whip antenna collars (Lotek Engineering,
Newmarket, Ontario), one programmable hand-held
receiver (Lotek model SRX-400; Lotek Engineering,
Inc., Newmarket, Ontario) that operated in the 151-
152 MHz range, one hand-held compass, and a four-
wheel drive pick-up truck. Animals were given at
least seven days to acclimatize to their collars before
radio-tracking began, in accordance with White and
Garrott’s (1990) recommendations. The tracking per-
iod lasted from 21 June to 16 October 1995 with
attempts being made to locate each Raccoon two to
three times per week. Since only one telemetry receiver
was available, sequential rather than simultaneous
bearings had to be taken. A maximum interval between
first and last bearings of 10 min was set to minimize
telemetry error caused by animal movement (except
for bearings taken during the day when the animals
were inactive, at which time the interval may have
been longer). In a study by Gert and Fritzell (1996),
23% of the locations came from triangulations with
between-bearing intervals in excess of 8 min. For this
reason, the 10 min cut-off was deemed reasonable for
this study.
Continuous radio-tracking (i.e., location of the ani-
mals at least every 15 min (Harris et al. 1990)) was
not feasible with only one receiver; therefore, for this
study, discontinuous tracking was performed. Location
estimates were made for each animal three or four times
between dusk and dawn at roughly 2-h intervals, and
once during the following afternoon to determine day-
time resting sites. The tracking schedule was construct-
ed by randomly selecting six of the collared animals
Vol. 118
trapped at the dump for one given tracking night. The
remaining Raccoons were then tracked on the next
scheduled night. A different set of Raccoons was ran-
domly chosen for the following tracking night and so
on. Dates of tracking nights were randomly selected
for each week.
Three types of location estimate techniques were
used: scanning, triangulation, and homing. Scanning
involved tuning into the collar frequencies of the dump
animals while the researcher sat in the middle of the
dump area. Data from telemetry accuracy tests indi-
cated a mean transmitter-receiver distance of 240 m+
30 m (n=20) when the signal was picked up at a gain
of 10. A Raccoon was therefore considered to be in a
radius of this distance from the center of the dump area
if its signal was detected from there at a gain of 10 or
less. Most of the locations for the dump animals were
obtained by triangulation. This technique involves tak-
ing directional bearings from two to three different
receiver sites at known locations and using these to
estimate the true location of a remote transmitter on
the animal’s collar (White and Garrott 1990).
Accuracy tests were performed to determine the
error associated with locations estimated by triangu-
lation in this study. Bearing accuracy has two compo-
nents: bias (the average difference between the true
bearing and the bearing estimated by the receiving
system for a series of receiver-transmitter locations),
and precision, which is the standard deviation of these
errors (White and Garrott 1990). The bias was 9° and
was significantly different from O° (t=3.61, n=63,
P<0.001; one sample t-test (Zar 1996)). Therefore 9°
was subtracted from all bearings. Precision of the sys-
tem was + 20°.
Screening criteria derived from telemetry accuracy
tests were applied to all bearings to eliminate errors
due to signal bounce. All bearings which did not inter-
sect with other bearings taken on the same transmit-
ter were removed. All bearings taken from receiver
sites associated with large errors (high levels of sig-
nal bounce) were removed from subsequent analysis.
Also, bearings taken when the transmitter-receiver dis-
tance was >2000 m were removed. In addition, all loca-
tions involving distances between transmitter and rec-
eiver of over | km were inspected for plausibility.
A computer program called TRIANG was used to
estimate animal locations from triangulated bearing
pairs and to calculate the distance between receiver
and transmitter for each bearing. TRIANG did not
compute animal locations when three bearings were
taken. In this case, locations were determined by plot-
ting the bearing angles in AutoCAD and estimating
the centre of the triangle created by the intersection
of the bearings.
Locations for two of the collared Raccoons were
usually obtained by homing (White and Garrott 1990).
Locations of animals determined by homing are not
affected by error in the telemetry system; however, they
2004
are affected by the researcher’s ability to pinpoint the
den location on a map (White and Garrott 1990). All
locations determined by homing in our study were
plotted by hand on 1:10 000 maps of the area to +50 m
to obtain Universal Trans Mercator Co-ordinates
(UTMC).
Home ranges were estimated using the minimum
convex polygon (MCP) method (Mohr 1947), since
this is the only home range method that is strictly com-
parable between studies (Harris et al. 1990). Ranges
for both seasons were combined to compare degree of
overlap between seasons. Because it is advantageous
to use more than one home range estimate technique
(Voigt and Tinline 1980), the grid cell method of
home range analysis (Siniff and Tester 1965) was
also used. Size of the grid cells was chosen to reflect
radio fix accuracy based on the results of accuracy tests.
In order to enclose the uncertainty area associated
with scanning the dump for transmitter signals (and
this was larger than the area associated with triangu-
lation) a grid square would have to measure 480 m on
each side. Therefore this was the size of grid square
(23 ha) used in estimating grid cell home ranges. The
grid was oriented by centering a grid square over the
dump site.
Summer home ranges were calculated from teleme-
try data collected in June, July, and August; Septem-
ber and October fixes were used to calculate fall home
ranges. Two female Raccoons were excluded from the
analysis because insufficient locational fixes (<16)
were acquired during the study. A Mann-Whitney U
test (Zar 1996) and Statistica Version 6.0 software
(StatSoft Inc., Tulsa, Oklahoma) were used to test for
statistical differences in Raccoon home range size.
Raccoons were grouped into regular and occasional
dump visitors based on the number of nights each
animal was seen at the dump out of a total of 35
observation nights in a concurrent behavioral study
(Totton et al. 2002). Raccoons were defined as regu-
lars if they were observed at the dump on >51% of
all observation nights and occasionals if they were
seen at the dump on <51% of the observation nights.
Since only one telemetry receiver was available, and
hence discontinuous locational fixes had to be ob-
tained, detailed analysis of the movement patterns of
raccoons in this study was not possible.
Trapping to estimate the Raccoon population size
took place at the dump from 28 August to 19 Sep-
tember 1995. At this time of year, juveniles are larger
and easier to trap and handle than they are earlier in
the summer (Seidensticker et al. 1988). The number
of Raccoons in the study area was estimated using a
modified Petersen Index (Begon 1979). Density of
the dump population was not based solely on the area
of the trapping site (garbage dump = 2.3 ha) because
it was evident from telemetry data that some Rac-
coons were travelling from a much wider area to feed
at the dump. Instead, using the number of Raccoons
TOTTON, ROSATTE, TINLINE,
AND BIGLER: RACCOONS 67
calculated by the methods above, estimates were made
of the crude density of the population as defined by
Seidensticker et al. (1988) based on the average maxi-
mum width of the dump Raccoons’ summer (MCP)
home ranges (1530 m). Since Seidensticker et al.
(1988) did not specify how this distance was used to
calculate overall area, a square was centred over the
dump with each side equal to the distance calculated
and this was used for calculation of crude density. Its
area was 234 ha.
Results
For locations determined by triangulation, distance
between the observer and estimated transmitter loca-
tion ranged from 8.3 m to 1837.9 m and averaged
330.5 m (SD=239.3 m). Uncertainties in Raccoon
position for triangulated bearings (tan 20° x trans-
receiver distance) ranged from +3.0 m to +668.9 m
with a mean of +120.3 m and standard deviation (SD)
of 87.1 m (n=1181). Overall locational uncertainty,
including that associated with scanning and homing
techniques as well as triangulation, was +146.6 m
(n=1110).
No statistical differences were detected between
male and female ranges for values calculated using
either the MCP method (P=0.78) or the grid cell meth-
od (P=0.26). Therefore, male and female data were
pooled to compare summer and fall ranges. As well,
only three yearlings were trapped at the dump in this
study and home range data were available for two of
those. Consequently, statistical comparisons between
adult and yearling home range sizes were not per-
formed. No differences could be detected between
home ranges of Raccoons that regularly versus occa-
sionally visited the dump. Average Minimum Convex
Polygon (MCP) summer and fall home ranges for the
collared raccoons were 78.4 ha (SD=46.2 ha) and
45.6 ha (SD=29.7 ha), respectively (Table 1). Average
MCP summer/fall home range overlap was 31.2 ha
(SD=17.2). Average grid cell summer and fall home
ranges for the collared Raccoons were 143.3 ha
(SD=40.0 ha) and 116.9 ha (SD=24.9 ha), respective-
ly (Table 1). Average grid cell home range overlap
between summer and fall was 95.8 ha (SD=27.5).
Summer ranges of the Raccoons were significantly
larger than fall ranges using both the MCP method
(P=0.05) and the grid cell method (P=0.073).
The most widely ranging Raccoon (a male year-
ling) in the study was originally trapped at the dump
on 27 June. It was later located by telemetry near a
farmhouse 4 km northeast of the dump on 16 July.
By 18 July, it was visually identified at the dump site
again where it remained until 8 August. The only other
yearling of the dump Raccoons wandered a maximum
of 769 m from the dump during the summer. The aver-
age distance of the farthest fix from the dump during
the summer for the yearling Raccoons was 2608 m
(SD=1964, n=3) and for the adults (2 2 yr), 1239 m
68 THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE |. Summer (June to August) and fall (September to October) home ranges of 13 Raccoons which fed at a rural
Ontario garbage dump and at a compost heap in 1995!.
Method Number Summer
of fixes range
(summer) (ha)
mean (SD)? mean (SD)
MCP SZe (ile) 78.4 (46.2)
Grid Cell 44 (6.7) 143.3 (40.0)
Number Fall Area of overlap
of fixes range of ranges
(fall) (ha)
mean (SD) mean (SD) mean (SD)
34.1 (9.6) 45.6 (29.7) Sil= (GU)
33a (92) 116.9 (24.9) 95.8 (27-5)
'n=13 raccoons {7 males — 6 adults and | yearling; 6 females — 5 adults (all lactating) and 1 yearling}
2 §D=Standard Deviation
TABLE 2. Home range, movements and density of Raccoons in different areas of North America
Location Habitat Home Range Movements
(km?) (km)
Ontario rural 0.5-4.0 4-45
North Dakota rural 0.2-49 1-24
Minnesota rural 7-12 >3
Wisconsin
Toronto urban 0.4 <l
Ohio urban <0.2 0.4-0.5
(SD=547, n=10) (P=0.31). The Petersen estimate of
the number of Raccoons using the dump was 19,
with upper and lower 95% confidence limits of 35
and 12 respectively. Crude density was estimated at |
Raccoon/12 ha.
Discussion
Home ranges of Raccoons in North America are
variable (Table 2) but tend to average around 100 to
300 ha (1-3 km?) (Kauffmann 1982), but may range
from 18 to 2560 ha (0.18-25.6 km?) for adult males
in North Dakota, or 5.1 to 372 ha (0.05-3.72 km?) for
adult females (Stuewer 1943; Hoffmann and Gotts-
chang 1977; Fritzell 1978). Urban Raccoons tend to
have smaller home ranges than rural Raccoons (Ros-
atte et al. 1991) (Table 2). Range size may also vary
with season, data collection methods and method of
home range estimation (Harris et al. 1990). Distribu-
tion and abundance of food also affect home range
size (Hoffmann and Gottschang 1977). Small home
ranges are associated with high population densities
and abundant food (Hoffmann and Gottschang 1977).
Fall home ranges of Raccoons in this study were found
to be significantly smaller than ranges during the sum-
mer. This was expected as, during the fall, in northern
areas such as Ontario, Raccoon movement is thought
to decrease to conserve energy in preparation for the
winter denning period (Rosatte 2000). Large move-
ments by Raccoons during the fall, when food sources
are not as abundant, would likely result in a net ener-
gy loss thereby decreasing the condition of the animal
Density Reference
(/km?)
4-11 Rosatte and MacInnes 1989
Rosatte 2000; Rosatte et al. 2001
0.5-1 Fritzell 1978; Greenwood 1982
2-6 Schnell 1970; Mech et al. 1968
Dorney 1954; Schneider et al. 1971
Rosatte et al. 1991; Rosatte 2000
Cauley 1970; Schinner 1969
Hoffmann and Gottschang 1977
7-85
45-100
and decreasing the probability of surviving a harsh
winter. Movements of Raccoons in this study were
smaller than noted in other rural Ontario studies and
in other North American jurisdictions (Rosatte 2000;
Table 2). That may have been due to the concentrated
food sources in the vicinity of the dump in this study.
Raccoons have been known to change their movements
and home ranges to include new concentrated sources
of food; Seidensticker et al. (1988) discovered that
within 27 days, 21 of 23 collared Raccoons living in
the area had visited their artificial feeding station at
least once. The feeding site in their rural study area
was 0.5 ha in diameter and attracted Raccoons from a
127 ha area.
Home ranges of male Raccoons tend to be larger
than those of females (Stuewer 1943: Fritzell 1978).
The explanation as to why no difference was found
in this study may have been because either there was
no difference (due to abundant food sources at the
dump), or the small sample size prevented the differ-
ence from being detected. Lack of a difference between
home ranges of regular and occasional dump visitors
in this study may have been the result of either a true
lack of difference or the small sample size involved.
It may also be that the definition for “occasional”
was not adequate for comparative purposes.
The coarseness of the grid used for grid cell home
range analysis in this study may have led to an over-
estimate of home range sizes based on the fixes ob-
tained in this study (White and Garrott 1990) and
would explain why the grid home range estimates were
2004
larger than the MCP estimates. The advantage of the
grid cell method over the MCP method is that the
grid method takes into account the precision of the
telemetry system (White and Garrott 1990). Rac-
coons in Hoffmann and Gottschang’s (1977) study in
suburban Ohio with a Raccoon density of 1/1.46 ha
had average home ranges of 5.1 ha. Fritzell’s (1978)
study with a very low density of Raccoons in the spring
and summer averaged 2560 ha. Home ranges of Rac-
coons in previous Ontario studies (densities of 4 —
94/km7), varied between 50 and 400 ha (Rosatte 2000;
Broadfoot et al. 2001). Raccoons in our study fell
between these two extremes, though their home ranges
appeared to be smaller than average. However, home
range estimates obtained from our study data are prob-
ably underestimates of actual home ranges because the
study animals were monitored discontinuously over
only two seasons. In a Niagara-St. Lawrence trap-re-
capture study, annual movements of Raccoons averaged
10 km and ranged up to 150 km. In a similar Barrie,
Ontario, study, nightly movements of 4 km were com-
mon (Rosatte 1996*; 2000). Unless Raccoons are
tracked continuously with an accurate system for a
long period of time (e.g., 1 yr), their movements and
home ranges will probably be underestimated.
Radio-telemetry indicated that one yearling male
Raccoon occupied two distinct and widely separated
areas during the summer of 1995. The fact that no
points were located between these two ranges may
have been because he traversed the distance between
the two areas in the time between tracking nights. The
distance between the two discrete areas was 4 km.
Raccoons have been known to travel this distance in
a single night (Rosatte 1996*). In addition, the main
dispersal period for yearling males in some areas is
May to June (Fritzell 1978) and this might have in-
clined this Raccoon to make such a movement if he
were dispersing. A second explanation for the yearling
male Raccoons’ summer home range pattern is that it
may have been aided by a vehicle. Raccoons have been
known to ride on such vehicles as boats, transport
trucks and rail cars (Rosatte et al. 2001).
One yearling female Raccoon did not travel as far
from the dump as the yearling male noted above, in-
dicating that it may have been a post-disperser, having
immigrated to the dump area the previous fall. Two
out of three of the yearlings in this study were found
in excess of 2 km from their initial capture site within
the same season of their capture; this indicates that the
potential for rabies spread in an unvaccinated popu-
lation using a common feeding site is probably exac-
erbated by dispersal of the yearlings from the site dur-
ing the summer. This has been confirmed by Rosatte
(unpublished data) in a Raccoon rabies epizootic area
in eastern Ontario. As with the home ranges, men-
tioned above, these movements are probably minimum
estimates of actual distances travelled by the dump
Raccoons.
TOTTON, ROSATTE, TINLINE, AND BIGLER: RACCOONS 69
Although caution should be exercised in using data
from healthy animals to predict the behavior of rabid
ones, telemetry studies on two other species indicat-
ed that movements of rabid animals are not very
different from the movements of healthy ones (Storm
and Verts 1966; Artois and Aubert 1985). Storm and
Verts (1966) determined that the movements of a
radio-tracked rabid Striped Skunk (Mephitis mephitis)
in its last weeks of life were not statistically different
from the movements of non-rabid skunks. Also, a
radio-telemetry study by Artois and Aubert (1985) on
three wild foxes inoculated with rabies indicated that
these animals occupied a comparable home range
before and during the phase at which the virus would
have been shed. Rosatte (unpublished) found that
during a trap-vaccinate-release study in eastern On-
tario, movements of rabid Raccoons were not different
from movements of non-rabid Raccoons. If the same
rules hold true for Raccoons as they do for skunks or
foxes, then rabid Raccoons are likely to encounter
the same conspecifics as they would while they were
healthy. This indicates that data obtained from this
study have direct relevance to potential movements of
Raccoons in the study population should they become
infected with rabies. That is, dispersing yearling Rac-
coons using the common feeding site would probably
be the main vectors spreading the disease into areas
beyond the population.
Contact rates for Red Foxes (Vulpes vulpes) used
in rabies simulation models are estimates of potential
contact rates drawn from analysis of home range over-
lap obtained from radio telemetry data (Blancou et
al. 1991). The low precision of the telemetry system
used in this study prevented analysis of home range
overlap, spatial relationships and potential contact
rates. It was not possible to tell, with the coarseness
of the grid used for grid cell home range analysis, the
potential for Raccoons with overlapping ranges to con-
tact each other. Two Raccoons could be within the
same 23-ha grid cell area at the same time and yet be
unaware of each other.
Data from this study indicated extensive overlap of
home ranges within the population. Territoriality does
not normally occur in Raccoons (Kauffmann 1982;
Seidensticker et al. 1988) and has only been found for
adult males in the spring and summer in North Dakota,
at the northern edge of the Raccoons’ range and is
thought to be due to competition for access to females
(Fritzell 1978). Studies from more southern latitudes
failed to demonstrate territoriality in Raccoons (Stuewer
1943; Johnson 1970).
Although caution should be used in comparing den-
sities between studies, especially if different method-
ologies, seasons, and habitats are involved, population
densities for Raccoons are usually around one Rac-
coon per 8-10 ha (Kauffmann 1982) but may range
from one Raccoon per 100 ha in North Dakota and
northern Ontario (Fritzell 1978; Rosatte 1996*) to one
70 THE CANADIAN FIELD-NATURALIST
Raccoon per ().4 ha in more favourable habitat (Twich-
ell and Dill 1949). In southern Ontario, Raccoon
density averaged over 200 plots sampled was one
Raccoon/9-33 ha (Rosatte, unpublished) though den-
sities of up to one Raccoon/1.8 ha have been recorded
in forested park areas of Scarborough, Ontario (Rosatte
et al. 1991). Density for our study area falls within the
high end of the average range for Raccoon density in
southern Ontario. It should also be noted that in our
study, trapping for population estimates occurred at
the end of summer when the local population ex-
panded because the young-of-the-year were entering
the population.
Causes of mortality for Raccoons include starvation,
heavy parasitism, poison, dogs, automobiles, hunting,
trapping, canine distemper, and of course, rabies (Mech
et al. 1968; Rosatte and MacInnes 1989; Riley et al.
1998; Rosatte et al. 1991; Rosatte 2000); however,
the hunting season in this area was from 15 October
to 31 December (OMNR 1996*), after Raccoon den-
sity was estimated in this study. Thus, trapping and
hunting mortalities for the fall had yet to occur. Also,
a considerable number of the dump Raccoons were
trapped early in the study and vaccinated against rabies
and distemper; therefore, the major source of mortal-
ity in this population at the time of the study was
probably due to collisions with automobiles. Apart
from roadway mortality, the death rate of juveniles in
this population was probably very low until winter
food shortages set in. For this reason, the density
estimated for our population probably represents a
peak annual value.
Management Implications
Raccoon home range and movement data were used
to estimate areas that need to be treated to control Rac-
coon rabies in Ontario (Rosatte et al. 2001). Intimate
knowledge of Raccoon behavior provides benchmarks
to consider when determining the width of the popula-
tion reduction and vaccination zones in order to pre-
vent the spread of Raccoon rabies (Raccoon Rabies
Task Force 1992*). These data are also being used to
develop a Raccoon rabies model for Ontario which
will be capable of predicting the movement of Raccoon
rabies over time in the absence or presence of rabies
control strategies.
Acknowledgments
We thank R. Harmsen, R. J. Robertson (Queen’s
University), D. Voigt (Peterborough Ontario Ministry
of Natural Resources: OMNR), and D. Johnston for
helpful comments during the planning of the study and
on early drafts of the manuscript. Field assistance was
provided by L. Smail, J. Lugarich, and A. Thompson.
Logistical support was provided by M. Power and D.
Grieve, and Raccoons were aged by D. Joachim and
A. Silver (Peterborough OMNR). Many thanks to A.
Cross (Opinicon Resort) for allowing the researchers
access to his property. And finally, thanks to F. Phelan
Vol. 118
and F. Connor at the Queen’s University Biological
Station, and to M. Schunk (Queen’s University). This
study was supported by an operating and equipment
grant from the Ontario Ministry of Natural Resources.
S. Totton received funding from an Ontario Graduate
Scholarship and a Queen’s Graduate Award.
Documents Cited (marked * in text)
Ontario Ministry of Natural Resources. 1996. Hunting
and Trapping Regulations for the 1996 hunting season.
Raccoon Rabies Task Force. 1992. The raccoon strain of
rabies: recommendations to prevent its becoming estab-
lished in Ontario. Unpublished report. 25 pages.
Rosatte, R. C. 1996. 1996 raccoon rabies research and con-
trol annual report. Ontario Ministry of Natural Resources
internal report.
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Received 4 October 2001
Accepted 20 May 2004
Status of Marine Turtles in British Columbia Waters: A Reassessment
DONALD F. MCALPINE! , STAN A. ORCHARD?, KELLY A. SENDALL?, and Rop PaLm*
'New Brunswick Museum, 277 Douglas Avenue, Saint John, New Brunswick E2K 1E5 Canada dmcalpin @nb.aibn.com
>3Royal British Columbia Museum, 675 Belleville Street, Victoria, British Columbia V8W 9W2 Canada
‘Strawberry Isle Research Society, Box 213, Tofino, British Columbia VOR 2Z0 Canada
>Present address: World Wide Fund for Nature, GPO Box 528, Sydney, NSW 2001 Australia
McAlpine, Donald F., Stan A. Orchard, Kelly A. Sendall, and Rod Palm. 2004. Status of marine turtles in British Columbia
waters: a reassessment. Canadian Field-Naturalist 118(1): 72-76.
Marine turtles in British Columbia have previously been considered off course stragglers. Here we document 20 new reports
for Green Turtles, Chelonia mydas, and Leatherback Turtles, Dermochelys coriacea, for the province. Until recently there
had been no concerted effort to acquire data on marine turtle abundance or frequency off British Columbia. Observations
presented here allow a reassessment of marine turtle status in British Columbia waters. We suggest Green Turtles and
Leatherbacks should be considered rare vagrants and uncommon seasonal residents, respectively, off British Columbia and
that they are a natural part of the British Columbia marine environment.
Key Words: Green Turtle, Chelonia mydas, Leatherback Turtle, Dermochelys coriacea, British Columbia, status.
There are few published reports for marine turtles
in British Columbia waters. Marine turtles in the prov-
ince have generally been considered “straggler[s]”
(Kermode 1932) or “off course” (Gregory and Camp-
bell 1984). Nussbaum et al. (1983) ignore marine tur-
tles in their treatment of northwest amphibians and
reptiles, and marine turtles are not included in a recent
field guide to northwest reptiles “because sea turtles
rarely visit these shores” (St. John 2002). During the
preparation of a review of the status and conservation
of marine turtles in Canadian waters (McAlpine et al.
in press) recent occurrences of Green Turtles off Brit-
ish Columbia were encountered (McAlpine et al. 2002).
Here we document additional new reports for Green
Turtles, Chelonia mydas, as well as Leatherback Tur-
tles, Dermochelys coriacea, for British Columbia. These
new records nearly double the number of published
occurrences for marine turtles from the province. When
considered in the context of a recent compilation for
adjacent Alaska (Hodge and Wing 2000), these obser-
vations suggest a reassessment of sea turtle status in
British Columbia waters is warranted. The precipitous
decline in Pacific Leatherback numbers (Spotila et al.
2000), so serious it has led to a call for a moratorium
on long-line fishing in the Pacific Ocean (Anonymous
2002), also provides a timely context.
Based on terms used to document bird status in
Alaska, Wing and Hodge (2002) have proposed a
standardized terminology to describe marine turtle
occurrences. This terminology, ranging through seven
categories from accidental to abundant, is loosely based
on number of occurrences only. Although useful, this
system ignores the ecological context for occurrence.
Here we suggest modifying the system of Wing and
Hodge (2002) by adding, where appropriate, one of
four descriptors to their categories: resident, seasonal
72
resident, migrant, or vagrant. Resident refers to turtles
present year round, seasonal resident refers to turtles
present only at certain times of the year, migrant refers
to turtles moving through a broad area to another loca-
tion, vagrant refers to turtles occurring outside their
normal resident or migratory range. We use this system,
in conjunction with that of Wing and Hodge (2002),
to describe marine turtle status in British Columbia.
There are 11 published reports for Green Turtles
(Carl 1955; Radovich 1961 cited in Stinson 1984;
Hodge and Wing 2000; McAlpine et al. 2002) from
British Columbia and 14 reports of Leatherbacks (Ker-
mode 1932; Carl, 1944, 1960; MacAskie and Forester
1962). Published and unpublished marine turtle reports
for British Columbia prior to 1982 are summarized in
Stinson (1984). Table | lists one unpublished British
Columbia Green Turtle report, included by Stinson
(1984) and six new ones; three unpublished
Leatherback reports included in Stinson (1984) and
10 new Leatherback occurrences. There are currently
26 British Columbia reports for the Leatherback
accompanied by sufficient locality data to map
(McAlpine et al. in press), as well as other reports
which are not site-specific. All of the 16 British Colum-
bia Green Turtle reports can be map plotted (McAlpine
et al. 2003). Several of the recent Green Turtle records
are supported by photographic evidence (Figures 1-
3), as are four of the Leatherback sightings (Figure 4;
Table 1). The skull in Figure | is readily identified as
that of C. mydas using the figures in Wyneken (2001).
This stranding is reported in issue Number 2 of KSM
Wutsiin, the official newletter of Hartley Bay School.
Unfortunately, the skeletal remains of this turtle were
not retained. Detailed necropsies carried out on the
Green Point and Matlahaw Point C. mydas are now
archived at the Royal British Columbia Provincial
2004
MCALPINE, ORCHARD, SENDALL, AND PALM: MARINE TURTLES 73
TABLE |. Recent occurrences of marine turtles from British Columbia waters.
Date Location
Chelonia mydas
22 November 1996 Hartley Bay
early November 1998 mouth of Tlell R
early November 1998 5 km S of Tlell R
6 November 2001 4km N of Tlell R
20 December 2001 Greene Point
21 January 2002 Matlahaw Point
Dermochelys coriacea
mid-July 1970 Sharbau Island
summer 1977 Off Ucluelet
September 1977 Off Ucluelet
30 August 1981 Skidiyate Inlet
Hectate Strait
Esperanza Inlet
1 September 1981
16 September 1982
August 1993 Clerke Point
26 May 1996 Mt Douglas Park
May 1997 Kyuquot Sound
September 1997 SE of Langara Island
Spring 1998 Tofino
6 September 2000 __ off shore
4 August 2001 off Langara Island
'PC = personal communication.
3525)
S336)
SS nS9:
SS esi)
49° (3'
49° 23'
S130;
49° 55'
49° (0!
Sul:
53° 20'
49° 52'
50° 05'
49° 08'
50° 05'
54° 12'
49° 07'
48° 43'
54° 18'
18"
129215)
131° 56'
131° 54'
ISH aps)
125° 43'
126° 29'
128° 45'
126° 38'
125° 50’
131 730%
130° 30'
126° 44!
127° 48'
123° 58'
W27e213\
132° 58'
1252753:
127° 26'
1335210;
Latitude(N) Longitude(W) Comments
Carcass, Figure |
Carcass, PC!: W. Flood to DFM
Carcass, PC: W. Flood to DFM
Fresh carcass, carapace 78.7 cm, Figure 2
Fresh carcass, male, carapace 68.7 cm, Figure 3
Carcass, male, carapace 69.9 cm
Stinson (1984)
Stinson (1984)
Free swimming, RBCPM photo number 695
Alive in salmon gillnet, RBCPM photo number 749
Stinson (1984)
RBCPM photo number 826
Feeding on Cyanea, pc: J. Watson to G. Ellis
Free swimming/Times-Colonist, 1 June, page B2
Carcass, PC: G. Jamieson to DFM
Free swimming, large numbers of Vellela sp.
present, PC: S. Buchanan to S. Stebbins
Decomposed carcass, PC: to SAO
Free swimming, PC: K. Morgan to DFM
Free swimming, PC: E. Simkin to G. Ellis, Figure 4
Ficure 1. Skeletal remains of a dead Green Turtle stranded at Hartley Bay, British Columbia, 22 November
1996. The skull in this photo can be readily identified as that of C. mydas (Hartley Bay School photo).
74 THE CANADIAN FIELD-NATURALIST
Museum and the Strawberry Isle Research Society,
Tofino. A report prepared by a veterinary pathologist
following examination of the Green Point Turtle states
this turtle died from a bacterial infection to which it
may have been predisposed following exposure to
environmental stressors, such as low water tempera-
ture. The animal was also suffering from a moderately
severe case of pneumonia. The Matlahaw turtle ap-
peared healthy and cause of death was not determined.
Gregory and Campbell (1984) suggested the single
live Green Turtle from British Columbia reported by
Carl (1955) was “probably just off course”. On the basis
of minimum thermal tolerance in cheloniid turtles and the
few additional reports of live C. mydas. McAlpine et al.
(2002) concurred, considering the species “accidental”
in the province. Kermode (1932) identified the Leath-
erback as a “‘straggler” in the North Pacific, Carl (1944)
reported the species as “wandering” to British Colum-
bia waters, and Cook (1981*) considered Leatherback
Turtles observed in Canada were either “migrants or
strays”.
Stinson (1984), however, suggested occurrences of
sea turtles in the northeastern Pacific could not be dis-
missed as accidental but are influenced by temperature
anomalies in the ocean. While she found sightings of
marine turtles occur regularly during years of normal
ocean temperatures, greater numbers of turtles were
observed than expected when sea temperatures were
above the mean. Hodge and Wing (2002) noted that
in Alaska marine turtle occurrences are almost equally
divided between warm-water and normal-water years.
Most noteworthy was the complete lack of turtles in
cold-water years.
Whether the increased number of recent reports
reflects a real increase in the prevalence of marine
turtles off British Columbia, or simply increased public
awareness and reporting, is unknown. However, based
on their standardized occurrence terminology for
< ESTOORG Ata oy AR RY a ARAN et os Ga
FIGURE 2. This 78.7 cm Green Turtle came ashore fresh
dead on 6 November 2001, 4 km N of the Tlell
River, Queen Charlotte Islands, British Columbia
(V. Flood photo).
Vol. 118
FIGURE 3. This 68.7 cm male Green Turtle came ashore fresh
dead at Green Point, Vancouver Island, British Col-
umbia, on 20 December 2001. (P. Clarkson/Parks Can-
ada photo).
marine turtles, Wing and Hodge (2002) report that
marine turtles occur too often in Alaska waters to be
considered accidental. These authors consider marine
turtles a natural part of the Alaskan marine environ-
ment. Likewise, Stinson (1984) concludes marine
turtles are a regular part of the environment in the
northeast Pacific. Based on the frequency of reports,
Wing and Hodge (2002) considered the Green Turtle
and Leatherback Turtle as rare and uncommon, respec-
tively, in Alaska. Stinson (1984) identified a marine
turtle season of July to September in the northeast
Pacific Ocean and stated September was the critical
marine turtle month in British Columbia waters. How-
ever, nearly all of her British Columbia marine turtle
observations are of Leatherbacks. Currently, the sea-
sonal pattern of occurrence that appears to be emerg-
ing, both in British Columbia and Alaska, suggests
that D. coriacea is indeed most frequent during the
July to September period, while C. mydas is most
likely to be found stranded in the northeast Pacific
during October to December. It should be noted that
most British Columbia Green Turtle observations have
been of stranded turtles, often recently deceased.
Hodge and Wing (2000) observe that the low
frequency of hard shell turtles from Alaska waters
indicates these turtles are straying beyond their toler-
able range, while they consider Dermochelys in Alaska
as occupying marginal habitat that may not be con-
sistently used from year to year. The accumulating
number of marine turtle observations from British
Columbia suggests that these species are even more
frequent in British Columbia than Alaska. Following
2004
MCALPINE, ORCHARD, SENDALL, AND PALM: MARINE TURTLES 75
Ficure 4. Leatherback turtle photographed 4 August 2001 off Langara Island, Queen Charlotte Islands, British Columbia
(Erik Simkin photo).
Wing and Hodge (2002), and our own suggestions
above, we describe C. mydas as a rare vagrant and
and D. coriacea as an uncommon seasonal resident
in British Columbia waters. However, we would add
there has been no effort to methodically collect infor-
mation from dead stranded turtles nor, until a recent
initiative by the Vancouver Aquarium (C. Sbrocchi,
personal communication to DFM), to acquire sightings
data on marine turtle abundance or frequency off
British Columbia. Anecdotal information on several
Leatherback occurrences is included in the KSM
Wutsiin newsletter noted above, indicating canvas-
sing local communities, and especially native fishers,
could be a source of information on marine turtle
occurrences in British Columbia. Additionally, Glen
Jamieson (Pacific Biological Station, personal commu-
nication to DFM) reports that Leatherbacks are
“periodically seen off the west coast of [Vancouver
Island]” and Frank Bernard (Pacific Biological Station,
personal communication to SAO) reported that he had
seen as many as six Leatherbacks in a day 80-320 km
off the west coast of Vancouver Island. Reports of the
Pacific Ridley, Lepidochelys olivacea, and the Logger-
head, Caretta caretta, for Alaska (Hodge and Wing
2000) suggest focused investigations may reveal these
species also occur off the British Columbia coast.
Acknowledgments
We thank the following individuals for sharing
British Columbia marine turtle observations and infor-
mation with us and allowing us to include their reports
here: Scott Buchanan, Barry Campbell, Graeme Ellis,
Glen Jamieson, Marilyn Joyce, Wayne and Virginia
Flood, Ken Morgan, Carla Sbrocchi, Eric Simkin, Jane
Watson, Kris Willcock, and the late Frank Bernard.
In particular, we would like to thank Eric Hill and
Simone Westgarth of the Hartley Bay School for their
efforts in obtaining information that allowed identifi-
cation of the Hartley Bay turtle.
Documents Cited (marked * in text)
Cook F. R. 1981. Status report on the Leatherback Turtle,
Dermochelys coriacea. Committee on the Status of En-
dangered Wildlife in Canada, Ottawa, 17 pages.
Literature Cited
Anonymous. 2002. Moratorium on Pacific long-lining could
save leatherbacks. Marine Turtle Newsletter 97: 26.
Carl, G. C. 1944. The reptiles of British Columbia. Hand-
book Number 3. British Columbia Provincial Museum,
Victoria, British Columbia.
Carl, G. C. 1955. The green turtle in British Columbia.
Report of the Provincial Museum of Natural History and
Anthropology, Victoria, British Columbia 1954: B77-78.
76 THE CANADIAN FIELD-NATURALIST
Carl, G. C. 1960. The reptiles of British Columbia. Hand-
book Number 3. British Columbia Provincial Museum,
Victoria, British Columbia.
Gregory, P. T., and R. W. Campbell. 1984. The reptiles of
British Columbia. Handbook number 44. British Colum-
bia Provincial Museum, Victoria, British Columbia.
Hodge, R. P., and B. L. Wing. 2000. Occurrences of marine
turtles in Alaska waters 1960-1998. Herpetological Review
31: 148-151.
Kermode, F. 1932. A remarkable capture of Leatherback
Turtles off Bajo Reef, near Nootka Sound, West Coast of
Vancouver Island, British Columbia. Report of the Prov-
incial Museum of Natural History for the year 1931.
Victoria, B.C. Pages 6-7.
MacAskie, I. B., and C. R. Forrester. 1962. Pacific Leather-
back off the coast of British Columbia. Copeia 1962: 646.
McAlpine, D. F., M. C. James, J. Lien, and S. A. Orchard.
In press, Status and conservation of marine turtles in
Canadian waters. Jn Ecology, conservation and status of
reptiles in Canada. Edited by C. R. Seburn and C. A.
Bishop. Herpetological Conservation 3.
McAlpine, D. F., S. A. Orchard, and K. A. Sendall. 2002.
Recent occurrences of the green turtle from British Colum-
bia waters. Northwest Science 76: 185-188.
Vol. 118
Nussbaum, R. A., E. D. Brodie Jr., and R. M. Storm.
1983. Amphibians and reptiles of the Pacific Northwest.
University of Idaho Press, Moscow, Idaho.
Radovich, J. 1961. Relationship of some marine organisms
of the northeast Pacific to water temperatures, particularly
during 1957 through 1959. California Fish and Game,
Fisheries Bulletin 112: 1-62.
Spotila, J. R., R. D. Reina, A. C. Steyermark, P. T. Plotkin,
and F. V. Paladino. 2000. Pacific Leatherback Turtles face
extinction. Nature 405: 529-530.
Stinson, M. L. 1984. Biology of sea turtles in San Diego Bay,
California and in the northeastern Pacific Ocean. MSc.
thesis, San Diego State University, California.
St. John, A. 2002. Reptiles of the Northwest: British Colum-
bia to California. Lone Pine Publishing, Edmonton, Alberta.
Wing, B. L., and R. P. Hodge. 2002. Occurrence terminology
for marine turtles. Marine Turtle Newsletter 95: 15-16.
Wyneken, J. 2001. The anatomy of sea turtles. U.S. Depart-
ment of Commerce, NOAA Technical Memorandum
NMEFS-SEFSC-470. 172 pages.
Received 27 February 2003
Accepted 20 November 2003
|
|
Introduced Marine Species in the Haida Gwaii (Queen Charlotte Islands)
Region, British Columbia
N. A. SLOAN and P. M. BARTIER
Parks Canada, Gwaii Haanas National Park Reserve and Haida Heritage Site, P.O. Box 37, Queen Charlotte, British Columbia,
VOT 1S0 Canada
Sloan, N. A., and P. M. Bartier. 2004. Introduced marine species in the Haida Gwaii (Queen Charlotte Islands) region, British
Columbia. Canadian Field-Naturalist 118(1): 77-84.
This historical review of a marine area’s introduced species was facilitated by geo-referenced marine species inventories of the
Haida Gwaii (Queen Charlotte Islands) region. One plant, 14 invertebrate, and two fish introduced species have been recorded
since the early 20" century from the marine waters around Haida Gwaii. Records of species occurrences are listed and mapped,
and modes of introduction are discussed. It will be important to continue documenting areas’ introduced species locations to
track the progress of invasions that could affect local marine ecosystem well-being.
Key Words: introduced species, marine, Haida Gwati, Queen Charlotte Islands, British Columbia.
*“... the control of alien marine species is in its infancy.”
(Bax et al. 2001)
Introduced (non-indigenous) marine species are of
global concern (Bax et al. 2001). The dynamism and
connectivity of marine ecosystems, mariculture and
shipping facilitate species’ introductions. The introduc-
tion of some species may be followed by rapid local
dispersal of propagules and appreciable ecological con-
sequences (Grosholz 2002). Introduced species know]-
edge is more developed for land and freshwater than
for marine ecosystems (Ruiz et al. 2000; Simberloff
2000; Bax et al. 2001).
Carl and Guiguet (1958) were the first to broadly
document species introductions in Pacific Canada. Cur-
rent awareness of the problem is growing in the region,
and Levings et al. (2002) have reviewed introduced
marine species found in the Strait of Georgia, south-
ern British Columbia.
Using the 30 introduced mollusks along the Pacific
coast of North America as an example, Carlton (1992)
reported the main modes of introduction as: (1) asso-
ciated with introduced Japanese and Atlantic oysters
imported for mariculture (approximately 27 species),
(2) via vessel hull fouling and organisms living in wood,
and (3) from overseas ships’ ballast water releases.
More recently, Chapman et al. (2003) reported that
along the U.S. Pacific coast, 24 of the 37 marine and
estuarine bivalve species commercially available as sea-
food are alien species.
We report on the documented presence of introduced
marine plants, invertebrates and fishes in the Haida
Gwatii (Queen Charlotte Islands) region of northern
British Columbia. No introduced marine birds or mam-
mals have been recorded. The plant and invertebrate
records, gleaned from the literature and museum col-
lections, are archived in the geographic information
system (GIS) databases of Gwaii Haanas National Park
Reserve and Haida Heritage Site (Sloan and Bartier
2000; Sloan et al. 2001). We excluded introduced
species whose total geographic range encompasses the
Haida Gwaii region, although, of course, their presence
could be inferred. An example is the amphipod Coro-
phium acherusicum from Asia and now known from the
northern mainland British Columbia coast (Bousfield
and Hoover 1997). The American Shad (Alosa sapidis-
sima) have long been known from the whole northeast
Pacific (Welander 1940), but only recently from Haida
Gwaii waters (Workman et al. 1996). Atlantic salmon
(Salmo salar) observations were from the Atlantic sal-
mon Watch Program web site: http://www.pac.dfo-mpo.
gc.ca/sci/aqua/AS WP_e.htm. The fish records are not
yet in our database.
Results and Discussion
For Haida Gwaii, accidental (or active) introductions
of one plant, 14 invertebrate, and two fish species asso-
ciated with fishery or mariculture development are
summarized in Table 1 and illustrated in Figures | and
2. Likely some of these species have spread northward
to Haida Gwaii from the more developed southern
mainland British Columbia and U.S. coasts where they
first became established. There have been introductions
of species to British Columbia targeted for mariculture,
such as Pacific Oyster (Crassostrea gigas) from Japan,
plus their attached associates (Quayle 1988) or parasites
(Bower et al. 1994). For example, the seaweed Sargas-
sum muticum is now ubiquitous coast-wide, including
Haida Gwaii (Figure 1). It was accidentally introduced
into southern British Columbia in the early 20" century
attached to Pacific oysters. Another example of collateral
introduction in British Columbia is the parasitic copepod
Mytilicola orientalis, likely introduced via Pacific Oyster
stock and now widely infesting Native Littleneck Clams
(Protothaca staminea) and Butter Clams (Saxidomus
giganteus) in southern British Columbia (Bower et al.
1994).
TL
Vol. 118
THE CANADIAN FIELD-NATURALIST
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SLOAN AND BARTIER
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80 THE CANADIAN FIELD-NATURALIST
Langara Island
Parry Passage
Cryplosula pallasiana
Lininodrilus monothecus
Cryptosula pallasiana
Graham
Rennell Sound Island
Rose
Masset Spit
Delkatla
Vol. 118
° Pelonaia corrugata
Trechus oblusus
Limnodrilus nonothecus
Kumdis Bay
Yakoun Bay
a
Skidegate
Inlet
Moresby
Island
Cartwright
Sound
Tasu
Sound
Bowerbankia gracilis
Sabia conica
Ciona intestinalis
Legend
a Sargassum mulicum
Mya arenaria
Ampithoe vallida
® Other invertebrate sightings as noted
FiGure |. Map of Haida Gwaii showing locations mentioned in the text and collection sites of introduced marine plant and
invertebrate species, based on data from Sloan and Bartier (2000) and Sloan et al. (2001).
Mariculture-associated Introductions
In 1977, concern over introduced aquatic species
issues stimulated establishment of the federal-prov-
incial Fish Transplant Committee (recently renamed
Introductions and Transfers Committee — ITC) under
Bowerbankia gracilis _
Schizoporella unicornis ®
Tubularia crocea
mandates from the federal Fisheries Act and the Bri-
tish Columbia Fisheries Act and British Columbia Wild-
life Act (BC 1990). The ITC evaluates potential risks
to the environment associated with introductions or
transfers of either finfish or invertebrates (“shellfish’’)
Hecate
Strait
Hotspring
Island
Dolomite "Burnaby"
Narrows
Harriet
Harbour
Houston Stewart
Channel
2004 SLOAN AND BARTIER: INTRODUCED MARINE SPECIES 8]
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FiGurE 2. Map of the northern British Columbia and southeast Alaska regions showing the density of Atlantic salmon obser-
vations. All data are from Fisheries and Oceans Canada’s Atlantic Salmon Watch Program: http://www.pac.dfo-mpo.gc.
ca/sci/aqua/ASWP_e.htm. [accessed May, 2004]. British Columbia data are from 1987 to 2002 and partitioned according
to Pacific Fishery Management Areas, and the Alaska data are from 1990 to 2002 and partitioned according to the
Alaska Department of Fish and Game Area Polygons.
into British Columbia marine or freshwaters. Besides _ genetic material into native species. Further, there are
the species themselves and their attached associates, concerns over potential ecological displacement of
there is the risk of introducing diseases, parasites or native species. The ITC issues licences to introduce
82 THE CANADIAN FIELD-NATURALIST
aquatic species into British Columbia or to transfer
species between domestic water bodies.
Shellfish mariculture remains a potential avenue of
species introduction to Haida Gwaii. A Masset-based
group has investigated the potential for local shellfish
mariculture for coastal community economic develop-
ment. Leased culture operations in Skidegate Inlet and
Rennell Sound remain active for Pacific Oyster culture.
These operations are unlikely a threat of introducing
oysters as local waters are too cold for oyster breeding
although they are suitable for growth of certified
disease-free juveniles (spat) from culture in southern
British Columbia. However, local waters may not be
too cold for oysters’ parasites or other associated
species. From 1997 to 2001, pilot raft culture sites
were tested to grow certified disease-free Weathervane
Scallop (Patinopecten sp.) hybrid (native x Japanese)
spat (B. Mark, Masset, personal communication). Only
the Rennell Sound site remains active for scallop cul-
ture (R. Lozon, Queen Charlotte City, personal com-
munication). The potential for species introduction is
likely low, because no successful settlement of hybrid
Weathervane Scallops has occurred in British Colum-
bia in the last decade (Island Scallops Ltd., Qualicum
Beach, personal communication).
Ships’ Ballast Water
Gauthier and Steel (1998) reported that Canada was
receiving approximately 52 million tonnes of ballast
water from foreign shipping annually with little pro-
tective policy or regulation. Indeed, the major vector
of introductions to Pacific North America has been
from shipping (Ruiz et al. 2000). Concerning Pacific
Canada, Levings (1999) mentioned the Canadian Bal-
last Water Management Guidelines issued by Transport
Canada in 2000 with an Annex (II) for the Pacific
coast aimed at preventing introduction of non-indige-
nous aquatic organisms (http://www.tc.gc.ca/Marine
Safety/). These Guidelines will become Regulations
under the Canada Shipping Act.
The Vancouver Port Authority has had a mandatory
ballast water program since 1997. It is based on the
assumption that mid-ocean ballast water exchange, with
water containing pelagic species not likely adapted to
coastal conditions, decreases likelihood of introducing
viable species into port waters (Levings et al. 2004).
Port authorities are now finding, however, that such ex-
change criteria are only partially effective (C. Levings,
Fisheries and Oceans Canada (DFO), personal com-
munication). Other British Columbia ports invoking
ballast water management are Nanaimo and New West-
minster. The north coast of British Columbia, with an
active deep-water international port in Prince Rupert,
however, has no ballast water program. Further, Lev-
ings et al. (2004) express concern about “intracoas-
tal” transport. For example, from Haida Gwaii there is
on-going barge and self-dumping log barge traffic with
Vol. 118
southern British Columbia and there has been relative-
ly recent international vessel traffic for mine ore con-
centrates from Tasu Sound (mine closed 1973) and
Harriet Harbour (mine closed 1968).
The ecological effects of introduced species such as
invertebrates on the Pacific coast are poorly studied
(Carlton 1992). It is sobering to reflect that, once in-
troduced, marine species may be difficult to control
and their ecosystem consequences may be damaging
(Simberloff 2000; Grosholz 2002). An example is the
European Green Crab, Carcinus maenas, introduced
to the San Francisco Bay area in 1989. The Green Crab
has since been recorded from Esperanza Inlet on the
northwest coast of Vancouver Island (Jamieson et al.
2002). As active predators, Green Crabs could affect
British Columbia intertidal fauna, as they have in
California (Grosholz 2000).
Times and attitudes have changed about introduc-
tions of marine species. In the 1980s, DFO discussed
introduction of the large, predatory Atlantic lobster
(Homarus americanus) around Haida Gwati. Barber
(1983) concluded that up to 7700 km? of Hecate Strait
area south of Skidegate Inlet, as well as Masset Inlet,
were suitable for lobster introduction. Now, such ini-
tiatives are contrary to agency mandates for sustain-
able, ecosystem-based management.
Among introduced marine species, Atlantic Salmon
(Salmo salar) currently has the highest ecosystem
and socio-political profile in British Columbia (Gross
1998; Volpe et al. 2001). Important issues include
escapement and persistence in river systems facilitating
competition for spawning habitat with native salmo-
nids. Further, the threat of continuing introductions
helps animate the vigorous debate over expansion of
salmon farming in British Columbia. Although Atlantic
Salmon have been reported from Haida Gwaii coastal
waters, there are no salmon farms in Haida Gwaii, and
there are no records at this time of Atlantic salmon from
within Haida Gwaii rivers and streams (V. Fradette,
DFO, personal communication).
This overview of a marine region’s introduced spe-
cies was facilitated through marine species inventories
from the historical literature of the Haida Gwaii region.
We do not claim that it is complete, but it is a start. It
will be important to continue documenting introduced
species reports to track the progress of introductions
that could affect local marine ecosystem well-being.
Acknowledgments
We thank C. D. Levings of Fisheries and Oceans
Canada (DFO) for reviewing an early draft and G. E.
Gillespie (DFO) for information on fishes.
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Received 27 December 2002
Accepted 11 June 2004
Ruby-throated Hummingbird, Archilochus colubris, Entanglements in
Burdock, Arctium spp., at Delta Marsh, Manitoba
HEATHER L. HINAM!, SPENCER G. SEALY, AND Topp J. UNDERWOOD
Department of Zoology, University of Manitoba, Winnipeg, Manitoba R3T 2N2 Canada
'Present Address: Department of Biological Sciences, University of Alberta, Edmonton, Alberta T6G 2E9 Canada
Corresponding author sgsealy @cc.umanitoba.ca
Hinam, Heather L., Spencer G. Sealy, and Todd J. Underwood. 2004. Ruby-throated Hummingbird, Archilochus colubris,
entanglements in burdock, Arctium spp., at Delta Marsh, Manitoba. Canadian Field-Naturalist 118(1): 85-89.
Exotic burdock (Arctium spp.) pose a risk of mortality for small native birds, such as the Ruby-throated Hummingbird (Archi-
lochus colubris), which may become entangled in its burrs. At Delta Marsh, Manitoba, we found 11 hummingbirds and five
individuals of four species of songbirds entangled on burdock in the dune-ridge forest over a 20-year period. Entangled birds
were mostly migrants. Most hummingbirds caught were juvenile males, whereas the few songbirds were mostly adult males.
We suspect that hummingbird entanglements resulted from an attraction to the purple flowers of burdock, but aggressive
interactions with conspecifics and other factors may have been involved. Birds may be at a higher risk of entanglement at
important migratory stopover sites, such as Delta Marsh, where both burdock and large numbers of birds are concentrated in
a small area.
Key Words: exotic plants, burdock, Arctium spp., fatal entanglement, Ruby-throated Hummingbird, Archilochus colubris, pas-
serines, mortality, Delta Marsh, Manitoba.
Exotic species often exert negative effects on the
survival of native flora and fauna (Atkinson 1989). This
is exemplified by the relationship between burdock
(Arctium spp.) and small birds and bats in North Amer-
ica (McNicholl 1988, 1994). Four species of burdock
were introduced from Eurasia into North America in
the early 1600s (Gross et al. 1980; Harms 2001). All
four species of burdock develop seed heads covered
with burrs that stick to passing animals, thus dis-
persing the seeds (McNicholl 1988). These burrs are
hazards for small birds and bats because individuals
may become entangled in the hooked bracts and die
(McNicholl 1988, 1994). The effect of such entangle-
ments on bird populations may be magnified when
the plants are concentrated in small areas where birds
nest or forage during migration.
For many songbirds, the dune-ridge forest that sepa-
rates the south shore of Lake Manitoba from Delta
Marsh (50°11 N, 98°19’ W), Manitoba, is an important
breeding area (Goossen and Sealy 1982; MacKenzie
et al. 1982) and migratory stopover site (den Haan
1996). Three species of burdock (A. minus, A. lappa,
A. tomentosum) have been documented in the area, but
Common Burdock (A. minus) is the most abundant,
occurring along the edge of the marsh and in the ridge
forest, as well as in ditches and at other disturbed
sites (Shay 1999). The composition of the understory
of the ridge forest has changed over the last 30 years
and the amount of burdock apparently has increased
(Kenkel and Graham 1994; S.G. Sealy, personal obser-
vations). With this apparent increase, Delta Marsh has
the potential to become a trap line for small birds such
as the Ruby-throated Hummingbird (Archilochus colu-
bris). Indeed, this species has been one of the most
frequently discovered entangled in burdock (McNicholl
1988, 1994; Raloff 1998; Nealen and Nealen 2000).
Here we document additional cases of mortality of
Ruby-throated Hummingbirds and songbirds due to
entrapment on the seed heads of burdock at Delta
Marsh, Manitoba.
Entanglements
Sealy and co-workers have studied songbird popu-
lations in the ridge forest at Delta Marsh since 1973,
but it was not until 1983 that the first bird was found
entangled on burdock. The decomposed remains of a
Ruby-throated Hummingbird were discovered that
spring, but death had occurred the previous year. Since
then, 10 more hummingbirds have been found, all but
one in August 1985 (Table 1). One of these was alive
and released, leaving behind several feathers stuck to
the burrs (Table 1). From 1977 to 1979, 1981 and 1983,
hummingbirds were banded in conjunction with gen-
eral songbird banding in the ridge forest from mid-May
through the end of August. The timing of the entan-
glements in 1985 coincided with the fall migration of
hummingbirds through the ridge forest in August
(Figurel). However, except for the live hummingbird,
the dates of entanglement only approximate the time of
death because the rates of decomposition and mummi-
fication are not known. Thus, some hummingbirds
could have been killed earlier in August.
Despite sporadic searching since 1985, only one
other entangled hummingbird was found, in 2002
(Table 1, Figure 2), but since 1994, five individuals of
four other species have been found entangled fatally
(Table 2). Another record consisted of only a few
feathers from an unknown passerine species, possibly
85
86 THE CANADIAN FIELD-NATURALIST Vol. 118
TABLE |. Records of Ruby-throated Hummingbirds entangled in burdock at Delta Marsh, Manitoba.
Date Age/Sex! Condition Specimen No.”
19 May 1983 Unk/unk Decomposed: overwintered, wings, ventral feathers attached 4986
15 August 1985 Unk/unk Released, feathers stuck on burdock 29817
18 August 1985 HY/female Recently caught (intact) 4982
18 August 1985 HY/male Recently caught (intact) 4983
18 August 1985 Unk/unk Partially decomposed: attached by ventral and wing feathers 4985
19 August 1985 HY/female Recently caught 4981
19 August 1985 AHY/male Partly decomposed 4984
19 August 1985 AHY/male, — Facing each other with burrs in between
HY/male (fresh and mostly intact) 4987 A,B
21 August 1985 HY/male Stuck across burr (fresh, mostly intact) 4980
14 September 2002 HY/female Decomposed, sternum visible 499]
"Unk = unknown, HY = hatch year, AHY = after hatch year.
Bird specimens deposited in the vertebrate collections of the Manitoba Museum, Winnipeg, Manitoba, Canada.
>Feathers deposited in the University of Manitoba Zoology Museum, Winnipeg, Manitoba, Canada.
TABLE 2. Records of songbird species entangled in burdock at Delta Marsh, Manitoba.
Species Date Age/Sex! Condition Specimen No.”
Unknown passerine 15 August 1985 Unk/unk Feathers stuck on burr 29823
Golden-crowned Kinglet 30 October 1994 Unk/male Wings and breast attached (fairly intact) 4976
Ruby-crowned Kinglet 2 November 1996 AHY/male Left wing caught (fresh, intact) 4977
Common Yellowthroat May 1999 AHY/female | Decomposed: overwintered,
caught by one leg 4978
13 May 2000 AHY/male Decomposed: overwintered, caught
by breast, both wings 4979
Yellow-rumped Warbler? —_10 October 2002 HY/unk Fresh, caught by right foot, feathers
of right flank, left wing 4988
'Unk = unknown, HY = hatch year, AHY = after hatch year.
*Bird specimens deposited in the vertebrate collections of the Manitoba Museum, Winnipeg, Manitoba, Canada.
Feathers deposited in the University of Manitoba Zoology Museum, Winnipeg, Manitoba, Canada.
‘Banded 14 September 2002.
a sparrow (C. Dove, personal communication). This
bird may have become entangled and freed itself; alter-
natively it may have been preyed upon or scavenged.
Two Common Yellowthroats (Geothlypis trichas), a
species that nests at Delta Marsh, were found in spring
after apparently becoming entangled the previous year.
One Golden-crowned Kinglet (Regulus satrapa) and
one Ruby-crowned Kinglet (R. calendula), both boreal
forest breeders and late migrants, were found freshly
dead in the fall. In October 2002, a freshly dead
Yellow-rumped Warbler (Dendroica coronata) was dis-
covered less than one month after it had been banded
in the ridge forest. All four of these species have been
found trapped on burdock elsewhere (McNicholl
1988, 1994).
The sex and age of birds were identified where pos-
sible by characteristics of the plumage, feathers and
bills (Pyle 1997). Of the hummingbirds entangled, five
were males and three were females, whereas three
songbirds were males and one was a female (Tables
1, 2). Six hummingbirds were juveniles and two were
adults (Table 1). By contrast, three songbirds were
adults and only one was a juvenile (Table 2).
Discussion
Most birds entangled in burdock at Delta Marsh
likely were migrants. Although Ruby-throated Hum-
mingbirds nest at Delta Marsh (Underwood and den
Haan 2000) in small numbers, all entanglements were
discovered during their fall migration period through
Delta Marsh (Figure 1). Among the other species killed
on burdock, only the Common Yellowthroat breeds
commonly at Delta Marsh (Underwood and den Haan
2000). The preponderance of migrants in our sample
of burdock mortalities is interesting. Several small
songbirds, such as the Least Flycather (Empidonax
minimus) and Yellow Warbler (Dendroica petechia),
nest at high densities in the ridge forest (Goossen and
Sealy 1982; Briskie and Sealy 1989; S. G. Sealy, un-
published data), but neither species has been recorded
entangled in burdock there, although the Least Fly-
catcher is a documented victim elsewhere (Underwood
and Underwood 2001). Individuals of both species have
been observed perched on stems of burdock (Sealy and
Underwood, personal observations) and Sealy ob-
served two male Yellow Warblers, one chasing the other
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HINAM, SEALY, AND UNDERWOOD: HUMMINGBIRD ENTANGLEMENTS IN BURDOCK
87
13 16 19 22
August
FicureE 1. Number of Ruby-throated Hummingbirds found caught on burdock at Delta Marsh, August 1985 (1 = 9), in
relation to the number of hummingbirds banded per day throughout 1977 (n = 7), 1978 (n = 37) and 1979 (n= 4),
1981 (n = 23) and 1982 (n = 42).
that hit seed heads during the chase. Although they
became stuck, they extricated themselves within sec-
onds of impact. This observation notwithstanding,
accidental strikes on burdock seed heads likely account
for few mortalities. This may explain the infrequency
of entanglements among the resident songbirds, which
have not been observed foraging on burdock flowers
or arthropods attracted to them.
It is commonly assumed that birds become entangled
while foraging (McNicholl 1988). Although humming-
birds feed mainly while hovering (Robinson et al.
1996), their small size may be the reason they frequent-
ly become entangled. As noted by Nealen and Nealen
(2000), Ruby-throated Hummingbirds prefer reddish
flowers (Robinson et al. 1996; but see Miller and Miller
1971), although they do not specialize on a particular
species (Bertin 1982). Because burdock flowers are with-
in the red spectrum (Gross et al. 1980), hummingbirds
may be attracted to them in the ridge forest where there
are few of the hummingbird’s putatively preferred spe-
cies (Robinson et al. 1996; Shay 1999).
Birds may also become entangled while foraging
for insects that inhabit the flowers or the seed heads.
Insects may comprise up to 60% of the diet of Ruby-
throated Hummingbirds and individuals have been
known to glean larval lepidoptera and other insects
from the surface of plants (Robinson et al. 1996). Over
20 species of insects from three Orders, Lepidoptera,
Coleoptera and Hymenoptera, have been found on
burdock seed heads (Mulligan and Kevan 1973; Gross
et al. 1980). The kinglets and warblers may have been
attempting to take insects from the burrs when they
became entangled (see Needham 1909).
Entanglements may also result from social inter-
actions between individuals. The deaths of two male
hummingbirds on the same burr cluster (Table 1, MM
4987A and B) may have resulted when one individ-
ual attacked the other at the flower cluster and they both
became entangled as the interaction ensued. Sealy
watched a male Ruby-throated Hummingbird attack
another male as it hovered by a seed head. The hov-
ering bird became entangled by one leg, but extri-
cated itself within seconds. The attacker had already
flown away. Wind may also cause entanglements, buf-
feting birds against seed heads as they move through
the area (McNicholl 1988). Thus, identifying the factor
or combination of factors that promote individual bird
entanglements is difficult.
88 THE CANADIAN FIELD-NATURALIST
FIGURE 2. Ruby-throated Hummingbird entangled in
burdock found 14 September 2002, Delta Marsh
(photograph by T. J. Underwood).
The large number of hummingbird entanglements
in burdock over a short period in August 1985 seems
unusual. Burdock apparently has increased in abun-
dance on the ridge forest (Kenkel and Graham 1994)
since our studies began at Delta in 1973. This suggests
that the frequency of entanglement should have in-
creased or at least remained constant. However, search
effort has varied widely since 1985 and migration
rates and weather patterns affecting bird movements
through the ridge forest vary from year to year. Hence,
it is difficult to assess from occasional records the
overall effect of burdock at Delta Marsh on migrating
birds. Nevertheless, the growing number of reports of
burdock-related deaths in birds (e.g., McNicholl 1994;
Raloff 1998; Underwood and Underwood 2001) sug-
gests that this type of mortality may be more important
than originally believed, particularly at places like Delta
Marsh, and King’s Park in Winnipeg (Underwood and
Underwood 2001), where burdock and large numbers
of migrating birds are concentrated. Further study of
the interaction between birds and burdock and the pos-
sibly fatal consequences for birds should result in a
better understanding of the effects of this exotic plant
species on bird populations.
Acknowledgments
We thank Janis Klapecki for cataloguing bird speci-
mens in The Manitoba Museum and Carla Dove,
Vol. 118
Smithsonian Institution, for attempting to identify
feathers. Some specimens were collected by G. C.
Biermann, J. V. Briskie, H. E. den Hann, K. A. Hobson,
E. Kiviat, A. Mcllraith, and R. M. Underwood. H. E.
den Haan provided details on the banding of the Yel-
low-rumped Warbler from the files of the Delta Marsh
Bird Observatory and assisted with age/sex identifica-
tion of specimens. We thank the reviews, A. J. Erskine
and M. K. McNicholl, for their comments on the man-
uscript. Accommodation and facilities were provided
by the Delta Marsh Field Station (University of Mani-
toba). Officers of the Portage Country Club permitted
us to conduct some of the field work on their property.
Funding was provided by the Natural Sciences and
Engineering Research Council of Canada.
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Received 7 March 2003
Accepted 23 April 2004
Multiple Mating Results in Multiple Paternity in Richardson’s Ground
Squirrels, Spermophilus richardsonii
James F. Hare!, GLENDA Topp!, and WENDY A. UNTEREINER?
' Department of Zoology, University of Manitoba, Winnipeg, Manitoba R3T 2N2 Canada
* Botany Department, Brandon University, Brandon, Manitoba R7A 6A9 Canada
Hare, James F., Glenda Todd, and Wendy A. Untereiner. 2004. Multiple mating results in multiple paternity in Richardson’s
Ground Squirrels, Spermophilus richardsonii. Canadian Field-Naturalist 118(1): 90-94.
Microsatellite DNA primers developed from Columbian Ground Squirrels (Spermophilus columbianus) were used to establish
paternity in a Manitoba population of Richardson’s Ground Squirrels (Spermophilus richardsonii). Primers resolving
variation at six microsatellite loci allowed ascription of paternity to 32 of 85 offspring born among litters of 15 breeding
females sampled. While the failure to unambiguously document paternity for all juveniles precludes the use of these data to
address questions of sperm competition and male mating success, the results do provide direct evidence that multiple mating
by female Richardson’s Ground Squirrels results in multiple paternity within litters.
Key Words: Richardson’s Ground Squirrel, Spermophilus richardsonii, mating, microsatellite DNA, multiple paternity, Manitoba.
Differences in gamete size, and hence the differen-
tial investment made in gametes by males and female
ultimately define the sexes (Parker et al. 1972) and have
promoted the evolution of disparate reproductive strate-
gies. Males commonly enhance their fitness by obtain-
ing copulations with more than one female (Bateman
1948), maximizing the propagation of like copies of
their genes by siring as many offspring as possible.
Conversely, the enhancement of female fitness is typi-
cally achieved through choosiness, whereby females
mate only with males providing the greatest access to
resources (Verner and Willson 1966; Thornhill 1976;
Stanford 1995) and/or who are the most fit and con-
tribute good genes to the female’s progeny (Zahavi
1975; Weatherhead and Robertson 1979; Hamilton
and Zuk 1982). At a proximate level, anisogamy also
promotes sex-differential mating behaviour. The rela-
tively few, large, nutrient-rich eggs produced by females
necessitate only a single male ejaculate containing
vast numbers of small, nutrient-poor spermatozoans to
achieve fertilization, and thus female reproductive suc-
cess may not increase through multiple mating.
Despite these fundamental predictions following
from anisogamy, multiple mating by females is com-
mon in animals and can prove beneficial to females for
various reasons. Obtaining multiple male mates may
ensure fertilization (Hoogland 1998), enhance access
to resources (Gray 1997), promote parental care on the
part of males (Davies et al. 1996), confuse males as to
paternity and thus reduce the probability of infanti-
cide (Hrdy 1977), increase female fitness by ensuring
genetic compatibility between the female’s eggs and
at least some of the sperm (Zeh and Zeh 1996) or in-
cite sperm competition (Gomendio and Roldan 1993),
whereby the fitness of the female’s offspring is en-
hanced by virtue of the good genes contributed by the
victorious spermatozoans (Evans and Magurran 2000).
Where multiple mating occurs, it is critical to un-
derstand its implications to both males and females.
Advances in molecular biology have revolutionized
the study of reproductive behaviour, and revealed that
observations of male/female association and mating
behaviour may not be representative of parentage in
free-living animal populations (Quinn et al. 1987).
Methods for determining parentage (see Fleischer 1996
for a review) have also become more powerful and ac-
cessible, thereby providing researchers with an oppor-
tunity to obtain comparative data which address both
the proximate and ultimate questions pertaining to re-
productive behaviour.
Such a comparative picture has begun to emerge for
the ground-dwelling squirrels (Spermophilus spp.),
where multiple mating commonly results in multiple
paternity within litters, and the first male to mate with
a given female often sires a disproportionate number of
offspring within a litter. Hanken and Sherman (1981)
reported that 78% of 27 Belding’s Ground Squirrel
(S. beldingi) litters for which paternity could be deter-
mined using polymorphic blood proteins were multiply
sired by between two and three males. Similarly, 50%
of eight Thirteen-lined Ground Squirrel (S. tridecem-
lineatus) litters were sired multiply, with the first male
to mate siring 75% of offspring in those litters (Foltz
and Schwagmeyer 1989). Boellstorff et al. (1994) de-
tected multiple paternity in 88.9% of nine litters of
California Ground Squirrels (S. beecheyi) and Murie
(1995) reported multiple paternity in 15.8% of 165
Columbian Ground Squirrel (S. columbianus) litters.
Murie (1995), however, predicted that his data likely
underestimated the incidence of multiple paternity
given that only five polymorphic loci were used, and
only one of those had more than two alleles. Indeed,
using a more comprehensive and variable series of
microsatellite primers (Stevens et al. 1997), multiple
90
2004
paternity was detected in 64% of litters born to fe-
male Columbian Ground Squirrels that had mated mul-
tiply (Stevens, Strobeck and Murie unpublished data).
Of those litters, 77% were sired by two males, 21%
by three males, and 2% by four males. Further, there
was a distinct first-male advantage, with 65% of the
offspring sampled from among 77 litters sired by the
first male to mate, and a progressively declining pro-
portion of paternity success for subsequently mating
males (Stevens, Strobeck, and Murie unpublished data).
Despite the widespread occurrence of multiple pater-
nity and a first-male mating advantage, deviations from
that pattern are apparent among ground squirrels.
Using both protein isozymes and DNA fingerprinting
(see Burke 1989), Lacey et al. (1997) revealed that
multiple paternity among Arctic Ground Squirrels (S.
parryi) was relatively rare; it occurred in only | (9%)
of 11 litters examined and the first male to mate sired
the majority (90%) of the offspring in that litter. A
departure from the first-male mating advantage has
been detected in Idaho Ground Squirrels (S. brun-
neus), Where Sherman (1989) reported a last-male
mating advantage (a minimum of 66 — 100% of pups
sired by the last/longest attending male) in the five of
seven litters (71.4%) where multiple paternity was evi-
dent. Additional data for other Spermophilus species
will prove useful in determining whether these species
are unique in their apparent departures from the gen-
eral pattern, and thus how these expressions of multiple
mating and sperm precedence impact the behaviour
and fitness of males and females.
Richardson’s Ground Squirrels (S$. richardsonii)
are locally abundant throughout grazed areas of the
Great Plains (Michener and Koeppl 1985). Females
mate multiply (Michener and McLean 1996), and al-
though this may result in multiple paternity within lit-
ters (van Staaden et al. 1994, Michener personal com-
munication), direct evidence of multiple paternity is
lacking. Such data would contribute to our understand-
ing of reproductive behaviour, and open new avenues
for research into the contributions of paternal kinship
to social interactions (e.g., Holmes and Sherman 1982)
and patterns of dispersion among relatives in nature.
We applied primers developed by Stevens et al. (1997)
to prospective parents and offspring from litters of 15
breeding females in a Manitoba population of Rich-
ardson’s Ground Squirrels to test whether multiple
mating results in multiple paternity within litters.
Methods
Study site, research subjects, and sample collection
Research was conducted between 8 April and 26
July 2002 on a 1.5-ha section of a larger 5-ha cattle
pasture near Westbourne, Manitoba (50°10.190'N,
98°38.103'W). Richardson’s Ground Squirrels on that
site were live-trapped in National or Tomahawk traps
baited with peanut butter and were marked for per-
manent identification with numbered metal ear tags
HARE, TODD, AND UNTEREINER: MULTIPLE MATING Q|
(Monel #1 fish fingerling tags). Each squirrel was
also given a distinctive mark on its dorsal pelage with
black hair dye (Clairol Hydrience 52 Black Pear]).
Trapping was conducted during the mating season (12
through 25 April 2002) to determine mating dates of
females and to monitor the reproductive condition of
all squirrels. After mating had ended, trapping con-
tinued to assess gestational progress in females, and
a 2-mm tissue punch was taken from one pinna of each
adult (10 males, 18 females). Samples were placed in
1.5-ml microcentrifuge tubes in 95% ethanol, and
stored at 4 — 7°C prior to DNA extraction and subse-
quent molecular analysis. Fifteen females for which
mating and parturition dates were known, and for whom
ear punches had been obtained, and nest-burrow en-
trances located were chosen to provide litters for pater-
nity analysis. All juveniles in those litters were trapped
within three days of their first emergence from their
natal burrow, marked with ear tags and dye marks, and
tissue sampled as described for adults. Animal research
was conducted in accordance with the guidelines for the
use of animals in research set forth by the Canadian
Council on Animal Care.
Molecular analysis of paternity
Individual ear punches were placed in 1.5-mL micro-
centrifuge tubes, centrifuged in a speed-vac for 5 min
to remove the excess ethanol and digested at 55°C
for 4 — 6 hrs in 70 uL of a sterile cell lysis solution
(10 mM Tris-HCL, 100 mM EDTA, 2% SDS, pH
8.0) containing 3 — 4 uL Proteinase K (10 mg/mL).
Following the addition of 4 uL of RNase A, the tubes
were mixed by inversion and incubated at 37°C for
30 min. Proteins were precipitated by adding 23.5 uL
of 7.5 M ammonium acetate to each tube of cell lysate
and placing the samples on ice for 30 min. Tubes were
centrifuged at 14000 rpm for 3 min and the superna-
tant was transferred to a new 1.5-mL tube containing
70 wL isopropanol. Samples were mixed by inversion,
stored at -20°C for several hours and centrifuged at
14000 rpm for 2 min. Following the removal of the
supernatant, the pelleted DNA was washed in 75 UL
of ice-cold 75% ethanol and centrifuged at 14000 rpm
for 1 min. The ethanol was removed with a pipette
and the tubes containing the DNA were placed in
speed-vac for 5 — 10 min. The dried pellets were re-
hydrated in 40 uL of sterile TLA buffer (10 mM Tris-
HCL, 0.1 mM EDTA, pH 8.0) and stored at -20°C.
Amplifications were performed on a GeneAmp®
PCR System 9700 (Applied Biosystems, Foster City,
CA) in a 25-uL volume containing ~ 200 ng DNA,
0.8 mM dNTP, PCR buffer (0.1 M Tris-HCI pH 8.3,
0.5 M KCl, 15 mM MgCl, 0.005 g gelatin/10 mL
buffer), 0.5 units of Taq polymerase, and 0.2 UM con-
centrations of each of seven primers (GS3, GS12, GS14,
GS20, GS22, GS25, GS26) described by Stevens et al.
(1997). The cycling conditions were 94°C for 2 min
followed by two cycles of 94°C for 30 s, 58°C for 20 s,
72°C for 5 s, and 33 cycles of 94°C for 15 s, 54°C for
92 THE CANADIAN FIELD-NATURALIST
20 s and 72°C for 5 s followed by a final extension at
72°C for 30 s. PCR products were diluted (1:1) with
sterile water and | uL of each diluted product was
resolved by polyacrylamide gel electrophoresis on an
ABI 373 Automated Sequencer (Applied Biosys-
tems). Microsatellites were visualized and sized using
GeneScan® 3.1 and Genotyper® 2.1 software (Applied
Biosystems).
Results
Of the seven primers employed, one (GS22) result-
ed in multiple banding patterns and was excluded
from subsequent analysis. The remaining six primers
resolved meaningful variation among individuals and
were used in establishing familial relationships among
the individuals sampled. Based upon the observed fre-
quencies of the three to six alleles evident at those six
loci (Table 1), the probability that two randomly drawn
unrelated individuals will be identical at all loci is |
in 9577 (from equation in Patekau and Strobeck 1994),
Further, the probability that an unrelated male will be
excluded as sire given knowledge of the mother’s geno-
type is 0.91 (from equation in Chakravarti and Li 1983).
All calculations assume that the loci examined are
not linked, and provide highly conservative estimates
of exclusion given that they are based on pooled data
from dams, sires, and their offspring.
Paternity was definitively ascribed to at least one
juvenile within litters of all 15 dams included in the
study. In total, however, unique identification of the
male sire was achieved for only 32 of the 85 juveniles
that emerged in those litters. Based upon those iden-
tifications, multiple sires were detected in 12 of the
15 litters examined (80%), with a minimum of two
sires in 11 and a minimum of three sires in one of
those 12 litters (2.1 + 0.1 sires/litter; mean + SE).
Discussion
The microsatellite primers developed by Stevens et
al. (1997) proved effective in resolving multiple pater-
nity within litters of Richardson’s Ground Squirrels.
Indeed, with multiple sires in 80% of the 15 litters
Vol. 118
examined, multiple paternity is at least as common in
Richardson’s Ground Squirrels as it is in other Spermo-
philus species with the exception of California Ground
Squirrels.
Definitive genetic evidence of multiple paternity in
the present study suggests that the use of the primers
described by Stevens et al. (1997) in future studies of
the reproductive and social behaviour of Richardson’s
Ground Squirrels would prove quite fruitful. In concert
with data on mating behaviour of the sort presented
in Michener and McLean (1996), such studies could
address the outcome of sperm competition and its rela-
tion to mating order (Sherman 1989), the role of aggres-
sion and male territoriality in affecting male mating
success (Schulte-Hostedde and Millar 2002), and the
factors underlying mate choice such as the effects of
symmetry (Penton-Voak et al. 2001), body size
(Gwynne 1981), paternal effort (Huber et al. 2002),
and genetic relatedness (Bateson 1983; Chapman and
Crespi 1998). The use of these microsatellite loci to
assess relatedness among individuals (Queller et al.
1993) would also allow insight into the role paternal
kinship plays in influencing social behaviour (Widdig
et al. 2002). Additional markers, however, would be
necessary to comprehensively document the paternity
of each and every individual. Microsatellite primers
that were not employed in the present study, such as
GS17 and GS34 (Stevens et al. 1997) or the 13 Idaho
Ground Squirrel microsatellite primers described by
May et al. (1997), would likely prove useful in this
regard.
The alleles identified in our Manitoba population
(Table 1) differ from those described for the Richard-
son’s Ground Squirrels examined by Stevens et al.
(1997) in evaluating the efficacy of their primers on
other Sciurids (see Table 2 in Stevens et al. 1997).
Given that geographic variation, the primers employed
here should also prove useful for studies of dispersal
(Chapuisat et al. 1997), interpopulation differences
related to conservation efforts (Patekau and Strobeck
1994), and perhaps even in refining the taxonomy of
the ground-dwelling squirrels (Gill and Yensen 1992).
TABLE 1: Characteristics of microsatellite loci (from Stevens et al. 1997) applied in paternity analysis of Richardson’s Ground
Squirrels. Results are based upon allele frequencies from 10 adult male, 15 adult female, and 85 juvenile squirrels. Expected
heterozygosity and probability of identity were calculated according to formulae presented in Patekau and Strobeck (1994),
and probability of exclusion was calculated following the methods of Chakravarti and Li (1983).
Locus Alleles
GS3 2215229523 18233
GS12 147, 149, 152, 154
GS14 242, 244, 246
GS20 220; 222.237
GS25 138, 142, 144, 146, 148, 154
GS26 109, 111, 113, 115
Expected Probability Probability
heterozygosity of identity of exclusion
0.630 0.178 0.347
0.672 0.128 0.416
0.549 0.298 0.253
0.105 0.803 0.053
0.769 0.057 0.557
0.480 0.336 0.232
2004. HARE, TODD, AND UNTEREINER: MULTIPLE MATING 93
Acknowledgments Fleischer, R. C. 1996. Application of molecular methods to
We are grateful to Curtis Strobeck and Lindsey the assessment of genetic mating systems in vertebrates.
Carmichael of the University of Alberta for making Pages 133-161 in Molecular Zoology: Advances, Strategies,
Fa and Protocols. Edited by J.D. Ferraris and S. R. Palumbi.
the primers available to us and providing guidance
on the use of the Genotyper® software, respectively.
Gail Michener facilitated our work by allowing Mag-
dalena Kujath to obtain samples from her study pop-
ulation that proved useful in piloting the application
of this technique. Our understanding of microsatellite
methodology was enhanced through conversations
with Nate Lovejoy, Ross McGowan, and Jan Murie,
while Andrea Angus provided sound advice and assis-
tance in the lab. We thank Jennifer Cassin, Kristin
Melnyk, Melanie Sharpe, and David Wilson for capable
field assistance and the Johnson family of Westbourne,
Manitoba, for allowing us access to the squirrels on
their land. Funding for this work was provided in part
by a stipend from Human Resources and Development
Canada in the form of a Summer Career Placement
grant for Kristin Melnyk, and by the Natural Sciences
and Engineering Research Council of Canada in the
form of a University Summer Research Award to
Glenda Todd, and operating grants to James Hare and
Wendy Untereiner. Research infrastructure was also
provided by a Canada Foundation for Innovation Res-
earch Development Fund award to Wendy Untereiner.
This is paper number 301 of the Delta Marsh Field
Station.
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Received 29 May 2003
Accepted 15 June 2004
Demographic Patterns and Limitation of Grey Wolves, Canis lupus,
in and Near Pukaskwa National Park, Ontario
S. ANNE FORSHNER!?, PAUL C. PAQUET?, FRANK G. M. Burrows*, GRAHAM K. NEALE, KEITH D. WADE®.
and WILLIAM M. SAMUEL
'Department of Biological Sciences, University of Alberta, Edmonton, Alberta T6G 2E9 Canada
*Mailing address: P.O. Box 10, Jasper National Park, Jasper, Alberta TOE 1E0 Canada
Faculty of Environmental Design, University of Calgary, Calgary, Alberta T2N 1N4 Canada
4Bruce Peninsula National Park, Tobermory, Ontario NOH 2RO Canada
‘Garcia and Associates, Bozeman, Montana 59718 USA
°Pukaskwa National Park, Heron Bay, Ontario POT 1RO Canada
Forshner, S. Anne, Paul C. Paquet, Frank G. M. Burrows, Graham K. Neale, Keith D. Wade, and William M. Samuel. 2003.
Demographic patterns and limitation of Grey Wolves, Canis lupus, in and near Pukaskwa National Park, Ontario.
Canadian Field Naturalist 118(1): 95-104.
In response to concern regarding the growth and long-term viability of the wolf population in and near Pukaskwa National Park,
a study of demographic patterns and limitation of radio-collared wolves (Canis lupus) was completed between 1994 and 1998.
The mean annual finite rate of increase (0.96) suggested that population growth of wolves was limited and declining slightly.
Small pack sizes, high cumulative mortality, and low reproductive success also suggested a declining population. Two limiting
factors, ungulate biomass and human-caused mortality, were examined to determine the importance of each in limiting the
population growth of wolves. Ungulate biomass was involved because occurrence of natural-caused mortality was high (9 of 17
wolves) compared with other studies. In addition, consumption rates were low and similar to other studies where starvation
and other signs of malnutrition were noted. Further, Moose densities in the study area were low to moderate and below thresholds
indicating nutritional stress for wolves. Occurrence of human-caused mortality was high (8 of 17 wolves) suggesting that it was
also an important limiting factor, particularly given the low availability of ungulate biomass and reproduction noted in this study.
Based on present demographic patterns, ungulate biomass, and human-caused mortality, the wolf population likely will remain
at present low densities or continue to decline.
Key Words: Canis lupus, wolves, limitation, demographic patterns, Pukaskwa National Park, Ontario.
In 1996, researchers in the Greater Pukaskwa Eco-
system (GPE) (Figure 1) in Ontario postulated that two
limiting factors were negatively affecting the growth
and long-term viability of the Grey Wolf (Canis lupus)
population (Burrows et al. 1996"). These limiting fac-
tors were low availability of ungulate prey and high
mortality from human causes. Managers in Parks Can-
ada Agency were concerned because wolves are a
native species in the GPE. Thus, Parks is legislated to
protect and further, to ensure the long-term viability of
that population (Parks Canada 2000). This prompted
a study of wolves in the western half of the GPE, in-
_ cluding Pukaskwa National Park (PNP).
In this paper, we quantify population limitation of
_ wolves and examine the importance of ungulate bio-
mass and human-caused mortality in limiting the popu-
lation growth of wolves, 1994-1998. For these pur-
_ poses, we review and discuss demographic data on wolf
_ densities, population growth, reproduction, and mortal-
ity. Further, we report and discuss data on the avail-
ability of prey and rates of kill and consumption.
' * References marked with asterix (*) are listed in a separate
Documents Cited section following Acknowledgements,
all others are in Literature Cited.
Study Area
The study area comprised 4500 km? in the western
half of the GPE on the north shore of Lake Superior in
Ontario (48°N and 85°W) (Figure 1). The area includes
PNP (1878 km?) but also adjacent land with intensive
forestry, gold mines, towns and associated infrastruc-
ture.
Two distinct physiographic regions, coastal and inte-
rior, occur within the study area. The coastal region is
characterized by rugged topography with elevations
ranging from 189 to 650 m. Many lakes and rivers occur
in the area, creating a patchy landscape. The interior
region is a flat plateau characterized by a heavily erod-
ed landscape of mountains previously scoured by con-
tinental glaciers (Poitevin et al. 1989").
Mean annual precipitation is 74 cm along the coast
and 64 cm inland. Winter and summer temperatures
range from —13C° — 14.6C° for the coastal area and
—17C° — 15.9C° inland (Poitevin et al. 1989"). Ice cov-
er on Lake Superior ranges annually from 5-100%
(Skibicki 1994’).
Vegetation on the coast along Lake Superior and in-
land is mixed with associations of Balsam Fir (Abies
balsamea), Jack Pine (Pinus banksiana), White Birch
(Betula papyrifera), White Spruce (Picea glauca),
Black Spruce (Picea mariana), Eastern White Cedar
95
96 THE CANADIAN FIELD-NATURALIST
Lake
Superior
Legend
| __ Greater Pukaskwa
Ecosystem
M8 Pukaskwa National Park
wolf study area
Highway 17 N
Peete earier en eaten
: 20 km M
|Prepared by: Parks Canada
a | Pukaskwa National Park
2001 —_L. Parent
Vol. 118
FicureE |. Location of the wolf (Canis lupus) study area within the Greater Pukaskwa Ecosystem, Ontario, Canada (center
48°N, 85°W).
(Thuja occidentalis), and Trembling Aspen (Populus
tremuloides), with occasional Red Maple (Acer ru-
brum) and other hardwoods more locally abundant in
the southeastern corner of the study area.
Predatory mammals included Grey Wolf, Black Bear
(Ursus americanus), Red Fox (Vulpes vulpes), Lynx
(Lynx canadensis), River Otter (Lontra canadensis),
Fisher (Martes pennanti), American Marten (Martes
americana), Mink (Mustela vison), and Weasels (Mus-
tela spp.). Coyotes (Canis latrans) were rare except
around towns.
Moose (Alces alces) were the primary and most
abundant ungulate prey species for wolves. Woodland
Caribou (Rangifer tarandus tarandus) were few and
concentrated in small bands along the coast of Lake
Superior (Bergerud 1985). Numbers ranged from 6-14
in PNP, 1993-1997 (Wade 1993*, 1995*, 1997", 1999*).
White-tailed Deer (Odocoileus virginianus) were rare
in the GPE.
Methods
Capture and handling
We attempted to locate wolves in as many packs as
possible. Wolves were captured with modified leg-
hold traps in summer (7 = 21) and by using a net-gun
from a helicopter in early winter (n = 5). All wolves
|
2004
Legend
A Heron Bay
@ Mobert First Nation
© Marathon
tx White River
see22 Swallow River Pack
—-—- Bremner River Pack
—--— White River Pack
== Cascade Lake Pack
—-— Neys Pack
|_| Rein Lake Pack
— — Black River Pack
(Cee Be}
0 _20 km
| Prepared by: Parks Canada
te Pukaskwa National Park
2001 _L. Parent
iiaebn
*
° ~
2
annneeeed
FORSHNER ET AL.: GREY WOLVES IN PUKASKWA NATIONAL PARK 97
i Highway 17
Ficure 2. Annual (1 April — 31 March) home ranges of wolves in the study area, 1994-1998. Home ranges are 95% MCP.
Years for home ranges of packs were Swallow and Bremner River Packs, 1997-1998; White River Pack, 1996-1998;
Cascade Lake Pack, 1995-1996; Neys Pack, 1995-1997; Rein Lake Pack, 1994-1998; Black River Pack, 1994-1996,
1997-1998.
were immobilized with Telazol® (tiletamine hydro-
chloride (HCL) and zolazepam HCL, A.H. Robins
Co., Richmond, Virginia). Rectal temperature, pulse,
and respiration of wolves were closely monitored
throughout the procedure. Immobilized wolves were
examined for injuries, equipped with conventional
VHF transmitters (Lotek®, Newmarket, ON), weighed,
sexed, and aged. A committee for care of wild animals
approved all capture and handling operations (Wildlife
Animal Care Committee, Ontario Ministry of Natur-
al Resources, 1994-1997).
Biotelemetry
The target frequency for locating each radio-collared
wolf was four times/month in summer (April-Octo-
ber) and six to eight times/month in winter (Novem-
ber-March). Wolves were located by plane using a
portable receiver (Lotek® SRX-400), right-left switch
boxes, and paired three-element Yagi antennae mount-
ed on the wing struts of a fixed-wing aircraft (Cessna
185). Wolf location was recorded with a Global Posi-
tioning System (Garmin® 75 Aviation). For all loca-
tions, transmitter frequency, observer, date, time of
location, number of wolves, color of wolves, and pre-
sence of pups were recorded. Mean error of telemetry
(difference between observed and true location) was
calculated by using data we collected when regularly
locating stationary transmitters placed throughout the
study area. Location data were downloaded into a Geo-
graphical Information System (GIS [Tydac SPANS*])
for display and analysis of wolf movements.
Home Ranges
Ranges V® software (Kenward and Hodder 1996°)
was used to calculate annual (1 April — 31 March)
sizes of home ranges. To represent these areas we
used relocations of packs and 95% minimum convex
polygons (MCP) (Mohr 1947). All obvious extrater-
ritorial forays and dispersals were excluded from the
analyses (Ballard et al. 1997). We assumed home
ranges were defined when the observation-area curve
formed an asymptote (Kenward and Hodder 1996")
and locations were obtained throughout the year.
For each pack we used one radio-collared wolf/year
to represent the annual home range of the pack. This
is reasonable as locations from one wolf indicate
position of the entire pack when a high degree of
association exists among pack members (Kolenosky
98 THE CANADIAN FIELD-NATURALIST
and Johnston 1967; Fuller and Keith 1980; Fritts and
Mech 1981; Ciucci et al. 1997). This condition was
confirmed in this study by aerial observations of
packs during telemetry flights.
Accuracy of locations for the entire study was 150 m,
which was the mean error of telemetry obtained by
all participants. Accordingly, we changed the fix reso-
lution from the Ranges V® default of 1 m to 150 m.
This resolution was used to set the width of the bound-
ary strip that was included in polygon edges and
areas (Kenward and Hodder 1996"). We left the scal-
ing parameter at the software default of 1 m, which
means that each coordinate unit was | m from the next.
Density, pack sizes, and population growth
Density of wolves/1000 km? was calculated by
determining intra-pack densities (number of wolves
in pack/home range size) and averaging these den-
sities/year (Potvin 1987; Bjorge and Gunson 1989;
Okarma et al. 1998). The number of wolves in a pack
was based on the maximum number of wolves ob-
served in mid-winter (15 January-15 February). We
defined a pack as a group of two or more wolves that
traveled together for more than one month (Messier
1984). In two cases we had insufficient data to deter-
mine the sizes of home ranges, thus we followed Mes-
sier (1985) and used data from previous or subsequent
years.
Population growth or the mean annual finite rate of
increase was calculated based on the ratio of succes-
sive yearly estimates of density (Fuller 1989).
Reproduction
We did not observe wolves at dens during this study.
Dense vegetation and the secretive nature of wolves
precluded accurate visuals of wolf groups until Octo-
ber or November, at which time pups were difficult to
distinguish physically from adults. Hence, successful
year-specific reproduction was ascertained when: (1)
pups were captured in spring; or (2) a pack increased
in size from March to the following December, pro-
viding that sites of focal activities (e.g., pup-resting
areas) were observed in the intervening time (Messier
1985). Unsuccessful reproduction (i.e., no or failed
reproduction) was ascertained when: (1) a pack did
not demonstrate focal activity sites in the summer; or
(2) a pair remained together from March to the follow-
ing December (Messier 1985). Results are reported for
each pack by year.
Moose density
To examine availability of ungulate biomass to
wolves, we used Moose density (moose/1000km?)
based on aerial surveys using stratified random sampl-
ing (Gasaway et al. 1986*). More specifically, from
1993 to 1999 a single Moose density was calculated for
PNP and the three Wildlife Management Units (21A,
21B, 33) surrounding PNP where wolf packs were
distributed. There was little or no change in Moose
Vol. 118
density among yearly estimates (Burrows 2001), thus
we averaged results from 1993-1999 for each area.
Rates of kill and consumption of prey by wolves
The rates of killing and consumption of large prey
by wolves in four packs were studied by daily aerial
and ground observation, January-March 1998. The
Bremner River Pack was located 57 times between
18 January and 27 March 1998 (69 days) and the
Rein Lake Pack was located 57 times between 8 Janu-
ary and 26 March 1998 (79 days). Other packs locat-
ed were the White River Pack, 22 times between 11
February and 20 March 1998 (38 days) and the Swal-
low River Pack, 22 times between 9 February and 22
March 1998 (42 days). To calculate the kill rate, we
recorded the number of animals killed by wolves/
tracking period and the number of wolves present at
the kill (Messier 1985). Prey killed were located
from the air and from ground-based tracking. At kill
sites, we confirmed prey species, time, and cause of
death. For only the largest pack of wolves (Bremner
River), in addition to aerial locations, we simultane-
ously snow-tracked wolf movements and collected
scats to determine if all kill sites were found with the
aerial telemetry. Technicians at Big Sky Laboratory
(PO Box 0776, Florence, Montana 59833-0776) iden-
tified prey remains by macroscopic examination and
comparison with known material and hair-scale im-
pressions (Adorjan and Kolenosky 1969°).
In this analysis we considered only tracking sessions
where pack locations were not separated by >54 hr.
There were a few exceptions, however, where loca-
tions were separated by 72 hr. These periods were
retained in the analysis because wolves made a kill or
visited one of several garbage dumps the day they
were relocated making it unlikely that we missed a
kill. Nonetheless, kill rates in this study should be
considered minimums as wolves were not relocated
every day and some small prey such as deer (fawns
and adults), Caribou calves, Beaver, and other smaller
prey items may have been missed. It is unlikely, how-
ever, that we missed many of these kills because
White-tailed Deer and Caribou were rare in the study
area. We report kill rates as ungulates killed/wolf/day.
Rates of consumption were calculated based on
kill rates and average weights of wolves and prey. We
calculated the whole weight of wolves based on the
average from radio-collared adults and other wolves
found dead in the study area. The average edible
weights of Moose and beaver prey were assumed to
be 330, 261, 114, and 13 kg for adult male Moose,
adult female Moose, young-of-the-year Moose and
Beaver, respectively (Peterson 1977; Thurber and
Peterson 1993). We assumed the average weight of a
White-tailed Deer was 105 kg for an adult male (Kolen-
osky 1972; Forbes and Theberge 1996). Eighty % of
the adult deer carcass was considered edible (Pimlott
1967; Forbes and Theberge 1996). All consumption
rates are reported as kg prey/kg wolf/day.
2004. FORSHNER ET AL.: GREY WOLVES IN PUKASKWA NATIONAL PARK 99
TABLE 1. Sizes of annual home ranges and home range areas/wolf of seven packs of Grey Wolves (Canis lupus) in the study
area, 1994-1998.
Early Late
winter winter
number number 100% 95% Number
of wolves of wolves MCP MCP of radio Area/wolf
Year Pack in pack* in pack? (km?)° (km?)° fixes (km?)¢
1994-1995 Black River® 6 4 283 156 53 26
Rein Lake 3 3 310 249 38 83
1995-1996 Black River® 4 4 548 388 5 97
Rein Lake 3 3 600 533 58 178
Neys* 3} 4 269 244 96 8]
Cascade Lake! 1 204 170 26 170
1996-1997 Rein Lake® 2 | 561 Syi/ 39 279
Neys* 6 4 113 101 96 17
White River 2 2 407 345 Sy) 173
1997-1998 Black River® 4 3 468 450 74 113
Rein Lake® 2 1 692 600 87 300
White River 2, 2 589 498 65 249
Bremner River 6 3 760 644 93 107
Swallow River 5 3 567 500 62 100
Mean 8}55) DEG 455 388 63 139
SE 0.5 0.3 52 48 6.3 25
“Maximum pack size, 15 January-15 February.
> Maximum pack size, March.
© Sizes of home ranges were described using the minimum convex polygon method (MCP) (Mohr 1947).
‘Based on 95% MCP.
© Packs that used town dumps.
‘Home range size and home range area/wolf were not included in mean because the areas were not fully defined; i-e., the
observation-area curve was asymptotic but locations were not obtained throughout the year.
Mortality and survival of radio-collared wolves
We completed survival analysis for radio-collared
wolves from 20 August 1994 to 31 December 1998.
Wolves were re-located from time of capture until
mortality or the radio-signal disappeared. For known
deaths we estimated the date of mortality to the near-
est day using evidence from the field. When evidence
was unavailable, day of mortality was deemed the
midpoint of the interval between the last day the wolf
was known alive and the day it was discovered dead.
The cause of mortality was often identified on site
and when possible, confirmed by necropsy.
We calculated the cumulative mortality of radio-
collared wolves (n = 25) using the Kaplan-Meier prod-
uct limit estimator and Minitab (Version 12) software.
One of 26 captured wolves was shot by a trapper
while in the research trap and is not included in the
analysis. Cause of mortality was described using %.
We assumed the proximate cause of death was the
ultimate cause of death. We were unable to assess the
relative importance of other factors that may have
been involved.
Results
Twenty-six adult wolves were captured and then
radio-collared (n = 25) or tagged (n = 1) from 1994-
1997. These animals represented seven packs and
one lone wolf. Two of seven packs occurred almost
exclusively in the park and all wolf packs were radio-
collared in the study area. There were no other wolf
packs in the study area during this study. We followed
two packs in 1994-1995, four in 1995-1996, four in
1996-1997, and six in 1997-1998. The average mass
of adult female wolves (n = 11) was 26.9 + 1.4 kg
and that of adult males (n = 14) was 36.5 + 2.8 kg.
Home ranges
Sizes of annual home ranges (Figure 2) of seven
packs across 13 pack-years were adequately described
in this study (Table 1). Estimates accurately repre-
sented areas used by wolves because sizes of annual
home ranges were not correlated with number of
relocations (r, = 0.52, 0.05 > P > 0.02). Home range
sizes of packs and home range areas/wolf were vari-
able. The average annual home range size was 388 +
SE 48 km2 (95% MCP, n = 13, range = 101-644 km’)
100
(Table 1). The average home range area/wolf was
139 + SE 25 km? (95% MCP, n = 13, range = 17-300
km?) (Table 1).
Density, pack sizes, and population growth
Wolf density did not change over time; recorded
densities were 7.9, 9.6, and 7.2 wolves/1000 km? in
1995-1996 (n = 4 packs), 1996-1997 (n = 4), and 1997-
1998 (n = 6), respectively. Density declines, however,
if the Neys pack (Figure 2) is excluded from the
calculations. This pack exclusively used dumps for
food (Krizan 1997) and the home range was much
smaller compared with all other packs in the study
(Table 1). Accordingly, wolf densities were 7.1, 5.9,
and 5.9 wolves/1000 km? in 1995-1996 (n = 3 packs),
1996-1997 (n = 3), and 1997-1998 (n = 5).
Average mid-winter (15 January — 15 February)
pack size was 3.5 + SE 0.5 wolves (n = 14 pack-years)
(Table 1). This average declined in late winter (March)
to 2.7 + SE 0.3 (n = 14 pack-years). The number of
wolves in all except two packs remained stable or
declined, 1994-1998. Numbers fluctuated annually in
the Neys and Swallow River Packs (Table 2). Accord-
ingly, the mean annual finite rate of increase from
1995-1998 was 0.96.
Reproduction
From spring 1994 to spring 1998, wolves reproduced
successfully in eight of 22 pack-years (36%) (Table 3).
This was a maximum estimate of successful repro-
duction. In two of eight pack-years, we assumed wolves
had reproduced because large numbers of wolves were
noted in the packs in the following early fall and winter.
Moose density
Average densities of Moose varied among manage-
ment units. Management Unit 33 had the highest
Moose density (0.285 + 0.03-0.07 moose/km? 90% CI)
followed by Unit 21A (0.225 + 0.02-0.03), 21B
(0.220 + 0.02-0.03), and PNP (0.153 + 0.03-0.08).
Rates of kill and consumption
The Swallow River (3 wolves) and Bremner River
Packs (5) killed and consumed more ungulates than
the White River (2) and Rein Lake Packs (2). The kill
rates for each pack respectively were 6.8, 3.4, 0.0, and
0.0 ungulates/wolf/day. Consumption rates were 0.21,
0.11, 0.0, and 0.0 kg prey/kg wolf/day. The White
River and Rein Lake Packs did not kill any ungu-
lates; however, both packs scavenged from various
sources. The White River Pack scavenged from Moose
that were killed by vehicles or trains, from other wolf
kills, and from snare sets. The Rein Lake Pack scav-
enged from refuse in the town dump for White River
(Figure 2).
Mortality and survival of radio-collared wolves
As of 31 December 1998, 17 of 26 wolves radio-
collared or tagged from 1994 to 1998 were dead, only
four were confirmed alive, and five were missing. Eight
wolves died from human causes: trains killed three,
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 2. Highest numbers of wolves in packs in the study
area, 1994-1998. The number of sightings is in parentheses.
Pack size*
Pack 1994 1995 1996 1997 1998
Rein Lake 3(4) = 3(3) 1(2) 1> 0
White River D (2) ee (A) 2(2) 2(9) 2(2)
Bremner River 3(3)P
Cascade River 1(4) 0
Black River 4Q) VAC) w4e@) 3(4)
Swallow River 5 (D)o 3(3) 4(1)
Neys 3(4) — 4(2) 2(2)) 4)
* Maximum numbers of wolves seen in March.
> Pack sizes were confirmed by track-counts made from
the ground.
TABLE 3. Reproductive success of wolf packs, 1994-1998.
Year
Pack 1994. 1995 1996 1997 =1998
Black River +4 4 - + +
White River “pb = = = =
Rein Lake +b = = = =
Neys + - ?
Bremner River ~ +
Swallow River = =
“+ = reproduced successfully; — = did not reproduce
successfully.
> This pack likely reproduced successfully because many
wolves (10) were seen in late fall (November — December).
three were snared, and two shot. Nine wolves died
from natural causes: two starved, two were killed by
other wolves, four died from disease (three from mange
and one from blastomycosis), and one died from un-
known natural causes. We assumed this last wolf was
not killed by humans because we were in a remote
area, there were no signs of humans in the area, and
we found no bullets, snares, or other human devices.
Survival of radio-collared wolves decreased between
one and three years post-collaring. Wolves had a 32%
(SE 0.10) chance of dying in the first year, a 30% (SE
0.15) chance of dying in the second year, and a 57%
(SE 0.26) chance of dying in the third year. Median
survival time was 689 days or 1.9 years post-collaring.
Discussion
Population limitation of wolves
The growth rate of the wolf population in the study
area was limited from 1995-1998. The mean annual
finite rate of increase, 0.96, indicated a 4% rate of
decline. This rate of increase is not unique, however,
and similar rates recorded from other populations
have varied from 0.93-2.40 (Theberge and Strickland
1978; Fritts and Mech 1981; Ballard et al. 1987;
Hayes et al. 1991"; Messier 1991; Pletscher et al. 1997).
\
|
i
{
2004
In addition to the estimated rate of growth, there are
a number of other factors that suggest the wolf popula-
tion was declining slightly. First, pack sizes were small
and generally declining. Mean pack size (3.5 wolves +
SE 0.5) was much smaller than the average of 10 wolves
for packs that hunt moose in North America (Mech
1970). Furthermore, five of seven packs in this study
remained stable or declined in size from 1994 to 1998.
If this population were increasing in size, the number
of wolves within packs would likely increase. This
happened in the Yukon where rapid increases in pack
sizes of colonizing wolves were the primary means by
which an intensively reduced wolf population reached
their pre-reduction densities (Hayes and Harestad
2000).
High cumulative mortality of wolves is the second
factor that suggested a declining population. We com-
pared the cumulative rate of mortality from the first
year (32%) of our study with annual rates of mortal-
ity from other studies. There is little agreement among
researchers on the annual rate of mortality that causes
a population decline in wolves. However, Fuller (1989)
reviewed several wolf studies across North America
and concluded that populations would stabilize with
an overall annual mortality rate of 35%. Given this, it
appears the mortality rate in this study was sufficient
to account for the slightly declining rate of growth in
this study.
Coupled with high mortality of adult wolves, low
reproductive success of wolves in this study suggested
a population decline. Wolves reproduced successfully
in only 36% of possible occasions compared with
45-93% noted in other areas (Messier 1985; Potvin
1987; Peterson et al. 1998; Hayes and Harestad 2000).
We were unable to determine if wolves produced pups
that died soon after birth or whether whelping occurred
at all. Lack of denning, however, suggests no pups
were produced.
Limiting factors
We examined the importance of two factors that lim-
ited the growth of the wolf population in this study: un-
gulate biomass and human-caused mortality. Ungulate
biomass is commonly reported to limit growth of other
wolf populations (Mech 1977a; Fuller and Keith
1980; Packard and Mech 1980; Keith 1983; Messier
1985; Peterson and Page 1988) and data from this
study suggest it was important. The strongest data rep-
resented the occurrence of natural-caused mortality.
In this study, more than half (9 of 17) of radio-
collared wolves died from natural causes, which is high
compared with other North American studies (Peter-
son 1977; Carbyn 1982; Peterson et al. 1984; Ballard
et al. 1987; Hayes et al. 1991”). Starvation and intra-
specific aggression were responsible for four of nine
(24%) wolves dead in this study and have been report-
ed common in other populations where ungulate bio-
mass is low. For instance, in southwestern Quebec,
FORSHNER ET AL.: GREY WOLVES IN PUKASKWA NATIONAL PARK
10]
Messier (1985) noted wolves with fewer prey available
incurred more deaths from natural causes, namely
starvation and intraspecific aggression. In that area,
similar to our study area, moose density was 0.23
moose/km? and there were no other ungulate species
present. Similarly, Mech (1977a) noted occurrence of
starvation and intraspecific aggression increased as
prey availability declined in Minnesota.
Disease was the other natural cause of death ob-
served in this study. Four of nine wolves (24%) died
from either sarcoptic mange or blastomycosis. Blasto-
mycosis is enzootic in Minnesota (Schlosser 1980) and
Wisconsin (Sarosi et al. 1979; McDonough and Kuzma
1980) but until now (Krizan 2000; Paquet et al. 2001),
had not been reported from other wolf populations
across North America. This level of disease-related
mortality has not been reported in any other popula-
tions of wolves. In other populations, disease accounts
for 2-21% of wolf mortality (Carbyn 1982; Peterson
et al. 1984; Fuller 1989; Ballard et al. 1997) and is
often not even reported (Messier 1985; Ballard et al.
1987; Potvin 1987; Hayes et al. 1991°; Meier et al.
1995; Pletscher et al. 1997). The only other study
where disease clearly affected a wolf population was in
Alaska where rabies accounted for 21% of wolf mor-
tality and was a significant factor in the decline of the
population (Ballard et al. 1997). Disease cannot be
linked with certainty to low ungulate biomass but wolves
that lack food should be more vulnerable to disease than
those with more food available. Furthermore, food
shortage leading to nutritional stress could combine
with disease factors to increase the significance of
otherwise innocuous or sub-lethal conditions (Brand
et al. 1995).
We also examined rates of consumption of ungu-
late prey to determine the importance of ungulate bio-
mass as a limiting factor. Consumption rates for three
of four packs in this study were low (Bremner River,
Rein Lake, and White River). These packs consumed
<0.13 kg/kg wolf/day, which Mech (1977b) deter-
mined is the minimum rate of consumption required
for all wolves to survive and rear pups successfully.
Two packs killed no ungulates and relied on scav-
enging to survive (White River and Rein Lake Packs).
These data suggest that at least three of four packs
could have been limited by food. Indeed, in the White
River Pack, the dominant female failed to reproduce
the following spring and was extremely emaciated
(mass = 23.5 kg) when killed by other wolves later in
the summer. Similarly, the Rein Lake Pack was reduced
to one wolf by winter 1997. She did not reproduce
the following summer and to survive, she scavenged
mainly from the town dump for White River (Figure
2). She was dead as a result of mange by December
1998 (mass = 28.5 kg). The Bremner River Pack may
have been limited by food but data were not strong.
One wolf dispersed in summer 1998 and died from
unknown natural causes. Other wolves could have dis-
102
persed and died later because pack numbers dropped
from nine to three over the winter 1997-1998 (un-
published data). Some members of this pack, however,
did survive and reproduce two years in a row.
Most of the rates of consumption in this study are
similar to those from other areas where starvation and
other signs of malnutrition of wolves were noted. For
instance, Messier (1987) noted more deaths of wolves
from malnutrition in areas of low density of moose
(0.23 moose/km7) where wolves had 0.05 kg/kg wolf/
day (based on kill rate of 1.7 kg/wolf/day and wolf
mass of 32.3 kg). Peterson and Page (1988) noted
starvation and other indicators of severe nutritional
stress in an area of high Moose density (1.9 moose/
km?) when food availability fell below 0.12 kg/kg
wolf/day (based on kill rate of 4.0 kg/wolf/day and
wolf mass of 32.3 kg).
As a final method to assess the importance of un-
gulate biomass, we examined density of Moose, the
main prey for wolves in this study. Moose density
was low to moderate (0.153-0.285 moose/km?) and
similar to Moose densities in other areas where wolves
were nutritionally stressed. Messier (1987) found that
in areas where Moose density dropped below 0.4
moose/km*, wolves were nutritionally stressed. He
also reported that below 0.2 moose/km? wolf packs
could not subsist and (or) reproduce successfully
(Messier 1985).
The second limiting factor we examined was human-
caused mortality. Besides ungulate biomass, it is the
other most commonly reported factor that limits the
growth of wolf populations (Gasaway et al. 1983;
Keith 1983; Peterson et al. 1984; Fuller 1989; Noss
et al. 1996; Paquet et al. 1996"). In other areas where
human-caused mortality was considered the primary
limiting factor, it accounted for 69-80% of all mortal-
ity (Peterson et al. 1984; Ballard et al. 1987, 1997).
In our study area, human causes accounted for only
47% of mortality of adult radio-collared wolves. None-
theless, human-caused mortality is likely still impor-
tant, particularly given the low ungulate biomass and
reproduction noted in this study. Gasaway et al. (1983)
found that in areas with low ungulate biomass, har-
vest levels as low as 20% can limit wolf populations.
Fuller (1989) found that wolf populations with low
productivity can withstand less overall mortality be-
cause there are fewer pups, which often make up dis-
proportionate amounts of harvests.
In conclusion, the population growth of wolves in
this study area was limited and declined slightly based
on (i) mean annual finite rate of increase; (ii) small and
generally declining pack sizes; (iii) high cumulative
mortality; and (iv) low reproductive success.
Based on these demographic patterns, low availabil-
ity of ungulate biomass and existing levels of human-
caused mortality, this population likely will remain at
present low densities or continue to decline. This situa-
tion is challenging to managers for Parks Canada Agen-
cy because the study area, which includes a National
THE CANADIAN FIELD-NATURALIST
Vol. 118
Park, may not have a highly productive source popu-
lation for wolves. Further, protection for wolves out-
side the park is limited because few restrictions exist
regarding the nature, timing, and extent of wolf har-
vesting.
Acknowledgments
Field research was funded by Parks Canada. We
thank all PNP wardens and staff for field and techni-
cal support, particularly K. Wade, S. Sutton, and C.
Strong. Additionally L. Parent provided much GIS
expertise. Thanks also to J. Whittington and R. Whit-
tington for field support and pilots W. Roberts and
M. Robb for many safe hours of flying time. Thanks
to Helicopter Wildlife Management Team for skillful
capturing and collaring of animals. All animal treat-
ment procedures were approved by the Wildlife
Animal Care Committee, Ontario Ministry of Natural
Resources (Permit Numbers 1994-13, 1995-13, 1996-
13, 1997-13). We thank J. Whittington, B. Dobson,
and M. Boyce who incisively reviewed later drafts of
this manuscript. S.A. Forshner was personally support-
ed by an NSERC scholarship, the University of Alber-
ta, a University of Alberta Teaching Assistantship,
Bill Samuel, and Parks Canada.
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Received 13 March 2003
Accepted | March 2004
Estimation of Seed Bank and Seed Viability of the Gulf of Saint
Lawrence Aster, Symphyotrichum laurentianum, (Fernald) Nesom
Joni F. Kemp and CureisTIAN R. LACROIX!
Department of Biology, University of Prince Edward Island, 550 University Avenue, Charlottetown, Prince Edward Island
C1A 4P3 Canada
'Author to whom correspondence should be addressed.
Kemp, Joni F., and Christian R. Lacroix. 2004. Estimation of seed viability of the Gulf of Saint Lawrence Aster, Symphyotrichum
laurentianum (Fernald) Nesom. Canadian Field-Naturalist 118(1): 105-110.
The Gulf of St. Lawrence Aster, Symphyotrichum laurentianum, is a member of the family Asteraceae and is listed as “threatened”
by COSEWIC (Committee on the Status of Endangered Wildlife in Canada). This rare and vulnerable halophyte grows in only
a few locations in New Brunswick, Prince Edward Island, and the Magdalen Islands, Quebec. As an annual, S. laurentianum
relies exclusively on its seeds to survive to the next generation. The goal of this study was to estimate the quantity of viable
S. laurentianum seeds in the persistent and transient seed banks at selected sites in Prince Edward Island. Overall, the number
of seeds in the transient and persistent seed banks is low. The greatest concentration of seeds was found near the surface of
the soil. In addition, only a small proportion of those seeds tested positive for viability based on Tetrazolium staining. Of the
seeds in the persistent and transient seed banks combined, 53% were viable whereas only 2% of the seeds in the persistent seed
bank were viable. Population surveys were also completed at the five known sites (both extinct and extant) in Prince Edward
Island National Park. All sites showed signs of decline based on population estimates dating back to 1993. The Covehead
Pond site showed the greatest decline: from 250-300 individuals in 1993 to only 10 individuals in 2002. The population at
Dune Slack also showed a dramatic decrease from approximately 65 000 in 1999, to 2 200 individuals in 2002. Monitoring
of this plant and the development of a management plan for the species are critical to its survival.
Key Words: Symphyotrichum laurentianum, Aster laurentianus, Gulf of St. Lawrence Aster, seed viability, Tetrazolium,
transient and persistent seed banks, rare plant, COSEWIC, Prince Edward Island National Park.
The Gulf of St. Lawrence Aster, Symphyotrichum
laurentianum (Fernald) Nesom, is a member of the
family Asteraceae and is listed as “threatened” accord-
ing to COSEWIC (Committee on the Status of Endan-
gered Wildlife in Canada 2004*). It is an annual plant
that relies exclusively on its seeds to survive until the
next germination season, which makes this plant very
vulnerable. S. /aurentianum is a rare halophyte only
found in a few areas in Prince Edward Island (PEI),
New Brunswick (NB), and the Magdalen Islands in
Quebec. It grows in salt marshes that are only flooded
during spring and high tides. The St. Lawrence Aster
has smooth, hairless, and fleshy linear-lanceolate to
spatulate, generally sessile leaves (Figure 1). It can grow
up to 30 cm tall and can bear | to over 700 flower heads
(Houle and Haber 1990). Each flower head is subtended
by leafy bracts and is composed exclusively of white to
pink disk florets surrounded by a white pappus (Stewart
2000* and Figure 1). Seeds are enclosed in achene fruit
walls when they are dispersed.
In 1990 fewer than 1000 plants were known to exist
in PEI, NB and Quebec (Magdalen Islands) combined.
However, further research and surveys have produced
several new sites. While several sites in PEI and Que-
bec contain more than 1000 individuals each, the St. Law-
rence Aster is still vulnerable to extinction (Gilbert et
al. 1999*; Stewart and Lacroix 2001). Recent research
conducted by Stewart (2000*) showed that population
sizes could suddenly decline dramatically.
The extent of the persistent seed bank of a plant must
be known in order to fully understand the germina-
tion ecology of the species (Baskin and Baskin 1998).
In addition, the viability of a plant’s seeds must also
be maintained in order for the plant to be successful
(Fenner 2000). A seed bank is a reserve of viable, un-
germinated seeds in the soil. Seeds are considered vi-
able if they have the ability/potential to germinate under
favourable conditions (Baskin and Baskin 1998). There
are two categories of seed banks: transient and persis-
tent. A transient seed bank refers to a short-term storage
of seeds, that is seeds that are viable for one year or one
germination season. The seeds in the transient seed bank
therefore germinate in the first year after dispersal. Any
seeds that are dormant and survive to subsequent ger-
mination seasons are considered to be part of the per-
sistent seed bank. The persistent seed bank contains
seeds that remain viable in the soil for at least two ger-
mination seasons, making this a long-term reserve of
seeds that are at least one year (or one germination sea-
son) old. A knowledge of both the extent of the seed
banks and the germination potential of seeds of S. lau-
rentianum constitutes crucial baseline data to develop
a management plan for the species.
The specific goals of this study were: (1) to estimate
the quantity of seeds in the seed bank (both transient
and persistent) for S. lJawrentianum at each of the select-
ed sites in PEI in order to evaluate the ability of the
plant to maintain current populations, and (2) to test the
105
106
THE CANADIAN FIELD-NATURALIST
Vol. 118
FiGurE |. Representative photographs of Symphyotrichum laurentianum, pre-flowering (A) and post-flowering (B).
viability of seeds in the persistent seed bank and the
transient seed bank.
Materials and Methods
Population Surveys
Five sites within the PEI National Park (Figure 2)
. Were visited. Total population counts were made at the
Covehead Pond and East Marsh A sites because of the
small number of plants at these locations. The Western
Wetland site was also surveyed to confirm that no
asters were growing there. Population estimates were
recorded for Dune Slack and East Marsh B sites be-
cause of the large population sizes. These estimates
were accomplished by using a grid system. The gener-
al area where the plants were growing was subdivided
into 0.5 m? sections. A random number of sections was
selected and all plants within these grids were counted.
These counts along with the total area of the site were
used to extrapolate the approximate number of plants
found at each site.
Collection of Soil Samples
Soil cores were taken from five sites within PEI
National Park (Figure 2), the only location in the pro-
vince where the plant is found: Covehead Pond, Dune
Slack, East Marsh A, East Marsh B and Western Wet-
land. Three transects were run at each site except Cove-
head Pond. Twenty coring points were flagged along
three transects in Dune Slack. Due to sampling limita-
tions imposed by Parks Canada, only ten coring points
were flagged along three transects at East Marsh A and
a further ten along the three transects at East Marsh B.
Similarly, ten coring points were also flagged along the
three transects for Western Wetland. Eleven coring
points were flagged at Covehead Pond in a slightly
different manner because of the physical nature of the
site. Four transects were run from the water’s edge of
the pond to the high tide mark along the traditionally
heavily populated side of the pond. Eight coring points
were flagged evenly among these transects and the re-
maining three points were spaced evenly along the other
side of the pond where the plants were also reported
to grow.
Two sets of soil cores were taken from each site: one
during late June/early July, and another during late
August/early September. These dates were chosen to
correspond to the type of seed bank that was sampled.
The late June/early July samples were taken before the
emergence of the 2002 season plants, to ensure that the
transient as well as persistent seed banks were includ-
ed. The late August/early September samples were
taken after all the seeds that were going to germinate
that season had germinated. Consequently, only the
persistent seed bank was included in this specific sam-
ple date.
All the core samples were taken using an Oakfield
“LS” 36” soil sampler with an effective coring length
of 24 cm and an inner diameter of | inch. In order to
study the vertical distribution of seeds in the soil, each
soil core was divided equally into a top, middle, and
bottom section. Each section of the core was labelled,
placed into a separate bag, and put in a freezer set at
-4°C until processing which took place two weeks to
three months later. All seeds found in the soil samples
were tested for viability.
Viability Testing
Seeds were tested for viability using 2,3,5-triphenyl
tetrazolium chloride (TTC) (Grabe 1970). The TTC
test is based on a colour reaction: any seeds that are
2004
KEMP AND LACROIX: SEED BANK AND SEED VIABILITY 107
FIGURE 2. Map of all Prince Edward Island sites used in this study. Study sites are depicted as squares on both maps. All five sites
shown in (A) are located in the national park: 1. Covehead Pond, 2. Western Wetland, 3. Dune Slack, 4. East Marsh B,
and 5. East Marsh A. (B) Location of sites on Prince Edward Island with black square highlighting the specific area
shown in (A).
viable will stain pink/red. Complete achenes (contain-
ing seeds) were placed on a piece of filter paper in a
petrie dish, and left overnight to soak in distilled water.
The next day, when the seeds were fully imbibed with
water, they were dissected out of the achene fruit
wall and seed coat. After removal of the seed coat,
the embryos were placed in a 1% TTC solution for
two hours at 35°C, as prescribed for dicotyledonous
seeds. The embryos were then evaluated for viability
according to the scheme developed in Grabe (1970).
As a general rule, the radicle, shoot tip and cotyledons
must stain pink/red in order for the seed to be con-
sidered viable.
Statistical Analysis
The viability of seeds in the soil was compared
graphically for vertical distribution and sampling dates.
Statistical analysis was not possible on these data be-
cause there was no replication. Due to the vulnerable
status of the plant, sampling was limited by restrictions
on collecting imposed by Parks Canada. The vertical
distribution of seeds and fruit walls within the soil was
compared using Kruskal-Wallis tests (non parametric
equivalent of ANOVA). All data from the five sam-
pling sites on PEI were pooled for analysis.
108
Results
Population Sizes
Population sizes for all known PEI sites are shown
in Table 1. All populations experienced a decrease in
numbers, the most noticeable of these being the pop-
ulation at the Dune Slack site with more than 95%
decline. The smallest population at the Covehead Pond
site also experienced a decrease from 243 individuals
in 1999 to only 10 individuals in 2002.
Seed Banks
A total of 122 cores were taken from PEI sites. Of
these, 32 contained at least one seed. There were sig-
nificantly more seeds in the top portion of those cores
than in any other portion of the soil samples (Figure
3; Kruskal-Wallis test; P < 0.05, n=45 for each por-
tion). The non-random distribution of the seeds, as evi-
denced by the highly variable number of seeds found
in the core samples, is also highlighted in Figure 3.
This may be related to where the plants clustered the
year before, a factor we were not able to determine
prior to establishing coring sites.
Seed Viability
There was a noticeable decline in the percentage of
viable seeds among the top, middle, and bottom sec-
tions of the soil cores taken on PEI. We found that
28.4% of the seeds in the top section of the cores were
viable compared to 20% of the seeds in the middle sec-
tion of the cores. None of the seeds in the bottom section
of the cores were viable.
There was a marked decline in the percentage of via-
ble seeds between the late June/early July sample and
the late August/early September sample (Figure 4).
The percentage of viable seeds in the persistent seed
bank (2%) is practically non-existent when compared
to the viability of the seeds in the persistent and tran-
sient seed banks combined (53%). This means that the
majority of viable seeds germinate within one year of
being produced.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Discussion
Population Sizes
Symphyotrichum laurentianum populations on PEI
continue to show dramatic fluctuations and it can be
very difficult for an annual plant to rebound from these
declines in population size. Although the Dune Slack
site was considered one of the two largest populations
on PET]; its rate of decline, if maintained, will bring the
population down to a size comparable to the smallest
populations. A comparatively small population at
Covehead Pond has been relatively stable at 150 to
300 individuals for the past ten years but the last popu-
lation count found only ten individuals which, cou-
pled with the low viability of seeds in the seed banks,
indicates that this site is on the verge of extinction if
preventive measures are not taken.
The Island Nature Trust, a local conservation orga-
nization, conducted a survey of suitable areas on PEI
in 2002 to locate new populations of S. /aurentianum.
Several prime candidate habitats were located but un-
fortunately no asters were found at those sites (Mac-
Quarrie, personal communication).
Seed Banks
There appears to be a lack of mixing of the soil in
the salt marshes which causes a clustering of seeds in
the top sections of the soil. This trend is obvious in the
vertical distribution of seeds shown in Figure 3. Seeds
that remain trapped in the upper layer of the soil are
more likely to get exposed to the elements thereby
potentially affecting the viability of the embryo.
One of the most meaningful results from this study
is the fact that the viability of seeds in the persistent
seed bank is practically non-existent. This can be dev-
astating for an annual plant such as S. laurentianum.
Without the long-term storage of viable seeds, this plant
is vulnerable to short term changes in its habitat, both
natural and anthropogenic.
TABLE |. Comparison of population sizes for Symphyotrichum laurentianum on Prince Edward Island.
Population GPS Location
Covehead Pond 46° 25' 49.39" N
63° 09' 07.98" W
46° 24' 47.88" N
63° O1' 16.89" W
Western Wetland
Dune Slack 46° 24' 51.49" N
62° 59' 41.98" W
East Marsh A 46° 24' 55.97" N
62° 58' 43.89" W
East Marsh B 46° 24' 55.27" N
62° 59' 06.11" W
* estimate
1992 1999 2002
168 243 10
425 0 0)
15 000 — 20 000* 65 250* 2 200*
133
50 000 — 60 000* 25 000 — 60 000*
(Sites A and (Sites A and 44 100*
B combined) B combined)
|
)
2004
40 ;
2
Qa.
5
om 30
th,
o
jo
gat °
io ‘0
o
ep)
— *
2 mn
o
a
E =—
yea
Top Middle Bottom
Portion of the Core
(N= 32)
FiGuRE 3. Box plots showing median (centre line) and 25" and
75" percentile for numbers of seeds found in cores
from all Prince Edward Island soil samples that con-
tained seeds. Outliers (*) are included to show the
non-random distribution of the seeds.
During the summer of 2002, the Dune Slack site was
heavily flooded during a storm. This caused the site, and
consequently the maturing aster plants, to be smoth-
ered in eel grass. Since the Dune Slack population had
already experienced a dramatic decrease in size between
1999 and 2002, the necessary number of mature viable
seeds needed to survive this natural short-term event
may not be available.
Covehead Pond is an example of a site that is very
likely to become extinct due to anthropogenic causes.
This site is isolated from Covehead Bay by a road. The
culvert that is presently in place did not allow proper
drainage from the pond during the summer of 2002 and
caused this site to be flooded. The ten plants that were
100 a
n
xo}
o
o
no
o
a 60
&
>
es
fo}
oO
RB 40 4
=
oO
2
a)
ae 20 |
)
i) 1 2 3
Persistent and Transient Persistent
N=89 N=93
Seed Bank Type
FiGurE 4. The percentage of viable seeds in the seed banks on
Prince Edward Island. Persistent and transient seed
banks = all late June/early July samples on Prince
Edward Island. Persistent seed bank = all late August/
early September samples on Prince Edward Island.
KEMP AND LACROIX: SEED BANK AND SEED VIABILITY
109
seen at this site in 2002 were flooded by water and also
smothered by eel grass. This occurred at a crucial time
during seed maturation. Only one plant was found at
the Covehead site in 2003.
Status of the Species
In 2003, there were 441 Canadian species at risk,
and 140 of these were plants (Committee on the Status
of Endangered Wildlife in Canada 2004%*). Until
recently, there has been very little in terms of Federal
legislation in place to protect these species. The Species
at Risk Act (SARA) which came into effect in 2002 will
hopefully facilitate this process especially with regard
to developing a plan for the recovery of every extir-
pated, endangered, or threatened species.
The results of this study show a disturbing trend: the
estimated number of seeds in the seed banks is low, the
viability of the seeds in those seed banks is also low
(especially in the persistent seed bank), and the popu-
lations are declining. The Gulf of St. Lawrence Aster
is currently under review and it is important that all
available information on the biology of the species be
considered (especially information pertaining to seed
banks). The status of this plant has recently been up-
dated to “threatened” which is defined as “a species
that is likely to become endangered if nothing is done
to reverse the factors leading to its extirpation or ex-
tinction” (Committee on the Status of Endangered
Wildlife in Canada 2004*). This new designation con-
firms the urgent need to design a management plan for
S. laurentianum to ensure that it does not become ex-
tinct. Although harsh weather patterns leading to strong
winds and flooding cannot be prevented (i.e., extreme
flooding of the Dune Slack site during summer of
2002), alternate measures such as transplanting ex situ
plants into affected sites should be considered. Pre-
liminary results show that seedlings of S. laurentianum
can be grown from seed and transplanted from cul-
ture medium to soil with a relatively high success
rate (Stewart 2000*). However, a population decline
and loss of suitable habitat due to anthropogenic
activities can be prevented and further steps. such as
ensuring proper drainage at a site such as Covehead
Pond, should be taken.
Acknowledgments
This research was partially funded by an NSERC
(National Sciences and Engineering Research Council)
operating grant to C. Lacroix. We would like to thank
Parks Canada for allowing us access to the sites to
collect samples. Thank you to Kate MacQuarrie for
her comments on this manuscript.
Documents Cited (marked * in text)
Committee on the Status of Endangered Wildlife in Can-
ada. 2004. COSEWIC assessment and update status report
on the Gulf of St. Lawrence Aster, Symphyotrichum lauren-
tianus in Canada. Ottawa. 39 pages. Retrieved May 2004,
froma http://www.cosewic.gc.ca
110
Gilbert, H., J. Labrecque, and J. Gagnon. 1999. La situa-
tion de l’aster du Saint-Laurent (Aster laurentianus, syn. :
Symphyotrichum laurentianum) au Canada. Ministére de
l'Environnement Direction de la conservation et du patri-
moine écologique, Québec.
Stewart, S. E. 2000. Micropropagation of Aster lauren-
tianus. Unpublished honours thesis, University of Prince
Edward Island, Charlottetown, Canada.
Literature Cited
Baskin, C. C., and J. M. Baskin. 1998. Seeds: Ecology, bio-
geography, and evolution of dormancy and germination.
Academic Press, San Diego.
Fenner, M. 2000. Seeds: The ecology of regeneration in
plant communities. CABI Publishing, New York.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Grabe, D. E., Editor. 1970. Tetrazolium testing handbook for
agricultural seeds: contribution Number 29 to the hand-
book on seed testing. Tetrazolium Testing Committee of
the Association of Official Seed Analysts.
Houle, F., and E. Haber. 1990. Status of the Gulf of St. Law-
rence Aster, Aster laurentianus (Asteraceae), in Canada.
Canadian Field-Naturalist 104: 455-459.
Stewart, S. E., and C. R. Lacroix. 2001. Germination poten-
tial, updated population surveys and floral, seed and seed-
ling morphology of Symphyotrichum laurentianum, the
Gulf of St. Lawrence Aster, in the Prince Edward Island
National Park. Canadian Field-Naturalist 115: 287-295.
Received 2 June 2003
Accepted 3 June 2004
Consumption of Shrews, Sorex spp., by Arctic Grayling,
Thymallus arcticus
JONATHAN W. Moore! and G. J. KENAGY?
' Department of Biology, University of Washington, Box 351800, Seattle, Washington 98195 USA;
e-mail: jwmoore @u. washington.edu
* Burke Museum and Department of Biology, University of Washington, Box 353010, Seattle, Washington 98195 USA
e-mail: kenagy @u.washington.edu
Moore, Jonathan W., and G. J. Kenagy. 2004. Consumption of shrews, Sorex spp., by Arctic Grayling, Thymallus arcticus.
Canadian Field-Naturalist 118(1): 111-114.
In an investigation of the dietary habits of Arctic Grayling (Thymallus arcticus) we found that two individuals out of 93 sampled
in southwestern Alaska (approximately 59°N, 159°W) contained a total of five shrews (Sorex spp.). These shrews contained
enriched levels of nitrogen stable isotopes, suggesting utilization of nutrients derived from salmon. We hypothesize that
normally terrestrial shrews accidentally enter streams while foraging along the productive riparian zones of creeks with high
densities of salmon. Shrews are apparently susceptible to opportunistic predation by resident stream fishes, including Arctic
Grayling, when they enter the streams.
Key Words: Arctic Grayling, Thymallus arcticus, diet, salmon-derived nutrients, shrews, Sorex spp., stable isotopes.
The Arctic Grayling (Thymallus arcticus) is a com-
mon nearctic freshwater fish in lakes and streams at
high latitudes (Nelson 1994). Grayling typically feed
on a variety of aquatic and terrestrial invertebrates in
the water column or air-water interface (Armstrong
1986). In addition, Arctic Grayling occasionally supple-
ment their diets with salmon eggs and small fish
(Armstrong 1986). Despite existing knowledge of Arctic
Grayling biology and its regional importance, the ecol-
ogy and behavior of this species remain not well un-
derstood, including the extent to which Arctic Grayling
exploit terrestrial sources of prey (Armstrong 1986).
As part of an extensive study of the aquatic and asso-
ciated terrestrial ecosystem and its relationship to sal-
mon in southwestern Alaska (Schindler et al. 2003),
we had the opportunity to investigate dietary habits of
Arctic Grayling. We discovered evidence of apparently
rare consumption by Arctic Grayling of small terres-
trial mammals of the Order Insectivora, shrews of the
genus Sorex.
During summer 2001 we sampled resident fishes in
five streams that flow into Lake Nerka in the Wood
_ River-Tichick State Park, Dillingham County, south-
western Alaska (approximately 59°36’N, 159°05’W),
by conventional and fly angling. The study streams sup-
| port large runs of Sockeye Salmon (Oncorhynchus
_ nerka). Captured fish were anesthetized, marked with
subcutaneous tags, weighed, measured, and released.
_ We obtained diet samples by back-flushing the stomach
with a gastric lavage. Diet samples were preserved in
| ethanol and transported back to the University of
Washington for analysis.
_ We sampled the stomach contents of 93 Arctic Gray-
| ling from five tributaries of Lake Nerka. Two of the
93 Arctic 2001 Grayling contained visible evidence of
the body parts of shrews (Figure 1, Table 1). One Arctic
Grayling (length 394 mm, mass 591 g), captured on
13 August in the Little Togiak River contained the
remains of three shrews. A second Arctic Grayling
(length 391 mm, mass 522 g), captured on 25 August
in Elva Creek contained the remains of two shrews.
Nothing else about the two observed Arctic Grayling
was unusual other than their stomach contents. Although
the fish were relatively large, they were not extreme,
being longer than about 70% of the other Arctic Gray-
ling. In addition to the shrews, the diets of these two
fish contained aquatic and terrestrial insects typical of
the diets of the other Arctic Grayling sampled at this
same time and location.
The five alcohol-preserved shrews (Sorex spp.) from
the diet samples of two Arctic Grayling were deposit-
ed in the Burke Museum mammal collection. Three
shrews (UWBM 74151, 74152, 74154) were sufficient-
ly intact that we could examine individual teeth in the
skull, which is critical for species identification. We
used the keys of Nagorsen (1996), based on body and
skull measurements and dental characteristics, particu-
larly the relative length of the third unicuspid. In two
cases, digestion had progressed too far to allow species
determination by these characters. We subsequently
referred tissue samples of all five specimens to Eric
Waltari, Idaho State University, for molecular (cyto-
chrome-b) identification, according to protocols used
in his systematic investigation of Sorex, as developed
by Demboski and Cook (2001). Molecular identification
confirmed the three initial morphological identifica-
tions and provided definitive identification for the two
previously unidentifiable individuals (UWBM 74153,
74155)
The two shrews from Elva Creek were identified as
Sorex monticolus and Sorex cinereus (Figure 1, upper).
The S. cinereus specimen had a wet weight of 3.3 g
IU
112
and was fairly intact except for digestion of the fur
away from the skin. Due to more extensive digestion,
the S. monticolus specimen could not be measured and
weighed accurately, but its intact skull and dentition
allowed a positive identification (Table 1).
The three shrews from the Little Togiak River (Fig-
ure 1, lower) included a highly intact S. cinereus with
considerable fur still attached to its skin (Figure 1,
lower, center). The other two shrews were extensively
digested and could only be identified by molecular
analysis, as S. cinereus (left) and S. monticolus (right).
In summary, the two Arctic Graylings from two dif-
ferent streams both had fed on shrews of two species
(Table 1).
The presence of the shrews Sorex monticolus and
Sorex cinereus in this region of southwest Alaska ly-
ing to the north of Bristol Bay and east of the Kilbuck
Mountains is consistent with the known geographic
ranges of shrews (Hall 1981) and a more recent dis-
tributional analysis (S. O. MacDonald and J. A. Cook,
personal communication). Shrew abundance and diver-
sity are high in this area, and three other species are
also present: S. hoyi, S. tundrensis, and S. yukonicus.
Although some species of the genus Sorex live and
feed primarily in water (Beneski and Stinson 1987),
none of the five Sorex species in the study area is pri-
marily aquatic. However, all five occur to some extent
in riparian habitat, where their success is enhanced by
the aquatic component of the food chain. As a result
of this habitat association, the shrews are potentially
accessible to predatory fishes in these waters. The ten-
dency for shrews of the genus Sorex to enter water,
whether for foraging or dispersal, has been reviewed
by Hanski (1986). In addition to intentional entry into
the water, it is also possible that these shrews occa-
sionally enter the water accidentally, resulting from
their normal activities near the water’s edge.
Shrews may be attracted to the riparian zones of
these creeks because of the potential foraging oppor-
tunities offered by abundant salmon carcasses. Ceder-
holm et al. (1999) list shrews, including Sorex cinereus,
as known scavengers of salmon carcasses. Evidence
from stable isotopes ('°N) from our study (Table 1)
and Ben-David et al. (1998) show that shrews (Sorex
spp.) living near streams containing anadromous sal-
THE CANADIAN FIELD-NATURALIST
Vol. 118
mon runs bear the enriched isotopic signature of feed-
ing directly or indirectly on salmon, for example, on
insects that feed on salmon carcasses. We analyzed
the stable isotope signature of muscle tissue from each
shrew. Because anadromous salmon have a relatively
high isotopic signature (6 °N = 11-13) compared to
most other potential food sources, isotopes have been
used to trace salmon nutrients through both aquatic
and terrestrial food webs (Kline et al. 1990; Ben-
David et al. 1998). The abundance of '°N in shrew
muscle tissue was measured by combusting several
mg of ground muscle tissue from each shrew in a mass
spectrometer by the Stable Isotope Lab at the Univer-
sity of California, Davis. Stable isotopes were expressed
as a delta (6) value—the deviation from an isotope
standard (atmospheric nitrogen). In other words,
SION) = (GSNae Nie ee) ON reenact) XoLOOO!
We used a two-sample t-test to compare 6°N of
shrews in diets of Arctic Grayling to published values
of isotopes from six shrews that were collected more
than 500 m from streams with salmon in southeast-
ern Alaska by Ben-David et al. (1998). The five
shrews we collected from Arctic Grayling diets were
relatively enriched, averaging 5.88 + 0.47 6 PN
(mean + standard error; Table 1), higher than shrews
collected from sites over 500 m from Alaskan
salmon-bearing streams, that averaged 4.5 + 0.3 6
!SN (ty9 = 2.24, P < 0.10) (Ben-David et al. 1998).
This relative enrichment suggests that the shrews we
found in the Arctic Grayling diets may have been
feeding directly on salmon carcasses or indirectly,
for example, by feeding on insects that had been
feeding on salmon carcasses. The high productivity
of these riparian zones, especially along streams with
high densities of salmon, probably contributes posi-
tively to the success and survival of shrews, the tiniest
of mammals, in this extreme northern environment.
The skewed distribution of the number of shrews
contained per Arctic Grayling is evidence that con-
sumption of shrews is not a random event. We assessed
whether Arctic Grayling consumption of shrews was
random by comparing the observed frequency distri-
bution of the number of shrews in Arctic Grayling
stomachs to the expected distribution, assuming pre-
dation to be random. We calculated expected frequen-
sample
TABLE |. Characteristics of shrews removed from the stomachs of two Arctic Grayling.
Sorex spp 6 ©N! Location
S. cinereus? 4.73 Elva Creek
S. monticolus* SP) Elva Creek
S. monticolus* 6.33 Little Togiak River
S. cinereus® 7.42 Little Togiak River
S. cinereus* 5.70 Little Togiak River
Body dimensions? Specimen number
96-38-11 mm UWBM 74151
indeterminable UWBM 74152
indeterminable UWBM 74153
88-38-12 mm UWBM 74154
indeterminable UWBM 74155
' 8I5N is the stable isotope of nitrogen and can be used to trace salmon-derived nutrients.
? Dimensions are total length, tail length, and hind foot length, in mm.
> Identified both by dentition and cytochrome-b analyses.
“Identified by only cytochrome-b analysis because of missing/digested dentition.
2004
MoOoRE AND KENAGY: CONSUMPTION OF SHREWS BY GRAYLING
FiGurRE 1. Shrews removed from the stomachs of two Arctic Grayling, in various stages of digestion. Upper: Shrews from a
522 g Arctic Grayling sampled at Elva Creek (59°34’N, 159°05’W) — Sorex monticolus (UWBM 74152) left and
Sorex cinereus (UWBM 74151) right. Lower: Shrews from a 591 g Arctic Grayling at Little Togiak River (59°36’N,
159°04’W) — Sorex cinereus (UWBM 74155) left, S. cinereus (UWBM 74154) center, and Sorex monticolus
(UWBM 74153) right.
cy distributions using the Poisson function in Matlab
5.313, assuming an average number of shrews per
Arctic Grayling of 0.054 (5 shrews in 93 Arctic Gray-
ling). We encountered fish with either two or three
shrews in their stomachs, but no fish with only one
shrew. Based on a random expectation for Arctic Gray-
ling consumption, there was a 0.12 probability of sam-
pling an Arctic Grayling with two shrews and only a
0.003 probability for three shrews. Thus we conclude
that Arctic Grayling consumption is not random, and
we speculate that this is due to individual differences
in either the effectiveness or motivation of individual
Arctic Grayling as shrew predators or scavengers. It
may also be due to differences in the probability of
shrews entering the feeding sites of specific Arctic
Grayling.
Although Arctic Grayling are typically considered
to be specialists on aquatic and terrestrial insects (Arm-
strong 1986), our observation indicates that some
Arctic Grayling are opportunistic feeders, capable of
consuming small mammals. Shrews, typically 4-8 g
(Nagorsen 1996), represent a meal for Arctic Graylings
that provides a large amount of energy compared to
that of typical individual invertebrate food items. Con-
sumption by Arctic Grayling of small mammals, in-
cluding shrews, has been reported by several previous
authors. Alt (1978*) reported an unspecified small
number of shrews in diets of Arctic Grayling in the
Fox River of western Alaska. De Bruyn and McCart
(1974*) found that seven out of 136 Arctic Grayling
contained a single shrew in the Firth River, Yukon,
Canada. A European study of the grayling Thymallus
thymallus indicated a 10% incidence of small mam-
mals in the diet, particularly the shrew Sorex araneus,
and the capture of these fish at night by bait angling
suggested their ability as nocturnal hunters of semi-
aquatic prey such as shrews (Teplov 1943). Miller
(1946) reported that one out of 102 Arctic Grayling
at Great Bear Lake, Canada, contained juvenile lem-
mings (rodent) of an unspecified species in the diet.
Reed (1964*) also found juvenile lemmings in two
Arctic Grayling out of 1300 individuals sampled in
the Tanana River drainage, Alaska.
Terrestrial food sources often subsidize the diets of
freshwater fish, and these food sources can include
small mammals (for example, Brown Trout [Salmo
trutta], Cochran and Cochran 1999; and Largemouth
Bass [Micropterus salmoides|, Hodgson and Kinsella
1995). Although Arctic Grayling are traditionally con-
sidered insectivores, our report demonstrates that they
also opportunistically consume shrews that venture
into freshwaters.
Acknowledgments
We thank the Alaska Salmon Project of University
of Washington for logistic support and the National
Science Foundation and ARCS foundation for finan-
cial support. D. E. Schindler and M. D. Scheuerell
provided insightful discussions and helped collect
fish diets. M. D. Scheuerell and J. I. Jones prepared
the shrew muscle samples fer isotopic analysis, which
were run by D. Harris. We thank E. Waltari for molec-
ular identification of the shrews and R. Rausch for
advice on the observation and literature.
114
Documents Cited (marked * in text)
Alt, K. T. 1978. Inventory and cataloging of sport fish and
sport fish waters of western Alaska. Alaska Department
of Fish and Game. Federal Aid in Fish Restoration, Annual
Performance Report, 1977-1978. Project F-9-10, 19 (G-I-
P): 36-60.
de Bruyn, M., and P. J. McCart. 1974. Life history of the
grayling (Thymallus arcticus) in Beaufort Sea Drainages
in the Yukon Territory. /n Fisheries research associated
with proposed gas pipeline routes in Alaska, Yukon and
Northwest Territories. Edited by P. J. McCart. Canadian
Arctic Study, Ltd., Calgary, Biological Report Series 15.
39 pages.
Reed, R. J. 1964. Life history and migration patterns of Arc-
tic grayling, Thymallus arcticus (Pallus), in the Tanana
River drainage of Alaska. Alaska Department of Fish and
Game Research Report Number 2: 8-30.
Literature Cited
Armstrong, R. H. 1986. A review of Arctic grayling studies
in Alaska, 1952-1982. Biological Papers of the Univer-
sity of Alaska, Number 23: 1-110.
Ben-David, M., T. A. Hanley, and D. M. Schell. 1998.
Fertilization of terrestrial vegetation by spawning Pacific
salmon: the role of flooding and predator activity. Oikos
83: 47-55.
Beneski, J. T., and D. W. Stinson. 1987. Sorex palustris.
Mammalian Species 296: 1-6.
Cederholm, C. J., M. D. Kunze, T. Murota, and A. Sibatani.
1999. Pacific salmon carcasses: essential contributions of
nutrients and energy for aquatic and terrestrial ecosystems.
Fisheries 24: 6-15.
Cochran, P. A., and J. A. Cochran. 1999. Predation on a
meadow jumping mouse, Zapus hudsonius, and a house
mouse, Mus musculus, by brown trout, Salmo trutta.
Canadian Field-Naturalist 113: 684-685.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Demboski, J. R., and J. A. Cook. 2001. Phylogeography of
the dusky shrew, Sorex monticolus (Insectivora, Soricidae):
insight into deep and shallow history in northwestern
North America. Molecular Ecology 10: 1227-1240.
Hall, E. R. 1981. The mammals of North America. John
Wiley, New York. 1175 pages.
Hanski, I. 1986. Population dynamics of shrews on small
islands accord with the equilibrium model. Biological
Journal of the Linnean Society 28: 23-36.
Hodgson, J. R., and M. J. Kinsella. 1995. Small mammals
in the diet of largemouth bass, revisted. Journal of Fresh-
water Ecology 10: 433-435.
Kline, T. C., Jr., J. J. Goering, O. A. Mathisen, P. H. Poe,
and P. L. Parker. 1990. Recycling of Elements Trans-
ported Upstream by Runs of Pacific Salmon: I. 6 '°N and
6 C Evidence in Sashin Creek, Southeastern Alaska.
Canadian Journal of Fisheries and Aquatic Sciences 47:
136-144.
Miller, R. B. 1946. Notes on the Arctic grayling, Thymallus
signifier Richardson, from Great Bear Lake. Copeia 1946:
227-236.
Nagorsen, D. W. 1996. Opossums, shrews, and moles of
British Columbia. University of British Columbia Press,
Vancouver. 169 pages.
Nelson, J. S. 1994. Fishes of the World. Third edition. John
Wiley and Sons, New York. 600 pages.
Schindler, D. E., M. D. Scheuerell, J. W. Moore, S. M.
Gende, T. B. Francis, and W. J. Palen. 2003. Pacific
salmon and the ecology of coastal ecosystems. Frontiers
in Ecology and the Environment |: 31-37.
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Received 9 June 2003
Accepted | June 2004
Unusual Behavior by Bison, Bison bison, Toward Elk, Cervus elaphus,
and Wolves, Canis lupus
L. Davip Mecu!, Rick T. McINTYRE2? and DouGLAS W. SMITH?
'U.S. Geological Survey, Northern Prairie Wildlife Research Center, 8711 - 37" Street, SE, Jamestown, North Dakota 58401 -
7317 USA; Mailing address: The Raptor Center, 1920 Fitch Avenue, University of Minnesota, St. Paul, Minnesota
55108 USA
* National Park Service, Yellowstone Center for Resources, P. O. Box 168, Yellowstone National Park, Wyoming 82190 USA
3 Mailing address: General Delivery, Silver Gate, Montana 59081 USA
Mech, L. David, Rick T. McIntyre, and Douglas W. Smith. 2004. Unusual behavior by Bison, Bison bison, toward Elk, Cervus
elaphus, and Wolves, Canis lupus. Canadian Field-Naturalist 118(1): 115-118.
Incidents are described of Bison (Bison bison) in Yellowstone National Park mauling and possibly killing a young Elk (Cervus
elaphus) calf, chasing wolves (Canis lupus) off Elk they had just killed or were killing, and keeping the wolves away for
extended periods. During one of the latter cases, the Bison knocked a wolf-wounded Elk down. Bison were also seen approach-
ing wolves that were resting and sleeping, rousting them, following them to new resting places and repeating this behavior.
These behaviors might represent some type of generalized hyper-defensiveness that functions as an anti-predator strategy.
Key Words: Bison, Bison bison, Wolt, Canis lupus, Elk, Cervus elaphus, Yellowstone National Park.
Bison (Bison bison) are known to be aggressive to directed the capturing and radio-tagging of the Wolves,
other ungulates including Elk and even to kill Elk allowing them to be located and observed.
(Cervus elaphus) calves (Chapman 1937: 148; Rush
1942: 225; McHugh 1958: 143; Mahan 1977). Little Observations
is known about the causes and circumstances of this 1. 30 May 1995 — Bison Attack Elk Calf
aggressiveness except for the scattered reports docu- A recently born Elk calf that separated from its
menting it. Bison also defend themselves aggressively mother became mixed up in the middle of a Bison herd
when attacked by Wolves (Canis lupus) (Carbyn and southwest of the Lamar Picnic Area. During the early
Trottier 1988; Carbyn et al. 1993; MacNulty 2002), stages of this observation, filmmaker Ray Paunovich
although Bison have been reported to be indifferent to saw a Bison knock the calf down and then repeatedly
close, but non-attacking, Wolves (Catlin 1876-1: 254 butt it to the ground.
cited by McHugh 1938; Goodwin 1939: 369 cited by RM watched a group of Bison encircle the calf, then
McHugh 1938; and Soper 1941: 403; Carbyn et al. lick and sniff it. The calf got up and tried to walk off,
1993). but several Bison chased it. One Bison butted the calf in
We also have observed the same types of behavior of _ the side and knocked it down. Twelve additional Bison
Bison toward wolves both when being attacked and came over to sniff it. The calf got up and ran off, but
not being attacked in Yellowstone National Park. How- was chased and knocked down again by the Bison.
ever, we have observed other types of Bison aggres- As long as the calf remained down or stood still, the
_ siveness toward Elk and toward Wolves that has not — Bison just sniffed and licked it, but whenever it ran off,
_ been reported, and we have seen another possible case they chased it and knocked it down. This sequence
_ of Bison killing an Elk calf. Because our observations __ took place at least four times. A cow Bison later butted
| considerably extend what is known about Bison aggres- _ the Elk calf several times as it lay on the ground. Then
siveness and because observation of any ungulates chas- _ the herd walked away. The calf was motionless as the
| ing predators are rare (Berger 1979), we report them Bison moved off and was possibly dead from all the
below and propose an explanation for the possible adap- _ butting. RM then left, but Paunovich thought he saw
tiveness of the aggressiveness. some movement from the calf after RM left. Whether
__ Both Elk and Bison have inhabited the park for many the calf survived is unknown.
_ decades, but Wolves were reintroduced to the ecosys- 2. 6 June 2001 — Bison Displace Wolves from Kill
Bea an P73) and 1996 (Bangs et al. 1998). Wolves in "at 0529 hrs, RM spotted a fresh adult Elk kill with
| Yellowstone prey primarily oo Elk (Mech et al. 2001) four yearling Druid Peak pack Wolves next to it south-
_ but do kill Bison as well (Smith et al. 2000). RM made east of the Lamar Valley Picnic Area. The carcass was
{ a peo auons in ns northeastem En of Yellowstone intact and the Wolves must have just killed it. Three
ational Park through binoculars and spotting scopes Wolves were about to start feeding.
_ with 60x power and recorded them by tape recorder: A Bison bull walked up to the carcass and sniffed its
_ LDM independently observed and recorded with pad head. The Wolves went to the rear of the carcass and
and pencil the observation on 20 March 2002. DWS
HS
116
started tugging on that section as the bull continued to
sniff the head area. This seemed to be the Wolves’ first
feeding on the kill. Three more Bison bulls approached
the carcass. One Wolf at the carcass walked off a few
steps with a tucked tail, then came right back and
snarled at the nearest bull. The bulls walked toward
the three Wolves, and the Wolves backed off. Two of
the bulls sniffed the Elk’s head. A Wolf sneaked back
in and fed on the rear end.
Soon six bulls were at the site. They had a stand-off
with the three Wolves at 0537 hrs. When one Wolf
tried to approach the carcass, a bull ran at it, and the
Wolf backed off. The other bulls walked toward the rest
of the Wolves, and they scattered. The six bulls kept the
three Wolves away from the carcass through 0554 hrs.
At that time, the bulls left the site, and the Wolves
moved to the carcass and fed. The three Wolves were
still feeding on the kill when RM left at 0615 hrs.
In Wood Buffalo National Park, Alberta, mixed
herds of Bison were observed forcing wolves away from
wolf-killed Bison calves about 1 and about 4 months
old (L. N. Carbyn, personal communication).
3. 3 March 2002 — Bison Attack Wounded Elk Calf
This incident was observed and video-taped by cine-
matographer Shane Moore in the Blacktail area of
Yellowstone National Park. The tape was viewed by
RM who transcribed the details summarized below.
The incident began when a herd of Bison ran
0.15 km downhill to a 9-month-old Elk calf with blood
on its neck. Several Coyotes (Canis latrans) were near-
by. The Bison herd gathered near the Elk, and over a
4-hr period, the Bison sniffed, licked, chased, and but-
ted the Elk as the animal tried to seek refuge from the
Coyotes by running into the Bison herd. The Bison but-
ted the calf throughout the episode on 21 occasions
during 40 minutes of videotaping, usually in the rear
or side, and once knocked it into the air. At times the
Elk was bedded or lying on its side when the Bison
butted it.
Partway through the video, it was apparent that the
Elk’s abdomen was wounded, and an organ was hang-
ing out. Moore believed that wound resulted from when
he saw a Bison charge the Elk at full speed and hit it
very hard in the side. Although the rest of the Bison
herd then blocked the view, the calf stayed down for
20 minutes and when it arose, its abdomen had been
ripped open.
Toward the end of the four-hour observation, the
Bison drifted away from the wounded and bedded calf.
As the calf continued to weaken, two Coyotes attacked
it. Three additional Coyotes joined the attack, and the
five Coyotes soon killed the calf.
4. 20 March 2002 — Bison Displace Wolves from Kill
Eleven members of the Druid Peak pack (1 1-months
old and 23-months old; no adults) had been chasing
Elk in the Hellroaring Creek area of Yellowknife Na-
tional Park. At about 0931 hrs, the Wolves targeted a
single cow Elk and pulled her down. A herd of about
THE CANADIAN FIELD-NATURALIST
Vol. 118
39 Bison rushed to the downed Elk, chased the Wolves
off, and surrounded the Elk tightly (0933 hrs). Sud-
denly the Elk leaped up. Two Wolves approached the
Elk and nipped at it. The Elk ran through the Bison
herd, and the two Wolves pursued it. After about 30 m
the Elk fell. The Wolves were on it again for about 30 sec
when the Bison chased them off again (0936 hrs). Later
the Elk arose and almost immediately collapsed. The
Elk arose a third time, ran a short distance and col-
lapsed. She later tried to stand again but could only
get up on her hind legs. A Bison butted the Elk’s rear
end and knocked her down, and the Bison herd
surrounded the Elk again and kept the Wolves away.
Each time a Wolf approached, a Bison would chase it
15-30 m. After a few minutes, the Wolves headed
away up a hill and bedded (0946 hrs).
The Elk, while surrounded by Bison, kept raising her
head and trying to get up. Usually the Bison stood
closely around her but sometimes jumped back a few
meters. The Bison remained tightly around the Elk
from about 0939 hrs on. By about 1135 hrs, the Elk’s
head was no longer up and her body lay flat; she seemed
dead. Ravens landed on or next to her, although the
Bison still surrounded her closely. Bison licked or
sniffed (we could not determine which) the carcass
intermittently for several minutes.
The Wolves had returned at 0955 hrs and hung
around 15-60 m from the Bison herd, and at various
times some tried to reach the downed Elk. Each time,
one or more Bison would skirmish with them and try
to drive them off.
About 1253 hrs, the Bison started moving away from
the Elk, and by 1305 hrs Wolves moved in. However,
the Bison quickly returned and ran the Wolves off. This
happened several times when Bison were both east
and west of the Elk. Eventually, however, the Bison all
grouped east of the Elk, and the 11 Wolves began to
feed. The Bison then charged the Wolves and ran them
off. Then the Wolves returned and chased the Bison
away. In the next few minutes there were two addition-
al standoffs at the carcass, and both times the Bison
chased away the Wolves.
Such skirmishes continued as Wolves and Bison
surged toward the Elk and each other, but gradually
the Bison began to head a few meters farther east, and
the Wolves became bolder. By 1313 hrs, the Wolves
controlled the carcass and remained there and fed, while
the Bison drifted off eastward. By 1350 hrs most of
Wolves were done feeding and slept on a hill above the
carcass, although individual Wolves fed later as well.
5. 22 March 2002 — Bison Roust Sleeping Wolves
In the same general area as observation 4 was made,
eight of the 11 Druid Peak Pack Wolves seen on 20
March were sleeping at 0909 hrs when six Bison lead-
ing a larger herd (probably the same 39 seen there two
days earlier) approached them. The Wolves arose,
moved 100 m, and lay down again. Two minutes later,
the Bison approached them to within 3 m, and the
2004
Wolves again moved off 100 m and lay down. At
0918 hrs, a Bison approached one of the Wolves,
which then confronted it; the other Wolves joined in
harassing the Bison for 30 seconds.
The Wolves then left at 0920 hrs and moved 90° and
a few hundred meters and lay down on a rocky ridge.
Eventually the Bison followed and rousted the Wolves
from there. Several more times the Bison followed
the Wolves and rousted them out of their beds.
6. 16 April 2002 — Bison Bulls Displace Wolves from
Kall
At 0826 hrs, RM saw 11 Druid pack Wolves (the
breeding male, two yearlings, and eight 1 1-month-old
pups) chase Elk about 1.6 km west of the Lamar Ran-
ger Station. They pulled down a cow Elk at 0858 hrs.
A few Bison bulls started moving toward them from
the north. Two Bison ran into the site and chased the
Wolves off. A yearling and two pups came right back
to the carcass. One of the bulls returned to the site and
chased off one of the Wolves.
At 0900 hrs several Wolves were feeding as four
Bison bulls stood near the carcass. Two bulls charged
the Wolves and drove them off, then stood close to
the carcass.
At that point, five Wolves watched the carcass from
35 m away. The two bulls charged the breeding male
and another Wolf, which fled eastward. The other
Wolves ran to the kill and fed. The breeding male cir-
cled around and joined them.
A bull then walked to the carcass, and the feeding
Wolves backed off a meter or so. The other nearby
Bison approached the site. That bull charged the
Wolves, and they ran off but came right back.
Both bulls then stood next to the Elk carcass and
sniffed it. The bigger bull charged the Wolves, but as
before the Wolves soon stopped, and the breeding male
and three others returned to the site.
The two additional Bison bulls came toward the car-
cass from the west. One of the bulls shook his head,
and some Wolves backed off a step or two. Other
Wolves stood their ground and faced the bull which
was about 6 m away. The bull shook his head again,
but the Wolves continued to feed and ignored him.
The breeding male Wolf stepped away and ate some
snow. When he returned to the carcass, a bull chased
him off. The Wolf came right back. The same bull,
which was the largest and most aggressive of the four
bulls there, then drove all the Wolves off. The breed-
ing male Wolf returned, and the big bull charged him.
A second bull was standing a meter or so from the
carcass. The big bull chased the breeding male Wolf
southward, then returned to the site. The two bulls
kept the Wolves from the kill until the bulls walked a
short distance away at 09:12; the Wolves immedi-
ately ran in. All 11 fed or were near the site. As the two
bulls walked off to the north a pup followed them.
Around 0920 hrs, three bulls approached the car-
cass from the northeast as the Wolves continued to
MEcH, MCINTYRE, AND SMITH: UNUSUAL BEHAVIOR BY BISON
Ki,
feed. One pup headed westward, but the others stood
their ground. The bulls turned back before they reached
the site. A fourth bull chased a Wolf to the north of the
carcass. One bull then ran in toward the carcass, but the
Wolves countercharged, drove him away, and resumed
feeding. A fifth bull was north of the carcass but did
not yet approach it.
A sixth bull approached the kill, and a pup circled
around to his rear and followed him. Another pup joined
the first pup behind the bull. Two more of the original
bulls approached the carcass from the north. The lead
bull walked by the north side of the carcass with a
raised tail. As another bull approached the site, the
seven feeding Wolves backed off. At 0927 hrs three
bulls remained at the carcass keeping the Wolves away.
The breeding male Wolf stood nearby. He and a pup
left, and the breeding male bedded north of the site at
0929 hrs. Eight other Wolves stood near the carcass.
At 0930 hrs two bulls started sparring with each
other and began to drift away from the carcass. The
breeding male Wolf and a yearling walked to the kill
and fed. In the next minute other Wolves joined them.
All six bulls remained away from the site, and the
Wolves fed unmolested.
Discussion
The aggressiveness shown by Bison toward Elk and
toward non-attacking Wolves is puzzling but might be
some kind of hyperdefensive or hyperaggressive behav-
ior. Predator harassment by several species of ungu-
lates has been documented, and various explanations
have been offered (summarized by Berger 1979), each
involving ultimate reduction of predation risk. These
explanations do not account for Bison attacking Elk,
however. The most common element in our observa-
tions and those reported earlier of Bison attacking Elk
was the presence of a weak or downed Elk and the
butting, sniffing, and mobbing of it. In the Elk inci-
dents involving Wolves, perhaps the presence of the
predators was only incidental and made the Bisons’
aggressiveness appear directed at keeping Wolves away
from the carcasses or injured animals.
In other words, our observations might involve two
phases of hyperaggressive behavior: (1) a general
aggressiveness toward various intruders, perhaps as
generalized anti-predator behavior that causes the Bison
to approach intruders, and (2) continued aggressive-
ness toward intruders that do not flee, e.g., wounded
animals or animals seeking refuge in the Bisons’ herd
because these animals persist in remaining nearby. This
would also include Wolves that are trying to feed on
carcasses near the Bison herd. Bison are so large and
powerful that when a herd acts aggressively, it can
charge and attack any animal with impunity, includ-
ing Wolves and Grizzly Bears (Ursus arctos). Thus it
may be generally advantageous for them to advertise
this ability by harassing intruders persistently without
making fine distinctions as to type.
118
Acknowledgments
This study was supported by the Biological Res-
ources Division, U.S. Geological Survey, and the
Yellowstone Center for Resources.
Literature Cited
Bangs, E. E., S. H. Fritts, J. A. Fontaine, D. W. Smith, K.
M. Murphy, C. M. Mack, and C. C. Niemeyer. 1998.
Status of gray wolf restoration in Montana, Idaho, and
Wyoming. Wildlife Society Bulletin 26: 785-798.
Berger, J. 1979. “Predator harassment” as a defensive strat-
egy in ungulates. American Midland Naturalist 102: 197-
199.
Carbyn, L. N., and T. Trottier. 1988. Descriptions of wolf
attacks on bison calves in Wood Buffalo National Park.
Arctic 41: 297-302.
Carbyn, L. N., S. M. Oosenbrug, and D. W. Anions. 1993.
Wolves, bison and the dynamics related to the Peace-Atha-
basca Delta in Canada’s Wood Buffalo National Park.
Circumpolar Research Series (4). Canadian Circumpolar
Institute, University of Alberta.
Catlin, G. 1876. Illustrations of the manners, customs, and
condition of the North American Indians. Two volumes.
Chatto & Windus, London, U.K. 530 pages.
Chapman, W., and L. Chapman. 1937. Wilderness wan-
derers. Charles Scribner’s Sons, New York. 318 pages.
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Goodwin, G. C. 1939. The bison. Chapter XX in North
American Big Game. Edited by Alfred Ely, H. E. Anthony,
and R. R. M. Carpenter. Charles Scribner’s Sons, New
York. 533 pages.
MacNulty, D. R. 2002. The predatory sequence and the influ-
ence of injury risk on hunting behavior in the wolf. Master’s
thesis, University of Minnesota, St. Paul, Minnesota.
Mahan, B. R. 1977. Harassment of an elk calf by bison.
Canadian Field-Naturalist 91: 418-419.
McHugh, T. 1958. Social behavior of the American buffalo
(Bison bison bison). Zoologica 43: 1-41.
Mech, L. D., D. W. Smith, K. M. Murphy, and D. R.
MacNulty. 2001. Winter severity and wolf predation on a
formerly wolf-free elk herd. Journal of Wildlife Manage-
ment 65: 998-1003.
Rush, W. M. 1942. Wild animals of the Rockies. Harper and
Brothers, New York. 296 pages.
Smith, D. W., L. D. Mech, M. Meagher, W. E. Clark, R.
Jaffe, M. K. Phillips, and J. A. Mack. 2000. Wolf-bison
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Received 11 August 2003
Accepted 4 June 2004
Notes
Morphology of Female Woodland Caribou, Rangifer tarandus caribou,
in Saskatchewan
W. JAMES RETTIE
Department of Biology, University of Saskatchewan, 112 Science Place, Saskatoon, Saskatchewan S7N 5E2 Canada
Present address: Northeast Science & Information Section, Ontario Ministry of Natural Resources, Ontario Government Complex,
Highway 101 East, P.O. Bag 3020, South Porcupine, Ontario PON 1HO Canada
Rettie, W. James. 2004. Morphology of female Woodland Caribou, Rangifer tarandus caribou, in Saskatchewan. Canadian Field-
Naturalist 118(1): 119-121.
I obtained morphological measurements from captured female Woodland Caribou in central Saskatchewan. I found that only
girth was a good predictor of body mass in adult animals. I also determined that Woodland Caribou from Saskatchewan, though
similar in size and mass to alpine Woodland Caribou in Yukon, are larger than migratory Woodland Caribou and smaller than
forest dwelling Woodland Caribou from western Alberta and Yukon.
Key Words: Woodland Caribou, Rangifer tarandus caribou, morphology, Saskatchewan.
Body sizes and body masses of subspecies and pop-
ulations of Rangifer tarandus (Eurasian Reindeer and
North American Caribou) vary considerably (e.g.,
Dauphiné 1976; Thomas 1982; Reimers 1983; Chan-
McLeod et al. 1995) in response to a wide range of cli-
matic and other environmental conditions (Skogland
1983; Reimers 1983). In North America, there is also
a high degree of morphological variation within the
Woodland Caribou subspecies (R. t. caribou). The
best described populations of Woodland Caribou are
those in Yukon (Gauthier and Farnell 1986; Kuzyk et
al. 1999) and in Québec and Labrador (Parker 1981;
Huot 1989). However, the subspecies has a more or
less continuous distribution across northern Canada and
the variations in climate, topography, and plant and
animal communities across the range of the subspecies
might be expected to favour different body sizes and
masses in different areas. In particular, Skogland (1983)
argued that morphology was density-dependent and
related to the factors limiting population growth. Both
Skogland (1983) and Chan-McLeod et al. (1999)
reported that female R. tarandus that had reproduced
successfully were significantly lighter the following
winter than those that had not. Here, I present the first
description of Woodland Caribou from central Saskat-
chewan and a discussion of their morphology relative
to limiting factors.
Study Area and Methods
As part of research into population dynamics (Rettie
and Messier 1998) and behaviour (Rettie and Messier
2000, 2001), I captured 43 female Woodland Caribou
in central Saskatchewan (approximately 54° N to
55°30’ N and 104° W to 109° W). All animals were
captured in winter (dates between 13 December and
14 March) between March 1992 and January 1995.
At the time of capture I used a flexible steel tape to
measure the following parameters from most animals:
total body length, body length to base of tail, girth (all
to the nearest cm), mandible, and metatarsal lengths (to
the nearest 5 mm). Methods followed those of Dauphiné
(1976), modified for application to live animals. I mea-
sured body mass to the nearest kilogram for ten animals
using an electronic load scale (Senstek, Saskatoon,
Saskatchewan) suspended from a tripod or beneath a
helicopter. I also extracted a tooth from most animals
for aging. Further details on capture and aging appear
in Rettie and Messier (1998). Animal capture and
handling procedures followed animal care protocol
number 920092 of the University of Saskatchewan.
Using natural log transformed values from the eight
adult animals for which I had complete sets of data as
well as body mass, I applied a stepwise multiple linear
regression to assess the relationship of body measure-
ments to body mass (p = 0.05 to enter, p = 0.10 to
exit) and then applied the resulting equation to the
morphometric data for all animals. I then tested for
differences in calculated body mass for adult females
that were accompanied by a calf at time of capture and
those that were without a calf. All statistical analyses
were conducted using SPSS for Windows Version 10.0.7
(SPSS Inc. 2000).
Results and Discussion
I had morphometric data from 34 adult animals
(>31 months old at time of capture) and from three
yearlings (19-22 months old at time of capture). The
summary statistics for all measurements appear in
119
120
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE |: Morphological measurements and actual and calculated body mass of adult female Woodland Caribou in central
Saskatchewan.
Parameter n
Actual body mass 9
Calculated body mass” 32
Body length to base of tail 33
Total body length 33
Metatarsal length 30
Shoulder to hoof tip 15
Girth 32
Mandible length 32
“ Body mass kg calculated using the equation arising from the regression analysis: e
mean + | sd range
131 + l6kg 96 -156kg
LS eye like 96 —-160kg
LOLS =p isiem 165 -—217cm
200)=9 = lsicm 177. —230cm
43.0 + 14cm 41.0 — 46.0 cm
Il). ee W/m 102. —126cm
AS) eee ikem 115) —154cm
S14 ei ple8 cm 28.0 — 35.0cm
1.76 In Girth — 3.78
TABLE 2: Morphological measurements and actual body mass of yearling female Woodland Caribou in central
Saskatchewan.
Parameter n
Actual body mass ]
Body length to base of tail 3}
Total body length 3
Metatarsal length 3
Girth 3
Mandible length 3
Tables 1 (adult animals) and 2 (yearling animals).
When compared to Yukon Woodland Caribou, the
animals in Saskatchewan are almost as tall at the shoul-
der (115 cm vs. 116 cm), are the same girth (129
cm), but are not as long (191 cm vs. 206 cm) as the
alpine animals measured by Kuzyk et al. (1999).
Saskatchewan caribou are smaller than forest
dwelling Woodland Caribou from Yukon (Kuzyk et
al. 1999) and from western Alberta (Gauthier and
Farnell 1986) in all comparable parameters.
From the regression analysis, I concluded that
only girth was significantly related to body mass (p
=0.04, r? = 0.78). I used the resulting equation, where
girth is measured in cm:
calculated body mass (kg) = e(!-76/Girth — 3.78
to calculate body mass for all adult animals for
which I had girth measurements. The calculated body
mass values appear in Table 1. Figure 1 shows the
relationship between girth and body mass and its 95%
prediction interval. Untransformed data are presented
in the figure while analyses were based on natural
log transformed data. The wide prediction interval in
Figure | suggests that further sampling is required to
reduce uncertainty in the girth-body mass relationship.
The relationship is particularly weak for smaller girths
where the relationship is influenced by a single obser-
vation. Though the summarised measurements present
a reference point for future studies on morphological
variation in Woodland Caribou, the prediction of body
mass from body measurement and the equation pre-
mean + | sd range
98 kg
GQ es. 3) con 170 —1175 cm
185i lem 182 —1188 cm
41.7 + 0.6cm 41.0 -— 142.0cm
See eee Src 110 —1116cm
28.2 + 2.0cm 26.0 — 130.0cm
sented should be made cautiously (Cattet et al. 1997).
Finally, I did not detect a difference in calculated body
mass between adult animals with and without a calf-at-
heel at time of capture (¢-test, t= 0.30, df = 30, p = 0.76).
Skogland (1983) argued that body sizes in R. tar-
andus were density-dependent, the larger body size
200 body mass = @(1-76!n Girth - 3.78)
*=0.78
180 r S52
P=0.004 -
160 aa
Body mass (kg)
XD
oO
110 120 130 140 150
Girth (cm)
FiGurE 1. Relationship between girth (cm) and body mass (kg)
for adult female Woodland Caribou in Saskatchewan.
Solid line represents the equation derived through
multiple linear regression; dashed lines represent the
95% prediction interval of the equation. Filled squares
represent data used to derive the equation.
2004
in North American Caribou being attributed to their
low densities, a consequence of limitation by predation
rather than by food resources. Amongst Woodland
Caribou populations, the George River Caribou Herd
in Quebec and Labrador is food limited and contains
the smallest individuals (Parker 1981; Huot 1989).
The body sizes of Woodland Caribou in Saskatchewan
are larger than George River Herd animals and support
the argument that Saskatchewan populations are not
food limited (Rettie and Messier 1998). As with the
larger animals in Caribou populations in western Al-
berta and Yukon (Edmonds 1988; Kuzyk et al. 1999),
predation is the likely proximate limiting factor for
Saskatchewan Woodland Caribou populations (Rettie
and Messier 1998).
Skogland (1983) also suggested that predator in-
duced constraints on lifetime reproductive success led
to larger body size in North American Caribou by de-
laying reproductive maturity in favour of increased
somatic growth. However, yearling female Woodland
Caribou in Saskatchewan were not only pregnant
(Rettie and Messier 1998) but larger than both adult
Reindeer (Skogland 1983) and adult migratory Wood-
land Caribou (Huot 1989). Relative to observations in
Norway, there does not appear to be a trade off being
made between reproduction and somatic growth. In-
stead, Saskatchewan Woodland Caribou appear able to
mature as yearlings and still achieve large adult body
sizes. My failure to detect differences in body mass
between reproductive classes may represent a lack of
difference, result from a poor predictive ability of my
equation for body mass, or be a consequence of inter-
annual variation as reported by Chan-McLeod et al.
(1999).
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Chan-McLeod, A. C., R. G. White, and D. E. Russell. 1999.
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Saskatchewan. Canadian Journal of Zoology 76: 251-259.
Rettie, W. J., and F. Messier. 2000. Hierarchical habitat
selection by woodland caribou: its relationship to limit-
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Rettie, W. J., and F. Messier. 2001. Range use and movement
rates of woodland caribou in Saskatchewan. Canadian
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Skogland, T. 1983. The effects of density dependent res-
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Received 3 December 2002
Accepted 21 May 2004
122 THE CANADIAN FIELD-NATURALIST Vol. 118
Occurrence of Parasitoid Wasps, Baeus sp. and Gelis sp., in the Egg Sacs
of the Wolf Spiders Pardosa moesta and Pardosa sternalis (Araneae,
Lycosidae) in Southeastern Idaho
LisA M. Coss! and VINCENT A. CoBB?
Department of Biological Sciences, Idaho State University, Pocatello, Idaho 83209 USA
Current Addresses:
'Department of Biology, Cumberland University, Lebanon, Tennessee 37087 USA
*Department of Biology, Middle Tennessee State University, Murfreesboro, Tennessee 37132 USA
Cobb, Lisa M., and Vincent A. Cobb. 2004. Occurrence of parasitoid wasps, Baeus sp. and Gelis sp., in the egg sacs of the
wolf spiders, Pardosa moesta and Pardosa sternalis (Araneae, Lycosidae) in southeastern Idaho. Canadian Field-
Naturalist 118(1): 122-123.
Egg sacs of the wolf spiders Pardosa moesta and Pardosa sternalis were sampled for two years during June to September in
southeastern Idaho. Parasitoid wasps, Baeus sp. (Sceleonidae) and Gelis sp. (Ichneumonidae), were observed in the egg sacs
of both Pardosa species. Of 322 egg sacs examined, 14.6% were parasitized. Parasitism of egg sacs occurred throughout
most of the Pardosa egg sac-carrying season.
Key Words: Wolf Spider, Pardosa moesta, P. sternalis, egg sac, predation, parasitic wasps, Baeus sp., Gelis sp., parasitoid,
reproduction.
Parasitic wasps are well known predators of spiders
and may serve as either ectoparasites (e.g., externally
feeding on the body) or endoparasites (e.g., feeding on
eggs and developing young within egg sacs) (Foelix
1982). Larval endoparasites that consume spiders eggs
are classified as parasitoids (Roberts and Janovy 2000)
with the most speciose family of parasitoid wasps be-
ing the Ichneumonidae (Godfray 1994). To parasitize
a spider egg sac, wasps insert their ovipositor into the
wall of the egg sac and lay eggs which develop into
larvae and predate the spider eggs (Austin 1985).
Female wolf spiders (Lycosidae) have the conspic-
uous behavior of carrying their egg sacs attached to
their spinnerets. Although it would appear that such
behavior could provide substantial maternal care, para-
sitism of egg sacs still occurs. The wasps Baeus (Scel-
ionidae) and Gelis (Ichneumonidae) have been found
in previous studies to be common parasitoids of Lyco-
sidae egg sacs (Kaston 1948; Edgar 1971a; Austin
1985).
Wolf spiders in the genus Pardosa are common
ground-dwelling spiders throughout much of the north-
ern hemisphere (Edgar 1971b; Dondale and Redner
1990; Buddle et al. 2000). Their reproductive period
may last several months (Edgar 1971b; Cobb 1992;
Buddle 2000) and some species may produce multi-
ple clutches during a single season (Edgar 1971b; Wolff
1981).
The main focus of this study was an investigation
of the reproductive ecology of P. moesta (Banks) and
P. sternalis (Thorell) in eastern Idaho. Cobb (1992) sug-
gested that in southeastern Idaho both species have a
tendency to produce multiple clutches within a season.
During the study, P. moesta and P. sternalis females
and their egg sacs were collected between one and five
times per month from June through September of 1990
and 1991. All collections occurred in a two hectare
meadow near the base of Scout Mountain (Caribou Na-
tional Forest, Bannock County, Idaho) at an elevation
of approximately 2000 m. During the late spring and
early summer the meadow was marshy, fed by a moun-
tain stream. However, in late summer and early fall the
meadow was dry and had been grazed by cattle. For
each spider and corresponding egg sac we collected a
variety of morphometric data, which included female
mass, clutch mass, and clutch size. While examining
the egg sacs we discovered several of them were para-
sitized.
Identifiable parasitoids of P. moesta and P. stenalis
egg sacs were wasps of the families Scelionidae and
Ichneumonidae. P. M. Marsh, of the USDA Agricultural
Research Station, Beltsville, Maryland, identified the
scelionid specimens as Baeus sp., and the ichneumonids
at Gelis sp. All but two of the identifiable parasitoids
for both Pardosa species were Baeus sp. Two egg sacs
of P. sternalis were found with a single Gelis sp.
each. The Gelis were collected on 23 June and 22
July 1991. Pupal parasitoids inside the egg sacs could
not be identified to species. Because not all individ-
ual parasitoids could be identified, other parasitoid
genera may have been present in the egg sacs.
Of 134 egg sacs for P. moesta and 188 egg sacs for
P. sternalis, 47 were infected with parasitoids (14.6%
parasitism overall). Within these infected egg sacs
281 parasitoids were counted. Parasitism rate was
12.7% for P. moesta and 16% for P. sternalis (Table
1). Egg sacs were found parasitized from June to Sep-
tember for P. moesta and P. sternalis. During mid and
late May 1990, a sample of egg sacs was collected from
P. sternalis but none contained parasitoids. All of the
P. sternalis egg sacs in the May collection contained
eggs only and no spider instar stages, indicating egg
|
|
2003
TABLE |. Number of parasitized egg sacs for Pardosa moesta
(n = 134) and Pardosa sternalis (n = 188) from southeastern
Idaho. Data are represented as number of egg sacs with para-
sitoids (number of egg sacs sampled).
P. moesta P. sternalis
Month 1990 199] 1990 199]
June 0 (23) = 8 (37) Le CS)
July 1 (40) 1 (9) 7 (45) Be (60)
August 12 (25) = 6 (15) IP (G21)
September 0 (27) 3(10) Dea alisia) Die (i)
sac formation had begun only recently. The number
of parasitoids per egg sac varied considerably. Mean
(+ SE) number of parasitoids per egg sac for P. moes-
ta was x = 5.1 + 1.4 (range = 2 - 15) in 1990 and
x = 6.5 + 2.3 (range = 1 - 12) in 1991. For P. sternalis,
the number of parasitoids per egg sac was x = 5.7 + 1.6
(range = | - 37) in 1990 and x = 8.4 + 4.6 (range = 1
- 35) in 1991.
This study indicates that parasitism occurred through-
out the egg carrying season and was highest in Aug-
ust 1990 and September 1991. Interestingly, these high
parasitism rates correspond to times when Pardosa in
this region are producing smaller egg clutches (Cobb
1992). Several species of Pardosa have their greatest
reproductive output early in the reproductive season
and produce smaller egg sacs and fewer eggs later in
the season (Eason 1969). Potentially, these higher para-
sitism rates in the late summer could have resulted in
selection for greater spring reproduction in Pardosa.
Although parasitism has been documented for several
species of Pardosa (Eason et al. 1967), recorded levels
of parasitism are uncommon and variable. Eason (1969)
indicated egg parasitism rates of less than one percent
in P. lapidicina in Arkansas, while Edgar (1971a) ob-
served levels that ranged from 3% to 35% in Scotland.
Our data indicate variable and sometimes high levels
of parasitism as well. Such high levels of parasitism
have been shown to reduce the number of spiders in
the field (van Baarlen et al. 1994) as well as the re-
cruitment of young (Edgar 1971a). Although we have
documented seasonal variation in parasitism rate, we
do not know if these Pardosa populations are being
negatively impacted by parasitoids.
Acknowledgments
We thank P. M. Marsh of the U.S. Department of
Agriculture for identifying parasitoid wasps and J.
Redner of the Canadian Department of Agriculture for
the initial identification of spider specimens. Funding
NOTES
for this project was provided partly by a grant to L.
Cobb from the Idaho State University Graduate Res-
earch Committee.
Literature Cited
Austin, A. D. 1985. The function of spider egg sacs in rela-
tion to parasitoids and predators with special reference to
the Australian fauna. Journal of Natural History 19: 359-
370.
Buddle, C. M. 2000. Life history of Pardosa moesta and Par-
dosa mackenziana (Araneae: Lycosidae) in central Alberta,
Canada. Journal of Arachnology 28: 319-328.
Buddle, C. M., J. R. Spence, and D. W. Langor. 2000.
Succession of boreal forest spider assemblages following
wildfire and harvesting. Ecography 23: 424-436.
Cobb, L. M. 1992. Reproductive tactics of two sympatric
species of Pardosa (Araneae, Lycosidae). M.S. thesis.
Idaho State University, Pocatello, Idaho. 59 pages.
Dondale, C. D., and J. H. Redner. 1990. The insects and
arachnids of Canada. Part 17. The wolf spiders, nursery-
web spiders, and lynx spiders of Canada and Alaska
(Araneae: Lycosidae, Pisauridae, and Oxyopidae). Agri-
culture Canada Publication 1856.
Eason, R. R. 1969. Life history and behavior of Pardosa
lapidicina Emerton (Araneae: Lycosidae). Journal of the
Kansas Entomological Society 42: 339-360.
Eason, R. R., W. B. Peck, and W. H. Whitcomb. 1967. Notes
on spider parasites, including a reference list. Journal of
the Kansas Entomological Society 40: 422-434.
Edgar, W. D. 1971a. Aspects of the ecology and energetics
of the egg sac parasites of the wolf spider Pardosa lugu-
bris (Walckenaer). Oecologia 7: 155-163.
Edgar, W. D. 1971b. The life-cycle, abundance and seasonal
movement of the wolf spider, Lycosa (Pardosa) lugubris, in
central Scotland. Journal of Animal Ecology 40: 303-322.
Foelix, R. F. 1982. Biology of spiders. Harvard University
Press, Cambridge, Massachusetts.
Godfray, H. C. J. 1994. Parasitoids: Behavioral and evolu-
tionary ecology. Princeton University Press, Princeton, New
Jersey.
Kaston, B. J. 1948. Spiders of Connecticut. State Geology
and Natural History Survey of Connecticut Bulletin 70.
1020 pages.
Roberts, L. S., and J. Janovy Jr. 2000. Gerald D. Schmidt
and Larry S. Robert’s Foundations of Parasitology. 6" edi-
tion. McGraw-Hill, Boston, Massachusetts.
Van Baarlen, P. 1994. Eggsac parasitism of money spiders
(Araneae: Linyphiidae) in cereals, with a simple method for
estimating percentage parasitism of Erigone spp. eggsacs
by Hymenoptera. Journal of Applied Entomology 118:
217-223.
Wolff, R. J. 1981. Wolf spiders of the genus Pardosa (Ara-
neae: Lycosidae) in Michigan. Great Lakes Entomologist
14: 63-68.
Received 4 March 2002
Accepted 14 June 2004
124
THE CANADIAN FIELD-NATURALIST
Vol. 118
The Northern True Katydid, Pterophylla camellifolia (Orthoptera:
Pseudophyllidae), at Ottawa, Ontario
STEPHEN J. DARBYSHIRE
Agriculture and Agri-Food Canada, Central Experimental Farm, Saunders Building #49, Ottawa, Ontario K1A 0C6 Canada
Darbyshire, Stephen J. 2004. The True Katydid (Prerophylla camellifolia) at Ottawa, Ontario. Canadian Field-Naturalist
118(1): 124-126.
Five males of the Northern True Katydid (Pterophylla camellifolia) are reported from Ottawa, Ontario (approximately
45°25°N, 75°42’W), in 2001 and 2002 at three separate locations. Based on its distribution and habits extralimital
occurrences in Ottawa are likely due to chance introduction.
Key Words: Northern True Katydid, Pterophylla camellifolia, Ontario, distribution, insect dispersal.
In mid-August 2001 two male Northern True Katy-
dids, Pterophylla camellifolia (Fabricius), were heard
calling at a site in an urban residential area of eastern
Ottawa, Ontario (location 1, Figure 1). Calling contin-
ued until about 9 October when daily minimum tem-
peratures fell below freezing. Calling perches in trees
were located between 5 and 10 metres above the ground.
Several species of trees were utilized, including Sugar
Maple (Acer sacharrum Marsh.), Norway Spruce
(Abies balsamea (L.) Mill.) and Red Oak (Quercus
rubra L.). Over the calling period they moved short
distances (less than 50 metres horizontally) from one
tree to another, but were never heard calling together in
the same tree (it was assumed that the two males heard
repeatedly were the same two individuals). Prerophylla
camellifolia is not usually associated with coniferous
trees and the Norway Spruce was occupied for only a
single night.
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FiGurE 1. Map of the Ottawa urban area showing the locations of calling males of Pterophylla camellifolia, approximately
45°25°N, 75°42’ W. Location 1: two males in 2001; location 2: one male in 2002; location 3: two males in 2002.
2004
NOTES
FIGURE 2. Male Pterophylla camellifolia from Ottawa, Ontario (location 3, Figure 1). Photographed 19 September 2002.
Katydids were also heard calling in August, Septem-
ber, and early October 2002 at two other locations
within urban Ottawa (locations 2 and 3, Figure 1). At
location 2 (Figure 1) a single male was heard calling
from a large silver maple (Acer saccharinum L.) at a
height of about 10 metres. It remained in the same tree
throughout the observation period (about two months).
At location 3 (Figure 1), two individuals were heard
calling in a landscaped area around a large apartment
complex. Perches were about three to four metres high
in English Oak (Quercus robur L.) and Crab Apple
(Malus sp.). Calling continued at these two locations
until about 10 October, when night-time temperatures
began to approach freezing.
Since the insect is univoltine (Riley 1874; Caudell
1906; Hebard 1941), searches were made of about
1 km around location 1 in September 2002 and 2003
and about 0.5 km? around locations 2 and 3 in Sep-
tember 2003. Although repeated searches were made
on warm evenings after complete darkness, no individ-
uals were heard calling at location | in 2002, or at any
of the sites in 2003.
The range of Pterophylla camellifolia is reported to
be from Massachusetts to north-central Florida, west-
ward through southern New York, southern Ontario
and Michigan to Iowa, Kansas, Oklahoma and eastern
Texas (Hebard 1941; Vickery and Kevan 1983). Caul-
_ field (1887) was the first to report the species in Ontario
(under the name Platyphyllum concavum). The known
distribution is primarily along the north shore of Lake
Erie from the Niagara Peninsula to Essex County in
southwestern Ontario and largely coincident to the
Carolinian forest region (Vickery and Kevan 1985).
The family Pseudophyllidae contains about 1000,
mostly tropical, species. In Canada, the only represen-
tative of the family is Prerophylla camellifolia. Although
there are a few similar large green tettigoniid species
in eastern Canada, P. camellifolia is readily distin-
guished morphologically by its large size (about 25-
50 mm) and its ovate, strongly convex tegmina (outer
or front wings) which are slightly longer than the abdo-
men (Vickery and Kevan 1983, 1985). The loud ono-
matopoeic stridulations (chirps) also readily distinguish
this species (audio file: Walker and Moore 2003*).
Differences in pulse number and pulse frequency of
the chirp occur throughout the range of the species
(Alexander 1968) and with environmental conditions
(Shaw 1975). The most common chirp is of three to
five pulses followed by a short pause (Caudell 1906).
Males heard in Ottawa produced three, or sometimes
two or four, pulses per chirp. Hebard (1941) recognized
two species of Prerophylla in the United States, one
restricted to Florida and the other widespread in North
America with considerable variation suggesting a sin-
gle polymorphic species with five geographic races
(subspecies). The northern type present in Ontario is
P. camellifolia camellifolia.
Blatchley (1920) stated that open forests are pre-
ferred, although Hebard (1941) found the insect most
common in dense forests, particularly where large oaks
occur. Calling perches are usually in canopies when-
ever tall trees are present, 25 to 100 feet (7.6-30.5 m) or
above (Hebard 1941; Shaw and Carlson 1969). Where
tall trees are absent, calling will occur from lower perch-
es in small trees, orchards and shrubbery (Caudell 1906;
Blatchley 1920; Hebard 1941). This is consistent with
the observations of individuals in Ottawa.
2003
Throughout most of the species’ range males mature
and begin calling in July and continue through to the
advent of cold weather: late July to late September or
early October in lowa (Shaw and Carlson 1969); late
July to early October (rarely to early November) in
Washington, D.C. (Caudell 1906); 30 July to 10 Octo-
ber in Michigan (Cantrall 1968); and, 10 July to 27
October in Indiana (Blatchley 1920). During the first
severe frosts of autumn the insects fall to the ground
(Hebard 1941) and perish unless the weather subse-
quently moderates.
Although possessed of tegmina and hind wings,
Pterophylla camellifolia does not fly, the wings being
used to parachute or glide from one perch to a lower
one or to the ground (Caudell 1906; Hebard 1941;
Shaw and Carlson 1969; Vickery and Kevan 1985).
When on the ground or accessing higher perches they
walk. Individuals normally travel only short distances
during their lifetime (Caudell 1906; Hebard 1941),
but may often move from tree to tree.
The Northern True Katydid seems to be expanding
its range northwards and westwards, with recent reports
placing calling males in southern Minnesota (as far
north as the Twin Cities area) (Tekiela 2002*), south-
eastern North Dakota (Walker and Moore 2003*), and
Colorado (Weissmann and Leatherman 1992: Walker
and Moore 2003*). In Ontario recent sightings have
been at Barrie (Sinclair 1998*) and Toronto (D. A.
Sutherland, personal communication).
What are the mechanisms by which this large flight-
less insect could expand its range northward and west-
ward to areas distant from its previous distribution?
The new extralimital records in Ontario come from
more-or-less urban regions, which suggests that inad-
vertent human transportation is involved. The apparent-
ly independent immigrations detected in the Ottawa
area have been to well-established residential areas
where commercial truck or rail traffic would not be a
likely mechanism. It seems possible that nymphs or
adults may be carried on non-commercial vehicles
moving from southern regions during the early part
of the summer. A trip from the contiguous range to the
Ottawa area would take a minimum of 8-10 hours.
The highway system and vehicle traffic have made such
a trip possible for many decades now, yet immigra-
tion has been noticed only recently. As it is one of the
loudest insects in North America, the presence of
mature males in residential areas is very conspicuous
in spite of their cryptic green colouration and usually
inaccessible calling perches. No females have been
found in the Ottawa area yet and there is no evidence
of an established breeding population.
Acknowledgments
D. A. Sutherland (Natural Heritage Information
Centre, Peterborough, Ontario) provided observations
on the occurrence of P. camellifolia in Toronto and
discussed aspects of dispersal. Jean-Francois Landry
and Henri Goulet (Agriculture and Agri-Food Canada,
NOTES
126
Ottawa, Ontario) kindly read earlier versions of the
manuscript and provided constructive criticism.
Documents Cited (marked * in text)
Sinclair, A. 1998. Pterophylla camellifolia “Northern True
Katydid”. http://www.muskoka.com/~sinclair/katy.html
[accessed 23 December 2003].
Tekiela, S. 2002. Minnesota Profile: Katydids. http://www.
dnr.state.mn.us/volunteer/julaug00/katydids.html [accessed
23 December 2003].
Walker, T. J., and T. E. Moore. 2003. Singing insects of
North America. http://buzz.ifas.ufl.edu/index.htm [accessed
23 December 2003].
Literature Cited
Alexander, R. D. 1968. Arthropods. Pages 167-216 in Animal
communication: techniques of study and results of research.
Edited by T. A. Sebeok. Indiana University Press, Bloom-
ington, Indiana. 686 pages.
Blatchley, W. S. 1920. Orthoptera of northeastern America
with especial reference to the fauna of Indiana and Florida.
Nature Publishing Co., Indianapolis, Indiana. 784 pages.
Cantrall, I. J. 1968. An annotated list of the Dermaptera,
Dictyoptera, Phasmatoptera and Orthoptera of Michigan.
The Michigan Entomologist 1: 299-346.
Caudell, A. N. 1906. Class I, Hexapoda. Order XI, Orthop-
tera. The Cryptophylli of the United States. Journal of
the New York Entomological Society 14: 32-45.
Caulfield, F. B. 1887. A sketch of Canadian Orthoptera.
Eighteenth Annual Report of the Entomological Society
of Ontario. Pages 59-72.
Hebard, M. 1941. The group Pterophyllae as found in the
United States (Orthoptera: Tettigoniidae, Transactions of
the American Entomological Society 67: 197-219.
Riley, C. V. 1874. Katydids. Pages 150-169 in Sixth annual
report on the noxious, beneficial and other insects of the
State of Missouri.
Shaw, K. C. 1975. Environmentally-induced modification
of the chirp length of males of the True Katydid, Ptero-
phylla camellifolia (F.) (Orthoptera: Tettigoniidae). Annals
of the Entomological Society of America 68: 245-250.
Shaw, K. C., and O. V. Carlson. 1969. The true katydid,
Pterophylla camellifolia (Fabricius) (Orthoptera: Tetti-
goniidae) in Iowa: two populations which differ in behav-
iour and morphology. Iowa State Journal of Science 44:
193-200.
Vickery, V. R., and D. K. McE. Kevan. 1983. A monograph
of the Orthopteroid insects of Canada and adjacent regions.
Lyman Entomological Museum and Research Laboratory
memoir, number 13. 2 volumes, 1462 pages.
Vickery, V. R., and D. K. McE. Kevan. 1985. The grass-
hoppers, crickets, and related insects of Canada and adja-
cent regions. Ulonata: Dermaptera, Cheleutoptera, Notop-
tera, Dictuoptera, Grylloptera, and Orthoptera. The insects
and arachnids of Canada. Part 14. Agriculture Canada,
Research Branch Publication 1777. 918 pages.
Weissmann, M. J., and D. A. Leatherman. 1992. Range
extension of the northern true katydid, Prerophylla camel-
lifolia (F.) (Orthoptera: Tettigoniidae Pseudophyllinae) into
eastern Colorado. Journal of the Kansas Entomological
Society 65: 448-449.
Received 28 November 2002
Accepted 6 January 2004
2004
L. Davip Mecu!? and SHAWN TRACY?
Jamestown, North Dakota 58401-7317 USA
127-129.
} couver Island, British Columbia, Canada.
Wolf (Canis lupus) densities are highly variable
' (Mech 1970), depending generally on prey biomass
| density (Keith 1983; Fuller 1989). Because prey bio-
| mass density is related inversely to latitude, Wolves
| tend to reach their highest densities at lower latitudes
| (Mech and Boitani 2003). The highest reported natu-
| rally occurring Wolf density is 14.1 Wolves/100 km?
| for a pack of nine Wolves on Vancouver Island (Scott
_ and Shackleton 1982).
| Herein we report on a Minnesota Wolf pack with a
| density higher for two years than the highest density
| reported elsewhere.
| Study area
| We studied the Farm Lake Wolf pack (FLP) that in-
| habited the Superior National Forest (SNF) of north-
| eastern Minnesota where most of the Wolf’s diet is
| White-tailed Deer (Odocoileus virginianus). The Wolf
| packs in the SNF are spaced into territories (Mech
| 1973, 1986) and the FLP territory, 10.0 km east of
| Ely (48°N, 92°W), was surrounded by four or five other
pack territories. The terrain, vegetation, and land use
| in the territory are typical of the surrounding region
| (Mech 1973). However, during winter, much of the ter-
| ritory encompasses part of the Garden Lake deer yard
(Nelson and Mech 1981). Deer densities there in the
| late 1970s were estimated at 16-23 deer/km? (Nelson
| and Mech 1981), and the deer population in the gen-
eral area has increased considerably since then (Mech
| and Nelson 2000).
Methods
‘| Wolves were live-trapped, radio-tagged, aerially
|) radio-tracked weekly when possible, and aerially ob-
|) served with their packs during winter. Estimates of FLP
|) territory size were made for summer (1 April—30 Sep-
ii tember), winter (1 October—31 March) and the entire
|}, year (1 April-31 March) from 1 October 1997 through
| 30 March 1999.
NOTES
‘Biological Resources Division, U.S. Geological Survey, Northern Prairie Wildlife Research Center, 8711
127
Record High Wolf, Canis lupus, Pack Density
- 37" Street, SE,
*University of Minnesota, Department of Fisheries and Wildlife, 1980 Hodson Hall, St. Paul, Minnesota 55108 USA
| 3The Raptor Center, 1920 Fitch Avenue, University of Minnesota, St. Paul, Minnesota 55108 USA
Mech, L. David, and Shawn Tracy. 2004. Record high Wolf, Canis lupus, pack density. Canadian Field Naturalist 118(1):
_ This report documents a year-around Wolf (Canis lupus) density of 18.2/100 km? and a summer density of 30.8/100 km?, in
a northeastern Minnesota Wolf pack. The previous record was a summer density of 14.1/100 km?, for a Wolf pack on Van-
| Key Words: Wolf, Canis lupus, Minnesota, Superior National Forest, White-tailed Deer, Odocoileus virginianus.
We used ArcView (copyrighted) GIS (ESRI Inc.,
Redlands, California) to estimate each period’s terri-
tory area corresponding to the combination of all FLP
radio-tagged Wolves. UTM coordinates of the FLP
Wolf locations were imported into ArcView GIS and
converted into point data. Minimum Convex Polygons
(Mohr 1947) were then constructed using Animal
Movement (Hooge and Eichenlaub 1997) extension
to Arcview.
By using observation curve analysis we determined
when a territory was defined (Odum and Kuenzler
1955). We subsampled period Wolf locations without
replacement, increasing the number of samples (loca-
tions) with each subsample treatment, and calculated
territory area from each subsample. Five repetitions of
each subsample were performed to generate a corres-
ponding mean territory area for each subsample. The
mean areas were then plotted against number of loca-
tions in the subsample. We considered territories de-
fined when there was <1% change in area (suggesting
asymptotic behavior) as a result of the addition of one
more sample.
We determined pack size through the winter aerial
surveys. The greatest number of Wolves seen was con-
sidered the pack size. Vegetative cover prevented aerial
surveys in summer. Pack sizes were divided by their
territory size and then multiplied by 100 to give den-
sity in Wolves/100 km’.
Results
We radio-tagged and tracked adult female Wolf 667
and male pup 673 (born in 1997) from 1 October 1997
through 30 March 1999 for this study (Table 1). A
total of 127 Wolf locations were obtained, with one
Wolf location defined as when one Wolf was at a point.
If both Wolves were together, two locations were re-
corded. Observation curve analysis suggested that 30
locations were needed to accurately define the winter
1997-1998 FLP territory, 50 samples for the 1998-1999
128
THE CANADIAN FIELD-NATURALIST
TABLE |. Background data for calculations of Wolf density in the Farm Lake Pack, northeastern Minnesota.
Period Number of Locations
1 October 1997 — 30 March 1998 39
1 April 1998 — 30 September 1998 44
1 October 1998 — 30 March 1999 44
1 April 1998 — 30 March 1999 88
Vol. 118
Number of Wolves Areakm? — Density/100 km?
4 22.88 17.5
— 19.50 30.8"
6 32.88 18.2
6 32.88 18.2
“Assuming only six Wolves, the number observed during the following winter.
territory, and 30 and 35 samples for the FLP summer
and winter periods, respectively. In all these periods,
these criteria were met (Table 1).
During winter 1997-1998, the FLP contained four
members and used an estimated area of 22.88 km?, a
density of 17.5 Wolves/100 km. In winter 1998-1999,
six FLP Wolves used an area of 32.88 km2, a density
of 18.2 Wolves/100 km?, and in summer only 19.5 km?
for a minimum density of 30.8 Wolves/100 km?
(Table 1).
Discussion
The Wolf densities we found exceeded the highest
previous record of 14.1 Wolves/100 km? for a Wolf
pack on Vancouver Island (Scott and Shackleton 1982).
Hebert et al. (1982), citing the Scott and Shackleton
(1982) study, claimed a density of one Wolf per 6.3
km, or 15.9/100 km?. However, Hebert et al. (1982)
included a third pack not mentioned by Scott and
Shackleton and presented no territory area data for this
pack. Density estimates using radio-locations can be
greatly influenced by the number and timing of loca-
tions. Our locations were evenly distributed throughout
the year and met the observation curve test (Odum and
Kuenzler 1955), even though the number of locations
available were fewer than recommended by others
(Fritts and Mech 1981; Bekoff and Mech 1984; Ballard
et al. 1987). No doubt the much smaller size of our ter-
ritory explains why fewer locations were needed to
define it.
It is notable that the previous high record Wolf
density (14.1 Wolves/100 km?) was based only on
summer locations during a relatively short period (11
April to 10 September). Furthermore, this period was
before when most of the year’s mortality occurs (Fuller
et al. 2003). Thus the earlier density is not strictly
comparable to either our year-around or winter den-
sities.
The extraordinarily small FLP territory areas of
1997-1998 and 1998-1999 resulted in the highest doc-
umented Wolf density to date. This density was no
doubt related to the high winter deer density in the area
as well as to the relatively harsh winters during that
period, with deep snow and extreme cold, that would
have caused deer to concentrate with greater density.
We know of no garbage dump or other regular source
of food in this territory.
Even so, our highest Wolf density (30.8 Wolves/
100 km?) occurred in summer, and it was a minimum
estimate because it was based on the pack size the
following winter, after any mortality may have oc-
curred. Thus the winter deer density at first seems
irrelevant. However, possibly such a high deer den-
sity allowed the Wolves to add sufficient fat and to
cache enough surplus food to help carry them through
the summer. In any case, this study demonstrates the
extreme density that Wolf densities can reach when
prey is plentiful.
Acknowledgments
This study was supported by the Biological Res-
ources Division of the U.S. Geological Survey and the
U.S. Department of Agriculture North Central Forest
Experiment Station.
Literature Cited
Ballard, W. B., J. S. Whitman, and C. L. Gardner. 1987.
Ecology of an exploited Wolf population in south-central
Alaska. Wildlife Monographs 98: 1-54.
Bekoff, M., and L. D. Mech. 1984. Simulation analyses of
space use: Home range estimates, variability, and sample
size. Behavior Research Methods and Instrumentation 16:
32-37.
Fritts, S. H., and L. D. Mech. 1981. Dynamics, movements,
and feeding ecology of a newly protected Wolf population
in northwestern Minnesota. Wildlife Monographs 80: 1-79.
Fuller, T. K. 1989. Population dynamics of Wolves in north-
central Minnesota. Wildlife Monograph 105: 1-41.
Fuller, T. K., L. D. Mech, and J. Fitts-Cochrane. 2003.
Population dynamics. Pages 161-191 in Wolves: Ecology,
Behavior, and Conservation. Edited by L. D. Mech and
L. Boitani. University of Chicago Press, Chicago, Illinois.
Hebert, D. M., J. Youds, R. Davies, H. Langin, D. Janz,
and G. W. Smith. 1982. Preliminary investigations of the
Vancouver Island Wolf (Canis lupus crassodon) prey
relationships. Pages 54-70 in Wolves of the world. Edited
by F. H. Harrington and P. C. Paquet. Noyes Publication,
Park Ridge, New Jersey.
Hooge, P. N., and B. Eichenlaub. 1997. Animal movement
extension to Arcview. Ver. 1.1. Alaska Biological Science
Center, U.S. Geological Survey, Anchorage, Alaska, USA.
Keith, L. B. 1983. Population dynamics of Wolves. Pages
66-77 in Wolves in Canada and Alaska. Edited by L. N.
Carbyn. Canadian Wildlife Service Report Series (45).
Mech, L. D. 1970. The Wolf: The ecology and behavior of
an endangered species. Doubleday Publishing Company,
New York.
2004
Mech, L. D. 1973. Wolf numbers in the Superior National
Forest of Minnesota. U.S. Department of Agriculture
Forest Service Research Paper NC-97.
Mech, L. D. 1986. Wolf numbers and population trend in
the Superior National Forest, 1967-1985. Research Paper
NC-270. U.S. Department of Agriculture, Forest Service,
North Central Forest Experiment Station, St. Paul, Min-
nesota. 6 pages.
Mech, L. D., and L. Boitani. 2003. Social ecology. Pages
1-34 in Wolves: Ecology, Behavior, and Conservation.
Edited by L. D. Mech and L. Boitani. University of
Chicago Press, Chicago, Illinois.
Mech, L. D., and M. E. Nelson. 2000. Do Wolves affect
white-tailed buck harvest in Minnesota? Journal of Wildlife
Management 64: 129-136.
NOTES
Mohr, C. O. 1947. Table of equivalent populations of North
American small mammals. American Midland Naturalist
37: 223-249.
Nelson, M. E., and L. D. Mech. 1981. Deer social organ-
ization and Wolf predation in northeastern Minnesota.
Wildlife Monographs 77: 1-53.
Odum, F. P., and E. J. Kuenzler. 1955. Measurement of
territory and home range size in birds. Auk 72: 128-137.
Scott, B. M. V., and D. M. Shackelton. 1982. A prelimi-
nary study of the social organization of the Vancouver
Island Wolf (Canis lupus crassodon). Pages 12-41 in
Wolves of the world. Edited by F. H. Harrington and P.
C. Paquet. Noyes Publication, Park Ridge, New Jersey.
Received 25 August 2002
Accepted 3 June 2004
Extraordinary Size and Survival of American Black Duck, Anas
rubripes, Broods
JERRY R. LONGCORE and DANIEL G. MCAULEY
United States Geological Survey, Patuxent Wildlife Research Center-Orono, 5768 South Annex A, Orono, Maine 04469-
5768 USA
Longcore, Jerry R., and Daniel G. McAuley. 2004. Extraordinary size and survival of American Black Duck, Anas
rubripes, broods. Canadian Field-Naturalist 118(1): 129-131.
Two female American Black Ducks (Anas rubripes) were initially observed during June 1982 with 20 Class Ib or 18-22 Class
Ta-b ducklings in two wetlands in Hancock County, Cherryfield, Maine. Fifteen of 20 ducklings (75%) in one brood and 16 of
18-22 ducklings (72-89%) in the other brood survived to fledge. These large broods probably resulted from post-hatch
brood amalgamation.
Key Words: American Black Duck, Anas rubripes, brood size, duckling survival, post-hatch brood amalgamation, Maine.
Exceptionally large broods of North American dab-
bling ducks (Anas spp.) that exceed average clutch
size (8-10 eggs, Zammuto 1986) occur when females
(1) lay extraordinarily large clutches, (2) lay eggs in
nests of conspecifics (“pre-hatch brood amalgamation”
(Pre-HBA), or brood parasitism; Eadie et al. 1988),
or (3) hatch their own clutches and acquire the brood
of another female (“‘post-hatch brood amalgamation”
| (Post-HBA); Eadie et al. 1988). Pre-HBA, which can
__ be either inter- or intra-specific, and post-HBA occur
| infrequently in the Anatini; only 3 of 9 species of Ana-
| tini were reported by Eadie et al. (1988) for either type.
Tufts (1986) in Nova Scotia reported brood amalga-
mation for three American Black Duck broods when
_ he released orphaned ducklings near females with
_ broods. Herein, we report two records of probable
post-HBA resulting in two extremely large broods of
wild American Black Ducks in Maine.
_ Study Area and Methods
| We observed the two broods in two Beaver (Castor
| canadensis) flowages (Snake Flowage, 44°37'N, 68°06’;
| BFA Flowage, 44° 39'N, 68°07'W) that were 20 km
, northwest of Cherryfield, Maine, in township T10 SD,
_ a forested area that has negligible acid-neutralizing
capacity and low nutrients in wetlands (Norton 1980).
We obtained morphometric and water chemistry char-
acteristics of wetlands by methods of McAuley and
Longcore (1988). We mapped and classified (Cowardin
et al. 1979) both wetlands, and we sampled inverte-
brates in one (Snake Flowage), as part of related field-
work (J. R. Longcore, unpublished data). All obser-
vations of broods followed the survey protocol of
Longcore and Ringelman (1980). Morning visits on
wetlands began 0.5 hour before sunrise and lasted two
hours; the 2-h evening visit ended 20.5 hour after
sunset. Broods were always sought on both wetlands
simultaneously, and observers scanned wetlands with
binoculars (7x50) and spotting scopes (20-60x) from
elevated (4-5 m high) platforms. We backdated brood
age (Gollop and Marshall 1954*) to determine approx-
imate dates that first eggs were laid.
Results
During 3 June — 12 July 1982. we observed two
American Black Duck broods that were twice (20 and
18-22 ducklings) the size of average broods. Each
brood was seen three times. Both broods were seen on
the same wetland on the same day (8 June) by DGM.
Both broods were observed on 12 July during the even-
130
Table 1. Characteristics of the two brood-rearing wetlands
with the large American Black Duck broods in Cherryfield,
Maine, 1982.
Variable Snake Flowage BFA Flowage
Wetland System, Palustrine, Palustrine,
Class Forested Wetland Forested Wetland
Basin area (ha) 4.9 4.5
Surface water area (ha) 4.9 3.4
% Submergents 10 78
% Emergents 28 DD,
% Flooded timber 4] 78
pH (in situ) Sy) 6.13
Alkalinity (ueq L"') 58.8 83.0
Conductivity (uS cm!) 24.0 23.0
Calcium (eq L"') 59.4 VS
Phosphorus (ug L”') 70 170
Color (Hazen units) 170 150
ing visit, each by a different observer on a different
wetland, thereby corroborating that two different broods
existed as first identified by plumage characteristics
(Gollop and Marshall 1954*). The brood of 20 dec-
lined to 15 (75% survival) and the brood of 18-22
declined to 16 (73 or 89% survival) at Class II size
near fledging. The features of the two wetlands are
described by the variables in Table 1. We sampled
invertebrates in Snake Flowage, which contained the
highest (P < 0.0001) number of aquatic Insecta per
sample (mean = 257) compared with nine other wet-
lands sampled in the area (J. R. Longcore, unpub-
lished data).
Discussion
At Moosehorn National Wildlife Refuge, Maine,
and at Lake Dalhousie, Nova Scotia (J. R. Longcore,
unpublished data), we have observed Class II Amer-
ican Black Duck broods of 10 ducklings, which are
near mean clutch size. The two large broods,
however, were twice the clutch size (mean +1 SD) of
American Black Ducks in Maine (10.4 +1.3), in
Vermont (9.6 +1.8; Coulter and Miller 1968), in
Maryland (9.1 +1.8; Stotts and Davis 1960), or in
Quebec (9.2 + 1.7; Reed 1970). Other studies of
American Black Ducks have reported large clutches
but rarely as large as the broods we observed. Reed
(1970) reported sizes of mostly first clutches during
12-25 April, as 13, 14, 15, and 17 eggs in Quebec.
Both Coulter and Miller (1968) and Stotts and Davis
(1960) reported clutch sizes of 14 or 15 eggs, and
Krementz et al. (1991) reported that in 1982
American Black Ducks nesting on islands in
Chesapeake Bay averaged 10.2 + 3.0 eggs per clutch,
ranging from 7-20 eggs, but it was unknown whether
large clutches were from one female.
For our two wetlands adequate food seemed avail-
able for females to lay large clutches because the
highest mean number of invertebrates per sweep net
THE CANADIAN FIELD-NATURALIST
Vol. 118
sample was from Snake Flowage among 10 wetlands
sampled (J. R. Longcore, unpublished data). By back-
dating clutches we determined that these females, if
they laid the entire clutch, wouid have initiated egg
laying about 7 and 14 April, similar to early egg dates
of 1-10 April for Maine and Vermont (Coulter and
Miller 1968). Although ducks may adjust clutch size
to environmental conditions (Skutch 1967), if these
two females had laid 20 to 22 eggs per clutch, mass
of the clutch would have been 1248 — 1373 g (62.4 g/
egg x 20 or 22 eggs), which would have equaled or
exceeded mass of a female and been >2 times the
average mass of a usual clutch (mean = 580.3 g,
Arnold 1988). Therefore, it is possible that each female
produced the entire clutch for these large broods, but
it seems improbable.
The possibility of intra-specific pre-HBA (hatch
brood amalgamation) is supported by Stotts and Davis
(1960) who reported two instances of American Black
Duck females laying eggs in the nest of another fe-
male. They (Stotts and Davis 1960: 145) also com-
mented that “Eleven others [clutches] may have been
the result of similar parasitism (a total prevalence of
1.8 percent). An example of inter-specific pre-HBA
also was recorded by Stotts and Davis (1960) who
documented that an American Black Duck female
began laying in a Mallard (Anas platyrhynchos) nest
that contained five eggs. The Mallard laid four more
eggs before deserting, but the American Black Duck
laid 11 eggs to equal a 20-egg mixed clutch. Also,
they reported that two American Black Duck females
nested within 46 cm of each other on an offshore
duck blind in Chesapeake Bay, Maryland; one female
gradually incorporated the other’s clutch into her
own and incubated all eggs (Stotts and Davis 1960:
142). Large clutches associated with ducks nesting
on islands, however, may be related to high nest
density (i.e., 25.2 — 35.7 nests/ha on Bodkin Island,
Chesapeake Bay, Krementz et al. 1991); but is uncom-
mon elsewhere (e.g., 0.06 — 0.12 nest/ha in Maine
bogs (Coulter and Miller 1968: 35). Because nest
sites are not limiting in Maine or across the breeding
range, nesting females are widely dispersed, except
on islands (Coulter and Miller 1968), nests are well
hidden (Bent 1923), and females are secretive when
returning to nests in twilight hours (J. R. Longcore,
unpublished data), it seems improbable that our large
broods resulted from intra-specific pre-HBA (Beau-
champ 1997). The third explanation for the large broods
is intra-specific post-HBA. For this scenario, two addi-
tional clutches of 10-12 eggs must have hatched at the
same time and ducklings in those broods were then
acquired by the females that we observed. We know
that two other American Black Duck broods (i.e., of
five and 10 ducklings) used Snake Flowage at the same
time as the large broods. To account for this scenario
of post-HBA, six American Black Duck broods of
similar age must have been associated with these two
wetlands. Concentration of broods on high quality
2004
wetlands is common (Longcore et al. 1998); indeed
these two wetlands also supported one Green-winged
Teal (Anas crecca), three Wood Duck (Aix sponsa),
and four Hooded Merganser (Lophodytes cucullatus)
broods. For the 20-duckling brood, JRL recorded on
24 June that some ducklings appeared to be in different
age Classes (i.e, I[b and IIc), which suggests post-HBA;
however, the duckling brood of 18-22 appeared as all
the same age to DGM. The two brood-rearing females
were large, extremely attentive, and especially adept in
eliciting rapid responses from ducklings by uttering a
few low calls. Although females are capable of laying
large clutches and the remote possibility of nest para-
sitism (pre-HBA) exists, we conclude that the most
plausible explanation for these two large broods was
intra-specific post-HBA.
Acknowledgments
We thank P. E. Malicky for assistance during brood
surveys and J. M. Eadie, T. W. Arnold, and A. J.
Erskine for review and helpful suggestions on drafts
of the manuscript.
Documents Cited (* marked in text)
Gollop, J. B., and W. H. Marshall. 1954. A guide for aging
duck broods in the field. Mississippi Flyway Council
Technical Report, Minneapolis, Minnesota. 14 pages.
Literature Cited
Arnold, T. W. 1988. Life histories of North American game
birds: a reanalysis. Canadian Journal of Zoology 66: 1906-
1912.
Beauchamp, G. 1997. Determinants of intraspecific brood
amalgamation in waterfowl. Auk 114: 11-21.
Bent, A. C. 1923. Life histories of North American Wild
Fowl. Order Anseres (Part). Smithsonian Institution, U.S.
National Museum, Government Printing Office, Washing-
ton, D.C.
Coulter, M. W., and W. R. Miller. 1968. Nesting biology of
Black Ducks and Mallards in northern New England. Ver-
mont Fish and Game Department Bulletin 68-2. 74 pages.
Cowardin, L. M., V. Carter, F. C. Golet, and E. T. LaRoe.
1979. Classification of wetlands and deepwater habitats
of the United States. U.S. Fish and Wildlife Service, FWS/
OBS-79/31. 103 pages.
NOTES 13]
Eadie, J. McA., F. P. Kehoe, and T. D. Nudds. 1988. Pre-
hatch and post-hatch brood amalgamation in North Ameri-
can Anatidae: a review of hypotheses. Canadian Journal
of Zoology 6: 1709-1721.
Krementz, D. G., V. D. Stotts, D. B. Stotts, J. E. Hines, and
S. L. Funderburk. 1991. Historical changes in laying
date, clutch size, and nest success of American black
ducks. Journal of Wildlife Management 55: 462-466.
Longcore, J. R., and J. R. Ringelman. 1980. Factors affect-
ing waterfowl breeding density and productivity estimates
in the northeast. Transactions of the Northeast Section,
The Wildlife Society 37: 169-181.
Longcore, J. R., D. A. Clugston, and D. G. McAuley. 1998.
Brood size of sympatric American black ducks and mal-
lards in Maine. Journal of Wildlife Management 62: 142-
151.
McAuley, D. G., and J. R. Longcore. 1988. Survival of juve-
nile Ring-necked Ducks on wetlands of different pH. Jour-
nal of Wildlife Management 52: 169-176.
Norton, S. A. 1980. Geological factors controlling the sen-
sitivity of aquatic ecosystems to acid precipitation. Pages
521-531 in Atmospheric sulfur deposition, environmental
impact and health effects: Proceedings of the Second
Life Sciences Symposium, Potential Environmental and
Health Consequences of Atmospheric Sulfur Deposition,
Gatlinburg, TN, October 14-18, 1979. Edited by D. S.
Shriner, C. R. Richmond, and S. E. Lindberg. Ann Arbor
Science Publishing, Ann Arbor, Michigan.
Reed, A. 1970. The breeding ecology of the Black Duck in
the St. Lawrence estuary. Ph.D. dissertation, Laval Uni-
versity, Quebec, Canada. 175 pages.
Skutch, A. F. 1967. Adaptive limitation of the reproductive
rate of birds. Ibis 109: 579-599.
Stotts, V. D., and D. E. Davis. 1960. The Black Duck in the
Chesapeake Bay of Maryland: breeding behavior and
biology. Chesapeake Science 1: 127-154.
Tufts, R. W. 1986. Birds of Nova Scotia. Third Edition.
Nimbus Publishing and Nova Scotia Museum, Halifax,
Nova Scotia.
Zammuto, R. M. 1986. Life histories of birds: clutch size,
longevity, and body mass among North American game
birds. Canadian Journal of Zoology 64: 2739-2749.
Received 28 February 2002
Accepted 15 June 2004
132 THE CANADIAN FIELD-NATURALIST Vol. 118
Observations of Interactions between Puma, Puma concolor, and
Introduced European Red Deer, Cervus elaphus, in Patagonia
WERNER T. FLUECK
CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnoldégicas), Postal address: DeerLab, C.C. 176, 8400
Bariloche, Argentina; e-mail: deerlab@infovia.com.ar
Flueck, Werner T. 2004. Observations of interactions between Puma, Puma concolor, and introduced European Red Deer,
Cervus elaphus, in Patagonia. Canadian Field-Naturalist 118(1): 132-134.
Direct observations of interactions between native Puma (Puma concolor) and introduced European Red Deer (Cervus elaphus)
in Patagonia are discussed with respect to the absence of evolutionary sympatry. Although the founding stock of European
Red Deer had been lacking natural predation pressure for considerable time due to the previous extinction of large predators,
these observations suggested that inherent antipredator behavior of European Red Deer toward this novel predator, once
detected, was effective and may partially explain the success of European Red Deer as an invasive species. Puma behavior
supported the view that they are a generalist predator which opportunistically utilizes new prey species like European Red Deer.
Key Words: European Red Deer, Cervus elaphus, Puma, Puma concolor, introduced species, predation, behavior, interaction,
Argentina.
The role of large predators in regulating northern
cervids continues to be debated. This function of large
predators has to be viewed from a historical-evolu-
tionary angle; how predators affect prey populations
in modern human-modified settings can be expected to
differ greatly (Berger 1998; Flueck 2000). The evolu-
tion of large predators appears to be a systemic func-
tional response as shown by re-evolving ecomorphs
among very distant taxonomic groups. Furthermore,
ecologically complete northern systems had several
predator species with different hunting strategies and
several prey species which thus prevented coevolution
(Flueck 2000). Parts of Patagonia represent a natural
experiment in south-temperate Argentina where Euro-
pean Red Deer (Cervus elaphus elaphus) were intro-
duced during the 1920s (Flueck and Smith-Flueck
1993) to areas with native Puma (Puma concolor). As
the Puma has only occurred in the Americas, these two
species have no evolutionary history of sympatry. Fur-
thermore, the native large predators had been extinct
for a considerable time in areas of Europe where the
European Red Deer originated, and immediate memory
of such predators was thus absent.
Hornocker’s (1970) work showed that direct obser-
vations of attempts by Puma to capture prey was near-
ly impossible and very few reports have been made
previously, mostly stories by hunters (see Robinette
et al. 1959). A few additional accounts are based on
interpretation of tracks in the snow (Robinette et al.
1959). During many years of studying Puma, Seiden-
sticker et al. (1973: 31) never observed Mule Deer
(Odocoileus hemionus) or American Elk (Cervus ela-
phus nelsoni) mobbing a Puma, and I found no refer-
ence to a cervid fighting off a Puma successfully. Here
I report on direct observations of interactions between
Puma and European Red Deer.
Study Area
The study area is in the western foothill portion of the
province of Neuquén, Argentina (40°58'S, 71°12'W).
The topography is primarily mountainous with most
features formed by glacial processes. The dominant
climate is temperate with main precipitation occur-
ring between April and September. There is an abrupt
precipitational gradient from west to east due to the
rain shadow effect of the Andes which results in a
strongly defined vegetation structure and floristic com-
position. The study site is between 900 and 1200 m
elevation and represents the ecotone between forest
and steppe. Patches of forests are characterized by
“Nire” trees (Nothofagus antarctica) and “Ciprés”
(Austrocedrus chilensis) at lower elevations and are re-
placed by “Lenga” trees (Nothofagus pumilio) at high-
er elevations. Forest patches at lower elevations alter-
nate with wet grasslands (“mallines”) with abundant
growth of herbaceous plants, whereas at high elevation
they are replaced by grass-dominated steppe of “Coirén
Amargo” (Stipa speciosa var. major) and “Coirén Dul-
ce” (Festuca pallescens), with variable occurrence of
brush species like “Neneo” (Mulinum spinosum),
“Calafate” (Berberis spp.) and “Espino Negro” (Colle-
tia spinosissima). Riparian areas also contain galleries
of small trees like “Radal” (Lomatia hirsuta), “Maitén”
trees (Maytenus boaria) and “Laura” (Schinus pata-
gonicus).
Methods and Results
Observations of interactions between European Red
Deer and Puma were recorded while stalking alone
during field work to collect deer for reproductive stud-
ies. Here I report on two such incidents.
On 10 November 1999 at 20:15 h I was returning
to camp at a pace faster than stalking as it was getting
2004
late and the deer had not yet descended into the flat
open feeding areas below surrounding hills which
they use for cover during midday hours. The area I tra-
versed was semi-open with patches of grassland inter-
spersed with some patches of trees like Laura, Radal,
and Cypress, typical of the acetone here. There were
also patches of brush, predominantly Espino Negro
and Calafate. As I was about to pass a stand of Radal,
which was approximately 10 m in diameter, I heard the
alarm bark of a European Red Deer cow about 20 m
away coming from within the stand. I stopped imme-
diately, believing that she must have seen me through
the Radal trees, particularly as the same had happened
only a short while earlier with a cow which was bed-
ded in a similar tree patch. I thus waited in antici-
pation that this animal might step out of the trees in
curiosity, in which case I would have collected her as
well. Looking with binoculars, I could see her move
behind the trees and affirmed that she had not yet left.
Suddenly, she barked again and came charging to-
ward me through the patch of trees. Once she was in
sight, I saw that she was pursuing an adult Puma, and
it was clear that the barking was aimed at the predator
and not at me. The Puma stopped shortly after get-
ting out into the open, but as the cow came charging
again, the Puma took off and the cow chased the cat
around a circular patch of Espino Negro of about 7 m
in diameter and | m in height. The fast chase took the
animals around this bush patch twice, until the Puma
apparently stopped out of sight behind the bush. The
cow then stopped in front of it and commenced bark-
ing again. Finally the cow trotted back toward the patch
of trees on the same path where she had come from,
only to turn around suddenly and charge toward the
patch of bush, stamping in front of it and barking con-
tinuously. Four times she repeated this behavioral pat-
tern of trotting away and turning back, but when she
finally reduced her aggressiveness and appeared about
to retreat, I got ready to collect her. As she turned to
enter the trees and was obviously walking away from
the scene, I shot, which caused her to run through the
tree patch on the same path on which she had origi-
nally come out.
After picking up my gear, I came around a bush
and went towards the trees. Immediately, I saw the
Puma jump out of a tree behind that patch of bush,
and follow the deer on the same path through the trees.
I then entered the tree patch, having to hunch down
to pass through the trail. As I reached the other side,
still in a hunched position, I saw the head of a Puma
appear at about 15 m from behind a patch of bunch
grass; it must have heard me coming through the trees.
Looking through the binoculars, I determined it was
a cub of the previous year. Still looking through my
binoculars, I saw the head of the mother Puma pop
up, and without hesitating she approached me to with-
in 10 m. Apparently this was the first she knew of my
presence and she began to snarl, which could be
NOTES
133
clearly heard. After 30 seconds of staring straight at me,
she sat down, but kept looking directly at me and snarl-
ing periodically. She then appeared to relax in the sense
that she would start to look from side to side, blink-
ing slowly, and she was no longer in an alert position.
As the sun had set and I needed to collect infor-
mation on the cow before dark, I decided after about
5 minutes to move on ahead. I stood up which im-
mediately put the Puma into alert mode. She stood
up, started to snarl continuously and stared at me. As
I made a first few steps towards her, it became clear
that she would rather move back than hold her posi-
tion, so I continued to move forward. She retreated as
much as I would move forward. Approximately 5 m
out into the open, I could again see the cub which
immediately retreated into the brush upon seeing me.
At 15 m from the trees I found the dead cow, while
the female Puma stood 10 m away still snarling. As I
started to make brisker movements, like taking off
the backpack, she retreated farther away and out of
sight behind the brush. The thorax of the European
Red Deer had already been torn open by the Puma.
The European Red Deer cow was of average body
size for this region (Flueck, unpublished data), except
girth (116 cm) which was 10% below average. She
had absolutely no fat reserves (sternum, rump, omen-
tum, kidney). This was probably due to extreme drought
conditions during spring through fall of 1999. Body
conditions in fall of 1999 were so low that only 56%
of adult females conceived (Flueck 2001) as compared
to 100% in previous years. This 14-year-old female
had given birth to a calf 1-2 days earlier as evidenced
by the still enlarged uterus and the large but hard
udder. Furthermore, in the trees I found remains of a
calf which had been partially scavenged at least a day
earlier; cause of death could not be determined.
The second observation occurred on 17 November
1996, while I was stalking in an area of hilly grassland
interspersed with brush. At 18:15 h, I heard a Euro-
pean Red Deer cow bark on the other side of a canyon
and shortly after, I observed her running nervously
back and forth in a semi circle at a patch of Espino
Negro brush, about 5x10 m in area and | m tall.
Then a calf cried and approximately 5 minutes later
cried again. It was obvious that the female had a prob-
lem with the calf. Shortly after, | saw an animal body
appear from behind the brush patch and enter it. A
few minutes later, the female stopped barking and
trotted away down the hill. I then went to the spot and
as I slowly approached the brush about where the ani-
mal had entered earlier, an adult Puma fled crossing
the brush patch. Right at the edge was a dead calf
which was barely eaten. The Puma had dragged it from
some distance when crossing the brush patch. The calf,
a male, had body measurements indicating it weighed
11 to 12 kg (Flueck, unpublished data), and several
features indicating it was only a few days old (first
incisors were out only 4 mm; umbilical scab).
134
Discussion
Puma in Patagonia are large predators and compar-
able to or surpass the largest races known from the
nearctic (Iriarte et al. 1990). Franklin et al. (1999)
reported average weights for female and male Pata-
gonian Puma as 47.5 and 75.8 kg, respectively. Female
Puma are known to increase their kill rate several
fold when accompanied by cubs and can be expected
to increase their aggressiveness. It is thus of interest
that a European Red Deer female at the energetically
most stressful period right after birthing coupled with
nutritional stress from the drought was able to chase a
female Puma which had young, up a tree. It indicates
that the defense behavior of European Red Deer
towards a discovered novel predator like Puma was
effective in preventing the death of the mother. In the
first case, the cause of the earlier death of the calf is
unknown, and as it is common for a cow to remain in
the vicinity of a recently born calf after it dies, it ex-
plains the aggressive behavior toward the Puma which
likely could have prevented predation on the offspring.
In the second case, the mother could not prevent pre-
dation of her calf by Puma; however, the learning event
might enhance the probability that a future offspring
might survive. Innate antipredator behavior of intro-
duced European Red Deer therefore, appears success-
ful in assuring adequate numbers of offspring to
survive against the native Puma hunting strategy. The
loss of exposure to large predators for the founding
stock in their original habitat did not prevent the estab-
lishment of the founding populations in Patagonia,
indicating that rapid learning to defend against Puma
must have occurred. Other cervids had become naive
to their large predators which became locally extinct,
but adapted quickly once these predators reappeared.
This was clearly shown for Roe Deer (Capreolus
capreolus), when Lynx (Lynx lynx) were reintroduced
(Breitenmoser and Haller 1993), and Moose (Alces
alces) with offspring after reestablishment of Wolves
(Cants lupus) and Bears (Ursus arctos) (Berger et al.
2001).
On a larger scale, it is also clear that Puma in Pata-
gonia, as the major predator of introduced European
Red Deer, are not able to prevent them from increas-
ing numerically (Flueck et al. 2003). Furthermore, as
Puma and deer occur across extensive landscapes with
no human-related mortality factors for Puma, I pos-
tulate that intrinsic mechanisms are responsible for
preventing Puma populations from reaching densities
where they would exert a control over the deer popu-
lations (Flueck 2000). Puma prey frequently on Euro-
pean Red Deer indicating their generalistic and oppor-
tunistic feeding behavior. Although about 80% of the
natural mortality of adult female deer was due to Puma,
annual survival rate of these deer remained high at
91% (Flueck et al. 2004).
THE CANADIAN FIELD-NATURALIST
Vol. 118
These observations support existing studies that the
Puma behaves as a generalist predator which can oppor-
tunistically adapt to new prey species. Furthermore,
they demonstrate that European Red Deer have an
ample repertoire of innate antipredator behavior which
may partially account for their success as an invasive
species.
Acknowledgments
I am grateful for the cooperation received from var-
ious landowners and the Administracion de Parques
Nacionales de Argentina. Thanks also to J. Smith-Flueck
and P. S. Gibson for useful comments on the manu-
script.
Literature Cited
Berger J. 1998. Future prey: some consequences of the loss
and restoration of large carnivores. Pages 80-100 in
Behavioral Ecology and Conservation Biology. Edited by
T. Caro. Oxford University Press, Oxford, England.
Berger, J., J. E. Swenson, and I. L. Persson. 2001. Recol-
onizing carnivores and naive prey conservation lessons
from Pleistocene extinctions. Science 291: 1036-1039.
Breitenmoser, U., and H. Haller. 1993. Patterns of predation
by reintroduced European lynx in the Swiss Alps. Journal
of Wildlife Management 57: 135-144.
Flueck, W. T., and J. M. Smith-Flueck. 1993. Uber das in
Argentinien angesiedelte Rotwild (Cervus elaphus, L.,
1758): Verbreitung und Tendenzen. Zeitschrift fiir Jag-
dwissenschaft 39: 153-160.
Flueck, W. T. 2000. Population regulation in large northern
herbivores: evolution, thermodynamics, and large predators.
European Journal of Wildlife Research 46: 139-166.
Flueck, W. T. 2001. Pregnancy rates of introduced red deer in
Patagonia, Argentina after a period of drought. Ecologia
Austral (Argentina) 11: 17-24.
Flueck W. T., J. M. Smith-Flueck, and C. M. Naumann.
2003. The current distribution of red deer (Cervus elaphus)
in southern Latin America. European Journal of Wildlife
Research 49(2): 112-119.
Flueck, W. T., J. M. Smith-Flueck, and N. A. Bonino. In press.
A preliminary analysis of cause-specific and capture-relat-
ed mortality, and survival of adult red deer in northwestern
Patagonia. Ecologia Austral.
Franklin, W. L., W. A. Johnson, R. J. Sarno, and J. A.
Iriarte. 1999. Ecology of the Patagonia puma Felis con-
color patagonica in southern Chile. Biological Conser-
vation 90: 33-40.
Hornocker, M. G. 1970. An analysis of mountain lion preda-
tion upon mule deer and elk in the Idaho primitive area.
Wildlife Monographs 21: 1-39.
Iriarte J. A., W. L. Franklin, W. E. Johnson, and K. H.
Redford. 1990. Biogeographic variation of food habits and
body size of the American puma. Oecologia 85: 185-190.
Robinette, W. L., J. S. Gashwiler, and O. W. Morris. 1959.
Food habits of the cougar in Utah and Nevada. Journal of
Wildlife Management 23: 261-273.
Seidensticker, J. C., M. G. Hornocker, W. V. Wiles, and J.
P. Messick. 1973. Mountain lion social organization in
the Idaho primitive area. Wildlife Monographs 35: 1-60.
Received | September 2000
Accepted 4 June 2004
2004 NOTES 135
Premieres mentions de la Couleuvre mince, Thamnophis sauritus
septentrionalis, au Québec
JEAN-FRANCOIS DESROCHES! et RICHARD LAPARE*
'Collége de Sherbrooke, Département des Techniques d’écologie appliquée, 475 du Parc, Sherbrooke (Québec),
J1K 4K1 Canada
2Ministére des Transports du Québec, Direction de Laval-Mille-fles, 1725 boulevard Le Corbusier, Laval
(Québec), H7S 2K7 Canada
Desroches, Jean-Francois, et Richard Laparé. 2004. Premiéres mentions de la Couleuvre mince, Thamnophis
sauritus septentrionalis, au Québec. Canadian Field-Naturalist 118(1): 135-137.
Deux Couleuvres minces, Thamnophis sauritus septentrionalis, ont été trouvées les 12 et 13 aoat 2003, dans le
comté de Pontiac en Outaouais, au Québec. II s’agit des premieres mentions de cette espéce dans la province.
Des détails concernant les spécimens trouvés et les habitats sont présentés, de méme qu’une breve discussion
sur la présence de cette espece au Québec. Trois autres Couleuvres minces ont été trouvées en 2004, dans le
méme secteur, le méme qu’une autre a I’ fle-du-Grand-Calumet, a environ 30 km au nord-ouest.
Two Ribbonsnakes, Thamnophis sauritus septentrionalis, were found on 12 and 13 of August 2003, in Pontiac
County, Outaouais region, in Québec. These are the first records of the species for the province. Details on the
specimens and habitats in which they were found are presented, as well as a brief discussion on the presence
of Ribbonsnakes in Québec. Three additional Ribbonsnakes were found in 2004, in the same area, and another
one on Ile-du-Grand-Calumet, about 30 km northwest.
Mots-Clés : Couleuvre mince, Thamnophis sauritus septentrionalis, aire de distribution, premieré mention,
habitat, Québec.
Key Words: Northern Ribbon Snake, Thamnophis sauritus septentrioncilus, distribution, first record, habitat,
Québec.
La Couleuvre mince (Thamnophis sauritus) est pré-
sente dans une grande partie de l’est de 1’ Amérique
du Nord, de la Floride jusqu’en Ontario (Conant et
Collins 1998). Au Canada, elle est représentée par la
sous-espéce T. s. septentrionalis, laquelle se rencontre
dans le sud de l’Ontario et sous forme de population
disjointe en Nouvelle-Ecosse (Cook 1984). Malgré
sa répartition limitrophe au Québec, cette couleuvre
n’avait jamais été rapportée dans cette province. 7! s.
septentrionalis mesure au plus 96,5 cm a l’age adulte
et ressemble a premiére vue a la Couleuvre rayée de
Pest (Thamnophis sirtalis sirtalis), présentant comme
celle-ci un corps foncé marqué de trois rayures longi-
tudinales généralement jaunes. On distingue la Cou-
leuvre mince de la Couleuvre rayée par la position de
ses rayures latérales, situées sur les 3*°™° et 4°™° ran-
gées d’écailles du corps, son corps plus élancé et sa
queue comparativement plus longue, et l’écaille pale
bien définie devant chaque ceil (Cook 1984). La colora-
tion des flancs, sous les rayures latérales, est souvent
marron. La Couleuvre mince est considérée menacée
en Nouvelle-Ecosse et en situation préoccupante en
Ontario (COSEPAC 2002*), tandis que la Couleuvre
rayée est tres commune dans ces provinces tout comme
au Québec.
Les 12 et 13 aoat 2003, dans le cadre d’un travail
d’inventaire faunique effectué par le Ministére des
Transports du Québec, dans un secteur circonscrit du
comté de Pontiac, en Outaouais, nous avons décou-
vert deux spécimens de la Couleuvre mince. Dans les
deux cas les couleuvres se trouvaient sur une route de
sable et de gravier et ont été apercues a partir d’un
véhicule en mouvement. Le temps était ensoleillé et
chaud, avoisinant les 30° Celsius.
Le premier spécimen de la Couleuvre mince a été
observé le 12 aoat a 18h10, sur le chemin Bristol
Mines, a 1,2 km a l’ouest de la jonction avec le che-
min Pontiac Station (45°29'29"N; 76°20'12"O), a
environ 2 km au nord de la riviére des Outaouais. Il
s’agissait d’un adulte mort écrasé, mesurant 57,6 cm
du museau au cloaque, pour une longueur totale (in-
cluant la queue) de 80,9 cm. Malgré que la couleuvre
semblait avoir été tuée plusieurs heures auparavant, il
a été facile de l’identifier par la position des rayures
latérales et la couleur marron des flancs. Le second
individu a été trouvé le 13 aodt a 16h53, sur un
chemin reliant les immenses tas de débris miniers a
la riviére des Outaouais (45°28'38"N; 76°20'15"O), a
environ | km au nord de cette riviére. C’était un sub-
adulte mesurant 29,7 cm du museau au cloaque, pour
une longueur totale (incluant la queue) de 45,5 cm.
Ce spécimen était vivant et 4 découvert sur le che-
min. Des photographies des deux Couleuvres minces
ont été prises par les auteurs. Les spécimens ont été
déposés au Musée canadien de la nature (CMNAR
35485, 35486).
136
L’habitat ot furent trouvées les Couleuvres minces
est majoritairement forestier avec présence de milieux
humides. Dans le premier cas, il s’agit dune forét
mélangée a dominance de feuillus, ou poussent Acer
rubrum, Populus grandidentata, Populus tremuloides,
Fraxinus sp. et Thuja occidentalis. En bordure nord
du chemin se trouve un étang 4 Quenouilles (Typha
sp.) dense d’environ 250 m de longueur par 20 m de
largeur. Dans le second cas, il s’agit d’une forét hu-
mide a dominance de feuillus. On y trouve Betula
papyrifera, Prunus sp., Acer rubrum, Populus balsa-
mifera, Larix laricina, Fraxinus sp. et Alnus incana
ssp. rugosa. A 40 m au nord, de chaque cété du ch-
emin, un marécage est adjacent a la route. On y retrou-
ve des arbres morts en milieu inondé. Des recherches
effectuées dans les habitats avoisinants n’ ont pas per-
mis d’observer d’autres Couleuvres minces. Quatre
Couleuvres rayées de l’est, soit deux vivantes et deux
mortes, ont été observées sur la route durant I’ inven-
taire.
En 2004, trois (3) autres Couleuvres minces adultes
ont pu étre observées dans le méme secteur, qui couvre
18 km?, et une (1) autre sur I’ Ile-du-Grand-Calumet,
a quelque 30 km au nord-ouest. La premiere a été
trouvée le 9 juin en bordure d’un étang a quenouilles
pres d’un chemin de terre (45°29'10"N; 76°20'56"0).
La seconde a été observée le 14 juin dans une flaque
d’eau en asséchement, bordée de saules (Salix sp.), a
10 m de la forét (45°29'40"N; 76°22'00"0). La troisiéme
a été vue le 12 juillet sur une hutte de Castors (Castor
canadensis) (45°31'51"N; 76°18'43"0). Le spécimen
de I’[le-du-Grand-Calumet a été trouvé le 11 aofit sure
une hutte de Castors (45°41'12"N; 76°38'31"0). Des
photographies des Couleuvres minces ont été prises
par l’un des auteurs (JED).
La présence de la Couleuvre mince au Québec n’est
pas surprenante puisqu’on la retrouve en Ontario a
proximité, de l’autre c6té de la riviére des Outaouais
(Tobias et Evans 1979; Cook 1981; Oldham et Weller
2000*). Il est plut6t curieux qu’elle n’ait pas été
rapportée plus tot dans la province. II s’agit bien sir
d’une région peu habitée et sous-inventoriée par les
biologistes, mais plusieurs inventaires spécifiques y ont
été réalisés notamment pour les tortues. Il apparait pos-
sible que sa ressemblance avec la Couleuvre rayée de
Vest, tres commune dans la région, ait contribué a la
garder dans |’anonymat durant toute cette période.
La Couleuvre mince devient donc la 38'*™° espéce
de l’herpétofaune au Québec et la 8°™° en ce qui con-
cerne les couleuvres. La liste des couleuvres du Qué-
bec comportait sept (7) espéces depuis 1927, année ot
la Couleuvre brune (Storeria dekayi) fut découverte a
Montréal (voir les données détaillées dans : Bider et
Matte 1991). Les additions récentes a l’herpétofaune
québécoise concernent les autres groupes (anoures,
urodéles et tortues). Ce sont la Salamandre sombre
des montagnes (Desmognathus ochrophaeus), décou-
verte au Québec en 1988 (Alvo et Bonin 2003), la
THE CANADIAN FIELD-NATURALIST
Vol. 118
Tortue musquée (Sternotherus odoratus) en 1989
(Chabot et St-Hilaire 1991) et la Rainette faux-grillon
boréale (Pseudacris maculata) en 1991 (Bider et Matte
1994). L’addition de la Couleuvre mince a la liste des
reptiles du Québec revét une importance particuliére
puisqu’il s’agit sans aucun doute d’une espéece trés rare
dans la province et qu’elle est déja considérée en situa-
tion précaire en Ontario et menacée en Nouvelle-Ecosse.
Des inventaires supplémentaires seront nécessaires afin
de préciser sa répartition et son statut au Québec. Fi-
nalement, cette couleuvre vient probablement clore
la liste de ’herpétofaune du Québec, si l’on se fie a
la répartition actuellement connue des espéces.
Remerciements
Nous tenons a remercier le Ministére des Transports
du Québec, et plus particulierement M. Ahmed Kho-
dari, chef de service du Service des inventaires et du
Plan, Direction régionale de |’Outaouais, pour avoir
permis la réalisation de l’inventaire faunique au cours
duquel les mentions de Couleuvres minces ont pu étre
faites. Nous remercions également MM. Daniel St-
Hilaire et Michel Lalancette, de la Société de la faune
et des parcs du Québec, pour le prét des cartes topo-
graphiques. Les spécimens de 2004 ont été trouvés par
Mathieu Ouellette, Josiane Bergeron, Louis-Philippe
Gagnon et Benoit Rivard.
Documents cités (identifiés par * dans le texte)
COSEPAC. 2002. Comité sur la situation des espéces en péril
au Canada. http://www.cosepac.gc.ca/index.htm.
Oldham, M. J., et W. F. Weller. 2000. Ontario Herpe-
tofaunal Atlas. Natural Heritage Information Centre,
Ontario Ministry of Natural Resources. http://www.
mnr.gov.on.ca/MNR/nhic/herps/ohs.html (a jour le 09-
11-2002).
Littérature citée
Alvo, R., et J. Bonin. 2003. Rapport sur la situation de la
Salamandre sombre des montagnes (Desmognathus och-
rophaeus) au Québec. Société de la faune et des parcs du
Québec, Direction du développement de la faune. Québec.
32 pages.
Bider, J. R., et S. Matte. (Compilé par). 1991. Atlas des
amphibiens et reptiles du Québec 1988-1989-1990, ver-
sion détaillée. Société d’histoire naturelle de la vallée du
Saint-Laurent et ministére du Loisir, de la Chasse et de la
Péche du Québec. Québec. 429 pages.
Bider, J.-R., et S. Matte. 1994. Atlas des amphibiens et rep-
tiles du Québec. Société d’ histoire naturelle de la vallée du
Saint-Laurent et ministére de l’Environnement et de la
Faune du Québec, Direction de la faune et des habitats.
Québec. 106 pages.
Chabot, J., et D. St-Hilaire. 1991. Premiére mention de la
Tortue musquée, Sternotherus odoratus, au Québec. Cana-
dian Field-Naturalist 105 : 411-412.
Conant, R., et J. T. Collins. 1998. A Field Guide to Rep-
tiles and Amphibians of Eastern and Central North Ameri-
ca. Third edition, expanded. The Peterson Field Guide
Series. Houghton Mifflin Company, Boston. 616 pages.
2004
Cook, F. R. 1981. Amphibians and reptiles of the Ottawa
District. Trail & Landscape 15 : 75-109.
Cook, F. R. 1984. Introduction aux Amphibiens et Reptiles du
Canada. Musée national des sciences naturelles et Musées
nationaux du Canada. Ottawa, Canada. 211 pages.
Desroches, J.-F., et David Rodrigue. 2004. Amphibiens et
reptiles du Québec et des Maritimes. Editions Michel
Quintin, Waterloo, Québec. 288 pages.
NOTES
137
Revisée 16 Aott 2004.
Tobias, T. N., et R. E. Evans. 1979. Range extension of the
Ribbon Snake in Ontario. Trail & Landscape 13 : 180-181.
Re¢u 20 aout 2003
Acceptée 27 fevrier 2004
Book Reviews
ZOOLOGY
Amphibian Decline: An Integrated Analysis of Multiple Stressor Effects
Edited by Greg Linder, Sherry K. Krest, Donald W. Sparling.
2003. SETAC North America, 1010 North 12th Avenue,
Pensacola, Florida 32501-3367 USA. xxi + 345 pages.
U.S.$98 Cloth.
This volume contains presentations at the Workshop
on the Global Decline of Amphibian Populations
sponsored jointly by the Society of Environmental
Toxicology and Chemistry (SETAC) and The Johnson
Foundation 1-23 August 2001 at Racine, Wisconsin.
Fifteen papers are included as 10 chapters, one with
A-B and another with A-E designations for no appar-
ent reason.
Canadian data and perspective on the problem of
declines are not neglected. Of the 35 contributing
authors listed, 31 are from the United States but four
are Canadian: Christine Bishop (Canadian Wildlife
Service, Delta, British Columbia), David Cunnington
(“freelance”’, Victoria, British Columbia), Martin
Ouellet (Redpath Museum, McGill University, Mon-
treal, Quebec), Bruce D. Pauli (Canadian Wildlife Ser-
vice, Hull, Quebec). Ouellet is one of nine coauthors
of Chapter 6 “Biotic Factors in Amphibian Population
Declines”, and Bishop, Cunnington, and Pauli are half
of the six coauthors of Chapter 7 “Physical Habitat
and Its Alteration: A Common Ground for Exposure
to Environmental Stressors”.
None of the individual chapters is a particularly easy
read and their results or conclusions often are neither
clear-cut nor universal in their application. However,
collectively, they effectively and repeatedly bring out
the complications in separating climatic, chemical pol-
Birds of Africa: From Seabirds to Seed-eaters
By Chris and Tilde Stuart. 1999. MIT Press, Five Cambridge
Center, Cambridge, Massachusetts, USA. 176 pages. U.S.
$29.95 Cloth.
This is an attractive book that appears to be in-
tended as a typical “coffee table” volume. It is large
in size (22 x 28 cm). profusely illustrated and very
well laid out, with between 2 and 9 illustrations on
each two-page spread. The plates themselves range
from full page to quite tiny (under 4 cm’).
The text is presented in 12 chapters plus an intro-
duction, species list, and index. Each chapter is devoted
to a group of bird families with some feature in com-
mon. Thus we have “Birds of the Oceans’, “Birds of
Inland Waters and the Coastline”, “LBJS”, and so on.
Chapters then deal with each family in turn (grouped
lutant, and biotic pressures, many of which doubtlessly
combine to produce documented or supposed losses
or declines. The texts are heavily laden with flow and
modelling in 18 figure diagrams, 18 tables, 5 matrices
and even two “test boxes” to visually present concepts
and consequences. Each chapter has its own biblio-
graphy.
The concluding summary chapter effectively stresses
the continuing, unresolved nature of the problems, but,
in an inevitable rather self-congratulatory manner,
arrives at the conclusion that this workshop was vital
to promoting a much-needed exchange of expertise on
various aspects of real and potential amphibian dec-
lines and that it has created a network for further
discussion and exchange. Although one could argue
that this was happening anyway, the workshop did
usefully focus discussions and the book spreads the
state of knowledge. It is useful both for what research
has been done and for what future approaches might be
productive. One can hardly disagree with the funda-
mental conclusion that further sharing of information
as it develops will be essential to adequately defining
future measures. If, eventually, there ever will be effec-
tive conservation of the world amphibian fauna it will
depend on a better understanding of the causes and
reality of the declines.
FRANCIS R. COOK
Canadian Museum of Nature, Ottawa, Ontario KOG 1RO
Canada
in the sequence of their common names), giving the
number of species that occur in Africa together with a
brief account of the family characteristics, and some-
thing about a sampling of the species. Occasionally
there are boxes which treat a particular topic in some
detail; for example, “The Dilemma of Island Birds”.
The main body of the text enlivens the chronicle of
numbers and species descriptions by concentrating on
interesting anecdotes and “gee whiz” facts about the
species under discussion. The authors are African and
obviously have had considerable experience with the
continent’s bird life. On the whole their statements
seem accurate, although I was unable to check some
of them, but some are incorrect. For example, Great
Skua does not breed in the Southern Hemisphere, Kelp
138
2004
Gull is not an African endemic, and the Australian
Ibis is not conspecific with the Sacred Ibis.
For me this book has some rather irritating problems
that in sum seriously detract from its interest. Overall
there is a lack of cohesion, mainly resulting from the
organization of the text. The arbitrary chapter group-
ings inevitably run into families that do not quite fit
the category, or fit into more than one. I would be in-
clined to place gulls and terns in the coastal waterbird
chapter, lots of the “Seed-eaters” are classic LBJ’s,
and “Terrestrial Birds” results in a strange collection
of species with Pittas following Ostrich. This is ac-
centuated by the layout within the chapters, with (for
example) “Avocets and Stilts” at the beginning of
Chapter 3, “Oystercatchers” and “Plovers and lap-
wings” in the middle separated by Pelicans, and the
“Waders or shorebirds” at the end. True, the system-
atic list at the end is in order, but this does little to
balance the sense of randomness that one gets from
the text itself.
Probably the authors would point out approaches
of this kind are not unusual for books of the genre:
they are not, after all, basic reference texts. Unfortu-
nately, attractive though the layout is, there are prob-
lems with the plates as well. In many cases the tinier
The Firefly Encyclopedia of Birds
Edited by Christopher Perrins. 2003. Firefly Books Ltd.,
3680 Victoria Park Avenue, Toronto, Ontario M2H 3K1
Canada. 656 pages. U.S.$59.95.
Naturalists across the continent strive to ever in-
crease their knowledge of local wildlife, and all love
to hear about wildlife from other localities. Birdwat-
chers, for example, can become very knowledgeable
about their local species, and the zealous ones will
even study species from other areas within the same
country, continent or even from around the world.
But the vast array of bird species is overwhelming,
and it takes a serious encyclopedia to pull them all
together. Luckily for us, The Firefly Encyclopedia of
Birds edited by Christopher Perrins is just what we
needed — a good collection of text and photos of the
birds of the world all in one volume. Nicely present-
ed with tons of sharp photos illustrating everything
from specific behaviours to simply jaw-dropping “‘cool-
ness” (including several underwater pictures such as
common murres on page 280-281, common kingfisher
on page 368, and American dipper on page 521), the
book is backed up by solid text summarizing well the
basic tenets of ornithology. Moreover, each chapter
BooK REVIEWS
eo)
illustrations are difficult to see properly, many of the
poses are poor, and the selection of subjects pictured
leaves something to be desired. Opening the book at
random I find pp. 130-1 show two different pictures
of Arrow-marked Babblers, one of the Southern Pied
Babbler, and one of a Wallcreeper. The latter only
occurs as a vagrant in North Africa, and the plate
shows little of this species’ remarkable wing pattern,
so it simply looks like a gray bird. Africa does have a
creeper species, and the text on these pages also in-
cludes the broadbills (Eurylaimidae). These species
are not illustrated at all.
In summary, this book brings together a large num-
ber of photographs of African birds, some of them
very good, together with a compilation of interesting
facts and anecdotes on African bird families. My
quarrels with content are really irrelevant if this is all
you are looking for, or if you find this book attractive
enough in itself to buy. Those who desire a thorough
overview of the African avifauna should look else-
where.
CLIVE E. GOODWIN
1 Queen Street, Suite 405, Cobourg, Ontario K9A 1M8
Canada
focuses on a bird family (the large number of species
precludes a species-by-species analysis), and is accom-
panied by a “factfile”. This sidebar summary provides
a general description of size and habits, as well as a
broad distribution map and my favorite, a visual com-
parison of bird size to a human.
The book also details several interesting specific
behaviors, such as pigeon homing (pages 294-295), or
the nest parasitism of Cuckoos (pages 316-317), but
nothing on the degredation of the tundra by Snow
Geese, a topic of high importance and actuality in
North America. It also discusses extinct birds such as
the Elephant Bird (page 21), the Dodo (page 291),
and a short paragraph on the Passenger Pigeon (page
293). The book provides a fantastic introduction to
birds from all around the world, is extremely well
presented, very reasonably priced ($75.00 CAN,
hardbound), and constitutes a worthy, if not essential,
addition to the library of all bird enthusiasts.
SERGE LARIVIERE
226 Rang Bois-Joly, St-Apollinaire, Québec GOS 2E0, Canada
140
Birds of Belize
By H. Lee Jones. 2004. University of Texas Press, P.O. Box
7819, Austin, Texas 78713-7819 USA. x + 444 pages.
U.S.$60.00 Cloth, U.S.$34.95 paperback.
This first edition covers the 574 species of birds
recorded in the old British colony of Honduras, and
now called Belize. Virtually all the birds are shown
in colour plates, with accompanying text and 234
range maps. The book has a brief introduction to the
biogeography and climate of Belize and a how-to-
use chapter. This latter is very important because it
explains how the author has chosen to organize the
book and select the “common” names, as well as the
names in Maya, Spanish and the aboriginal language.
The range maps, at the back of the book, mostly cover
the resident species and are large enough to be a
useful guide.
The text is precise and clear and contains much
useful information. For example, the call of the North-
ern Potoo is described in terms that should enable
anyone to recognize it. This is the key characteristic
in separating the Common from the Northern Potoo.
Another good example is the description of the Double-
toothed kites, explaining the “Distinctive puffy white
undertail coverts that spread to the sides of the rump
.... This is a very good field character and this
description captures it well.
The artwork is by Dana Gardiner, the same artist
that illustrated the Birds of Costa Rica by Stiles and
Skutch. I found his style a little stiff, giving the birds
a flat appearance and missing something of their jizz.
These new renderings, while similar to those in Birds
of Costa Rica, are an improvement. The Wedge-billed
Woodcreeper illustration more clearly depicts its re-
markable tail. The Emerald Toucanet is the correct
subspecies, Aulacorhynchus prasinus prasinus, show-
ing a white throat. However, I did have difficulties
Herpetology: Third Edition
By F. Harvey Pough, Robin M. Andrews, John E. Cadle,
Martha L. Crump, Alan H. Savitsky and Kentwood D.
Wells. 2004. Pearson Prentice Hall, Upper Saddle River,
New Jersey, USA. ix + 726 pages. U.S.$93.
In the preface to this edition of Herpetology, the
authors state, “understanding amphibians and reptiles
as organisms requires a perspective that integrates
their morphology, physiology, behavior, and ecology
and places that information in a phylogenetic context.”
The authors have done a commendable job at fulfill-
ing this daunting task.
The text book is divided into four parts and each
part is subdivided into chapters. Part one (What are
amphibians and reptiles?) explores the field of her-
petology, the place of amphibians and reptiles in ver-
tebrate evolution, systematics and diversity of amphib-
ians and reptiles, and biogeography. Part two (How do
THE CANADIAN FIELD-NATURALIST
Vol. 118
with some plates, but I think this relates more to the
printing than the artwork. For example, the depiction
of Cedar Waxwing is far too intense and the elaenias
are much too dark. The depiction of the Violet Sab-
rewing is deep blue. I have never seen one in the field
that did not look violet (as described accurately in
the text and depicted accurately in Birds of Costa
Rica) under any light conditions. In particular I
checked the depictions of Scaly-breasted Humming-
bird (poorly done in Birds of Costa Rica) and it is
better, but I still think a novice would have trouble in
the field using the plate for identification purposes.
The nomenclature is fairly standard. The author
retains Rock Dove for Columba livia (instead of the
new “Rock Pigeon” — thereby reducing confusion
with the orange-brown Rock Pigeon of South Africa,
Columba guinea). | had to use the scientific name of
Phaethornis longirostris to be sure the author’s Long-
billed Hermit was the same as Stiles and Skutch’s
(Western) Long-tailed Hermit. I am still confused as to
the status and distribution of Passerini’s and Cherrie’s
Tanager (a recent split of Scarlet-rumped Tanager).
Only Paserrini’s Tanager is listed for Belize, which I
believe is correct.
This guide is just under 6” x 9” x 1.25” (15 x 22 x
3 cm) and is too large for the average pocket. Al-
though I have some reservations, | still think this book
will make a useful field guide, especially if you use
the text in conjunction with the plates. This book rep-
resents a good stride forward in literature for this
section of the Americas. If it is to be used in the field
I would be tempted to take along a Mexican guide as
a second reference.
Roy JOHN
2193 Emard Crescent, Beacon Hill North, Ottawa, Ontario,
K1J 6K5 Canada
they work?) has chapters on temperature, energetics,
reproduction, locomotion and feeding. Part three (What
do they do?) covers movements, communication, mat-
ing systems, diets and species assemblages. The fourth
part (What are their prospects for survival?) discuss-
es conservation of amphibians and reptiles in a single
chapter.
How does this edition differ from previous editions?
The second edition was published in 2001 and hence
this edition includes many references to recent pub-
lications. There is also a greater emphasis on phylo-
genetic analyses, particularly in the early chapters on
systematics. This edition also features colour photo-
graphs and colour distribution maps for the families
of amphibians and reptiles. The colour maps do not
really add much, but the colour photographs are effec-
tive. A chapter on biogeography is one of the biggest
2004
changes in content in this edition. The authors have
also wisely split the chapter on reproduction into two
chapters, one each for amphibians and reptiles. The
section on conservation has also been expanded, re-
flecting the growing concern over many species in
both groups.
It is hard to find much wrong with this exhaustive
examination of the current state of herpetology. The
one conspicuous absence is a glossary, something that
would surely be important in any comprehensive text-
book such as this. Overall, the combined talents of
Lizards: Windows to the Evolution of Diversity
By Eric R. Pianka and Laurie J. Vitt. 2003. University of Cali-
fornia Press, 2120 Berkeley Way, Berkeley, California,
USA. xii + 333 pages. U.S.$45 Cloth.
Individually, each author of this volume has more
than 30 years of lizard study in various areas of the
world. These include the southwestern (both) and
southeastern (Vitt) United States, as well as Africa and
Australia (Pianka) and Central and South America
(Vitt). Each has included a personalized capsule bio-
graphy of his background and interests, each empha-
sizing what first attracted him to lizards.
This book is number 5 in the University of Califor-
nia Press series Organisms and Environments. The
introduction explains that it grew from a resolve by
authors 10 years ago. At that time, while working on
a third lizard ecology symposium volume, they envi-
sioned production of a comprehensive semi-popular
book on the group. In a review of the earlier work,
the 1994 Lizard Ecology: Historical and Experimental
Perspectives, Robert W. Murphy (1995. The Canadian
Field-Naturalist 109(1): 135-136), while generally
praising its standards of “highest academic acumen”,
thought it “not necessarily well suited for bedside
reading by the merely curious. And it will not make a
good coffee table book as there are no high-gloss
photographs”.
The latter criticism has been particularly well res-
ponded to in the new volume. It is not only coffee-
table size in design (28.6 x 22.5 cm) but has the req-
uisite high-gloss photographs scattered throughout.
These, often emphasizing activity or displays, splen-
didly illustrate the diversity of behaviour as well as
form and pattern for a well-chosen variety of lizards.
There are also a scattering of graphs, tables, diagrams,
and maps to illustrate particular points. Included are
evolutionary relationships between groups of lizards,
biotic and abiotic factors affecting a lizard’s well-
being, avenue of heat gain and loss for a diurnal bask-
ing lizard, comparison of mean percent use of the
seven most important prey categories by neotropical
and desert lizards, prey size vs lizard size, independent
evolution of body type in Jamaica and Puerto Rico,
and population size for species of land iguanas on
islands of the Caribbean, to choose a few at random.
Book REVIEWS 14]
six experts with diverse research interests is hard to
beat. After two previous editions, the authors have
resolved most of the inevitable errors and contradic-
tions resulting from integrating the writing of so many
people. It is hard to imagine a better single volume
overview of these fascinating creatures.
DAVID SEBURN
Seburn Ecological Services, 920 Mussell Road, RR 1, Oxford
Mills, Ontario KOG 1S0 Canada
The introduction raises the question: “what good
are lizards?” This is first summarily dismissed with a
curt retort, emphasizing the authors’ abhorrence of
anthropocentrism, “what good are people?”. Subse-
quently, the instructive value of lizards in relation to
the ecosystem is attributed to their multitude of forms
and the variety of habitats they have successfully
occupied. They can thus effectively serve as “model”
organisms for broad understanding of ecology and
the diversity of animal life, a theme also emphasized
in the earlier symposium volumes.
Following the introduction are three major parts
with seven, six, and two sections: (1) Lizard Life-
styles: Evolutionary history and phylogeny, Getting
around in a complex world, Lizards as predators, Es-
caping predators, Social behavior, Reproduction and
life history, and Reflections of a real world; (2) Liz-
ard Diversity: Iguanians, From Geckos to Blind Liz-
ards, From Racerunners to Night Lizards, Skinks, From
Girdled Lizards to Knob-scaled Lizards, Monsters and
Dragons of the Lizard World; (3) Synthesis: Historical
perspective, Lizards and humans. In the initial section
it is pointed out that as a group “lizards” is para-
phyletic due to excluding the snakes. The latter are
omitted as they traditionally have been treated as a
separate equal group, though now recognized in con-
temporary clarification as just an offshot within vara-
noid lizards (as shown in Figure 1.4, page 16).
The major partitions are followed by a four-page
Taxonomic Summary (with number of species in each
family or subfamily (if it has been subdivided) listing
all included genera). The species totals are given (by
major subdivisions) as [guania 1340+; Scleroglossa:
Gekkota 973+, Incertae sedis 151+; Autarchoglossa
(excluding snakes but inclusive of Scincomorpha:
Lacertoidea, Scincoidea: Anguimorpha [including
Varoidea]) 1745+; or collectively over 4200. The book
concludes with a three-page Glossary (abiotic to zygo-
dactyly), an 18-page references section, and a nine-
page index.
Throughout, the book is a pleasant mix of formal
and informal styles. Scientific discussions have shuffled
among them separate blocks of personal observations,
often field experiences of one or the other author. As
stated (page 7) “Throughout this book, we continu-
142
ally return to questions we asked as children in an
attempt to encourage readers to open their minds and
to ask questions”. This responds splendidly to the ear-
lier reviewer’s wish for a text “well suited for bed-
side reading by the merely curious”. Unfortunately,
the large coffee table format and the glossy reflective
pages make it awkward to handle in bed and read by
bedside light. But as an up-to date comprehensive
survey of world lizards it has no equal. It provides
Raptors of Western North America
Brian K. Wheeler. Princeton University Press, 41 William
Street, Princeton, New Jersey 08540-5237 USA. 544 pages,
625 colour photographs, 56 maps, U.S.$49.50 Cloth
This book is both a tour de force and a labour of
love, and the immediate new standard for diurnal
raptors in western North America. Raptors are known
for their variable plumages, and standard field guides
cannot cover the almost infinite permutations and com-
binations; hence, erroneous identifications are legion
among regular birders, and even among raptor enthu-
siasts. No full-time museum, government or university
employee has dared to undertake a book of this scope;
it is all the more astounding that this hiatus was filled
by a truck driver. More incredibly, Wheeler has devel-
oped the skills to take the great majority of the pho-
tographs himself. His experience and enthusiasm are
evident throughout. He has reviewed the literature
carefully and has been given access to unpublished
information from graduate students and others; for
example, numbers of Northern Goshawk and Bald
Eagle territories are provided for each state. There are
nearly two pages about the ten-year cycle of the Snow-
shoe Hare and Northern Goshawk, absent from most
other raptor books; goshawks peaked at Duluth, Min-
nesota, during the irruption years of 1972, 1982, 1992
and 2001, mostly adults fleeing the mixed forest fol-
lowing each Snowshoe Hare crash.
Excellent historical accounts include notably that for
the California Condor. There are four excellent glos-
saries: general, anatomy and feather, plumage and molt,
and displays. The detailed descriptions of raptor plu-
mages are unprecedented and unequalled. Fortunately,
important points are highlighted in bold, making the
tedious mass of description more user-friendly.
Readers will be amazed by the remarkable variabil-
ity of plumage in species such as the Ferruginous
Hawk (25 photos), Rough-legged Hawk (39 photos),
and Swainson’s Hawk (40 photos), and especially the
Red-tailed Hawk; variants within the latter species are
depicted in 82 photographs, 22 pages of verbal des-
cription and six maps.
THE CANADIAN FIELD-NATURALIST
Vol. 118
great perspective of their global importance, a fact
strictly Canadian naturalists, who have only six spe-
cies belonging three families of non-snake lizards to
observe in their entire country, have little first-hand
chance to appreciate.
FRANCIS R. COOK
Canadian Museum of Nature, Ottawa, Ontario K1P 6P4
Canada
John Economidy has contributed clear, accurate
range maps for 33 species, six for the Red-tailed Hawk
alone. The maps are incredibly precise, but I noticed
four minor errors for Saskatchewan species: the Big
Muddy area of Saskatchewan is omitted from the
Golden Eagle; the two southern year-round localities
for Bald Eagle should be winter only; recent small
southerly extensions of Osprey and Northern Goshawk
ranges are not shown; the two races of the Merlin are
not known to overlap between Saskatoon and Prince
Albert. The maps also give no indication of range
changes in the past.
Since this veritable encyclopaedia of western raptors
(an eastern counterpart became available simultane-
ously) is too heavy for most backpacks and too large
for most glove compartments, most of us will use it
as a reference in our libraries. One hesitates to quibble
about the first edition of such a superb book. Yet the
title is misleading, since owls are not included; inclu-
sion of the term “diurnal” would have made the title
more accurate. The ground squirrel has not lost half
its range in western Canada, as it has in Idaho (page
521). Use of dieldrin, not DDT, was coincident with
the early 1960s crash of the Merlin on the Canadian
prairies (page 447). Use of “very uncommon” some-
times contradicts his definitions in the introduction. I
detected few errors, but “verses” in place of “versus”
jarred me (page 199). Wheeler has been involved in
two previous hawk identification books, each excel-
lent, each with William S. Clark as co-author. The
first was Hawks in the Peterson Field Guide series and
the second, A Photographic Guide to North American
Raptors. For most general birders, either would suffice,
although many plumages are omitted from both of the
smaller books. If you are a raptor aficionado, don’t
let the cost of the new book deter you; the 603 colour
photographs easily justify the price and the 33 colour
maps are more detailed than anything previously
available.
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N OJ8,
Canada
I
2004
Raptors of Eastern North America
By B. Wheeler. 2002. Princeton University Press, 41 Williams
Street, Princeton, New Jersey, USA. xv + 439 pages,
U.S.$45.00 Cloth
Let me begin by saying this is a wonderful book. It
gives a very detailed account of all the 26 full species
of hawks, eagles and falcons occurring in eastern North
America. It is profusely illustrated with extremely good,
frame-filling, crisply focused photographs. These range
from nine photographs for the Short-tailed Hawk to
an incredible 82 of the Red-tailed Hawk. The text, des-
pite its somewhat clipped English, is very informative.
All of the known and recognizable sub-species are
included, both in the text and, where valid, in the
photographs. The level of detail given in the plumage
descriptions is far greater than in any other book I
have read. The range maps are sized as appropriate to
the species they cover. For widespread birds the map
depicts all of eastern North America. However, larger
scale maps are used for such localized birds as Flor-
ida’s Snail Kite.
This is easily the best photographic-style guide I
have seen and is a real testament to the author’s dedi-
cation. Thus it is the most thorough guide to this group
of North American birds you can purchase. The full-
color, superb photographs alone are worth the price
of the book. The author has included all the plumages,
races, and colour variations possible. They cover a
bewildering range of plumages for species that can
be annoyingly difficult to identify in the field. This
makes it an almost essential book for serious bird-
watchers and ornithologists and a great resource for
beginners trying to grapple with the plumage variabil-
ity. I do not consider this book to be a portable field
guide, but a reference work. It is a little too large and
Turtles and Tortoises
By Vincenzo Ferri. 2002. Firefly Books Ltd., 3680 Victoria
Park Avenue, Toronto, Ontario M2H 3K1 Canada. 255
pages. $24.95
This compact little book is a translation of the 1999
Italian publication, Tutto Tartarughe e Testuggini. It
can best be thought of as a photographic guide to 152
species of turtles — roughly half of the species alive
today.
The book opens with an introduction covering the
biology, evolution, classification and conservation of
turtles. The bulk of the book is occupied by species
accounts. The species accounts are grouped geograph-
ically into oceans (sea turtles) and six terrestrial areas:
Palearctic, Afrotropical, Oriental, Nearctic, Neotropical
and Australian regions. There are 152 numbered spe-
cies accounts and additional unnumbered accounts
sprinkled throughout the book. It is unclear why some
species accounts are not numbered, although the un-
numbered accounts do not have a colour photo (they
BOOK REVIEWS 143
heavy (due to the thick, high-quality paper). More
important, this would be too precious a book to risk
damaging in the field.
I searched through for errors and did not notice any.
In fact, I was impressed by the thoroughness of the
coverage. For example, the author has correctly includ-
ed the spotty northern locations for Osprey in Lab-
rador.
However, I do have one major problem with this vol-
ume. It is a companion volume to Raptors of Western
North America, a slightly larger book covering 33
species. Thus, there are 23 species common to each
book. The species accounts and photograph are almost
identical, except that the range maps are different. This
means there is a good deal of unnecessary repetition.
I can only assume that some marketing guru felt that
two versions would sell better than one. Combining
into one book would increase the size from 544 to
about 600 pages to allow for the text for two addition-
al species and the eastern range maps for all species
(plus a little added to the index.). This would presum-
ably increase the price to around U.S.$60. Each book
is a worthwhile purchase on its own. If you buy the
western book you will miss the accounts for Snail Kite
only. If you buy the eastern guide you will lose the
accounts for nine western raptors. If you buy both you
will get more than 75% repetition, in essence wasting
U.S.$30, to get the coverage of one extra species plus
the relevant range maps. If you can afford only one
book, buy the western guide.
Roy JOHN
2193 Emard Crescent, Beacon Hill North, Ottawa, Ontario,
K1J 6K5 Canada
do have a colour illustration) or map. The species ac-
counts are brief (some less than 100 words), with most
ranging from half a page to a full page in length. Each
account has standardized subheadings: Family, Distri-
bution and habitat, and Characteristics. Some of the
accounts also have a “Situation” subheading describing
conservation issues.
Perhaps because it is a translation, this book is
plagued with errors. Translation-type errors include
some unusual common names. For example, the Bog
Turtle (Clemmys muhlenbergii; now Glyptemys muh-
lenbergii) is called Muhlenberg’s Turtle. That may well
be the English equivalent of the Italian common name,
but that term is not used in North America. Similarly,
the Painted Turtle (Chrysemys picta) is referred to as
the Painted Tortoise. In addition, the genus is mis-
spelled “Chrysemis.” Errors in content also abound.
The author asserts that Eunotosaurus is the earliest
known ancestor of turtles, yet this theory is no longer
144
widely accepted. It is also stated that some turtles can
hibernate for 2-3 months, a gross understatement of
the 6+ months that some turtles spend in hibernation.
The species accounts are also fraught with errors
or misleading information. For some North American
species, the author lists individual U.S. states where
the species is present, yet the list is rarely complete.
The Blanding’s Turtle (Emydoidea blandingii) account
omits any mention in the text or the map of the Nova
Scotia population. The author accepts the Mississippi
Map Turtle (Graptemys pseudogeographica kohni) as
a species (G. kohni), even though the species account
THE CANADIAN FIELD-NATURALIST
Vol. 118
suggests it is a subspecies. There are also some curi-
ous omissions. There are six species accounts for mem-
bers of the genus Graptemys yet the most wide-ranging
species, the Northern Map Turtle (G. geographica) is
not included. Overall, one has the sense that the text
was assembled quickly, or by using outdated reference
materials, and that it was not reviewed by a scientific
expert. Enjoy the photos but don’t believe everything
you read.
DAvID SEBURN
Seburn Ecological Services, 920 Mussell Road, RR 1, Oxford
Mills, Ontario KOG 1SO Canada
What Good are Bugs? Insects in the Web of Life
By Gilbert Waldbauer. 2003. Harvard University Press, 79
Garden Street, Cambridge, Massachusetts, USA. 384 pages.
U.S'$29295
Waldbauer has written several other popular books
about insects, and these have been met with high
acclaim; I have not read those tomes, and so see his
most recent work with unbiased eyes.
What good are bugs? focuses on the interactions
insects have with other animals and plants, both living
and dead. Several chapters in each category illustrate
the myriad ways in which insects, wittingly or unwit-
tingly, are key to earth’s ecosystems as we know them
today. Topics range from seed dispersal to recycling
dead animals and the control of animal and plant
populations. Truly, the scope of this book is close to
all-encompassing, and is written in a style that will
not be condescending to the informed naturalist or
biologist, but will be readily consumable by the bud-
ding naturalist, too.
There are a few factual problems, as well as some
opinions that are more typical of the entomophobic
component of the public, that were surprising and dis-
appointing to see in a book which promotes insects.
Several times Waldbauer has insects “attacking” plants,
when he really means “feeding on” plants. No one
would ever say that deer or rabbit attack plants, it’s
no different with insects; they are just feeding on the
plants, a point that naturalists, biologists, and surely
this author should understand. “Attacking plants” is
an expression used by certain people or industries to
incite action, to justify eradication, to gain sympathy
from the uninformed, and should itself be eradicated
from our vocabulary.
The book ends with a chapter-by-chapter listing of
selected readings. I like this method of listing refer-
ences since the reader can readily choose among
works only in the topic of interest. Overall, this is a
book well worth having.
RANDY FE. LAUFF
Department of Biology, St. Francis Xavier University,
Antigonish, Nova Scotia B2G 2W5 Canada
Belugas in the North Atlantic and the Russian Arctic
Edited by M.P. Heide-Jorgensen, @.Wiig, and D. G. Pike.
2002. NAMMCO Science Publication 4, The North At-
lantic Marine Mammal Commission, Polar Continental
Centre, N-9296, Tromso, Norway NOK 150. 270 pages.
The greater part of this symposium is devoted to
those beluga whales that migrate through Baffin Bay
and Davis Strait between the eastern part of the
Canadian Arctic and West Greenland, and are difficult
to follow across the deep water (and impossible in
the dark season). Moreover, it is a difficult publica-
tion to review because it represents “work in progress’’,
the results of which are not yet fully understood by
the authors themselves. Three main techniques of study
were (1) mitochondrial molecular genetics from tissue
sampling of restrained or dead animals; (2) aerial pho-
tographic surveys; (3) tracking individuals by means
of satellite radio tags attached to implants in the dorsal
ridge of temporarily trapped belugas. The results are
too tentative to summarize easily. Many groups of bel-
ugas observed in summer in arctic estuaries are essen-
tially matrilines, that is, adult females with young ani-
mals of both sexes, while most adult males may move
independently in different ways. There is also the prac-
tical concern that catches of belugas at southwest Green-
land, where there is most open water and the largest
catching boats, appear to exceed recruitment. The exact
area from which these animals come is unknown.
After this it is a pleasure to move on to simpler
studies! An overall survey of Russian and Siberian
arctic waters from the mainland was carried out in
the course of ice studies for belugas, narwhals and
Greenland or Bowhead whales, plus the few Grey
whales that enter the Arctic Ocean. There is now little
hunting for them in this half of the Arctic.
Lastly, a summary is given of up-to-date knowledge
of the numerical status of belugas that inhabit, year-
round, the less than 200 linear km of the St. Lawrence
2004
estuary in Quebec. This is the most biologically pro-
ductive part because of year-round vertical water mix-
ing. Aerial photographic surveys of numbers are there-
fore simple to carry out, but it is necessary to measure
the percent of animals diving too deeply to be regis-
tered visually or by camera form the air. M. C. S.
Kingsley and team did this using a helicopter hover-
ing at an altitude that did not disturb the animals. The
correction factor turned out to be more than two, so
that estimates of numbers needed to be more than
doubled, giving a total of more than 1200. Moreover,
a series of estimates made since even casual hunting
ended, ca. 1979, up to the last recorded survey in 1998,
showed that the population has been growing slowly.
I add to this review some more recent information that
several belugas, including one radio-tracked animal,
moved in autumn 2002 from SE Hudson Bay to off
The Firefly Encyclopedia of Insects and Spiders
Edited by Christopher O’Toole. 2002. Firefly Books Ltd.,
Willowdale, Ontario
I will first state my biases and say that I’m not a big
fan of encyclopaedias. Having got that out of the way,
I must say this book was engaging, excellently laid out,
and an absolute joy to read. The photographs ranged
from very good to excellent to amazing. The full-frame
images of even small insects startled me with their
clarity. Diagrams were liberally used, effective, and
also of exceedingly high quality. Each chapter was
written by one or more experts, and I enjoyed reading
them all. The majority of insect orders are covered,
as are most of the arachnids (not just the spiders as
the title alludes).
Although this book could not serve as a university
text in entomology, if I were to offer a bug course at
the high school level, I would use this book. I have
seen many entomology texts, and none are as visu-
ally appealing as this book. This book would not sub-
stitute for a field guide because of its size, but the qual-
ity of the text, illustrations and photos far exceeds any
of the field guides I’ve used.
Interspersed with the taxonomic accounts which
dominate the book were photo stories, fact files and
special features. These articles ranged from less than
a page to two pages and provided a different tangent
on insect and arachnid life. As with the rest of this
book, these articles were well done.
BooK REVIEWS
145
Nain, Labrador (D. W. Doidge, personal communi-
cation), showing that therefore some animals “bleed”
from the Arctic into the Labrador Current. These
must be the source of infrequent but not rare animals
which reach the east coast of Newfoundland (Curren
and Lien. 1998. Canadian Field-Naturalist 112(1); 28-
31). These were noted by Kingsley in this book, but
have not been tracked further. Animals coming from
the St. Lawrence estuary are also known to “bleed”
into waters around the Maritime Provinces as far as
the Bay of Fundy and even to New Jersey (various
references). It therefore seems very unlikely that the
St. Lawrence population is isolated genetically from
the main Arctic population of belugas.
D. E. SERGEANT
Box 745, Hudson Heights, Quebec JOP 1JO Canada
The weaknesses were very few. My underlying
feeling was that I couldn’t be certain as to the in-
tended audience. The wording is usually so straight-
forward that children from eight or nine years old
should be able to read it; however, technical ter-
minology creeps in now and again, and would likely
give those same early readers quite a pause. For the
most part, the technical lingo is kept to a minimum,
and is often isolated from the main text in‘ sidebars.
This book is billed as an encyclopaedia, and the
publishers I think were striving to market the book to
a wide audience.
My only quibble about the actual content was that
the minor taxa were mentioned only in a list along-
side the more dominant taxa, and not given their own
words or photographs to describe them. I realize that
no book that features the ricinuleids more than the
beetles will ever sell, especially to the general public,
but a photograph and a quarter page or so of text for
each of these minor taxa would have been appropriate.
Overall though, a great reference book, with won-
derful visual appeal.
RANDY F. LAUFF
Department of Biology, St. Francis Xavier University,
Antigonish, Nova Scotia B2G 2W5 Canada
146
BOTANY
Biotic Forest Communities of Ontario
By Norman Duncan Martin and Norma M. Martin. 2003.
Commonwealth Research. Belleville, Ontario, Canada.
195 pages. $10.00 paper.
Martin and Martin set out to identify the basic for-
est communities of Ontario, describe their biotic com-
position, and consider the successional relationships
among them. While they draw on an impressive amount
of personal research and a broad literature survey, the
book lacks focus and therefore may have a limited
value to a general audience.
A fundamental component of any scientific study
is that the work must be repeatable. When presenting
study results it is therefore essential that the methods
are Clearly laid out. This is not the case here. The read-
er is informed that the authors tallied vegetation in
transects in various types of forest. A single map of
transect locations is provided, with numerous exam-
ples of data sheets. No details are provided to explain
the selection of transect locations nor which aspects
of the vegetation were sampled or how. There is also
no explanation of the analysis itself, other than to
acknowledge the influence of the “schools of inter-
pretation” of Clements, Curtis, Hills, Whittaker and
others. These were indeed important workers in this
field, but listing their names doesn’t allow the reader
to critically examine the results of the current study.
The bulk of the book is devoted to descriptions
and tables illustrating the ten forest community types
identified by the authors. There are interesting obser-
vations here, but the sheer quantity of poorly organized
data makes it difficult to appreciate. Most of the data
is presented as tables showing various measures of
THE CANADIAN FIELD-NATURALIST
Vol. 118
abundance in selected samples. The only graph pre-
pared by the authors is labelled as showing a “dis-
cernable pattern with characteristic variability”. The
discernable patterns are lines overlaid on the plotted
points without any statistical support. This would not
be acceptable in an undergraduate ecology class, let
alone a scholarly thesis.
It is unfortunate that the authors make no reference
to Lee et al. (1998), which has become the standard
forest classification system for Ontario. It may be in-
teresting to contrast the ecological land classification
(ELC) of Lee et al. with Martin and Martin’s forest
communities. If their data could be used to refine or
correct the ELC system it would be far more useful
than it is as a stand-alone study.
The most interesting part of this book is the rela-
tionship between forest types and their fauna. The
authors have collated a great deal of their own data as
well as data from published and unpublished sources.
A more thoughtful analysis of this aspect of their
study might produce a more enduring contribution to
the study of forest ecology in Ontario.
Literature Cited
Lee, H., W. Bakowsky, J. Riley, J. Bowles, M. Puddister, P. Uhlig,
and S. McMurray. 1998. Ecological land classification for
Southern Ontario: first approximation and its application. Ontario
Ministry of Natural Resources, Southcentral Science Section,
Science Development and Transfer Branch. SCSS Field Guide
FG-02.
TYLER SMITH
5900 rue Monkland, Apartment 10, Montreal, Quebec,
H4A 1G1 Canada
Les champignons des arbres de l’est de l’ Amerique du Nord
By Bruno Boulet. 2003. Les Publications du Québec, Sainte-
Foy, Quebec, Canada. 727 pages. $49.95
The author and a number of colleagues have invest-
ed a considerable effort to produce this detailed treatise
on the principal wood-inhabiting fungi (mostly poly-
pores) of eastern North America. The 19 x 24 cm,
hardcover book is heavy but the binding is robust. The
book contains nearly 500 color pictures, typically 6 or
7 on a page, of very good quality.
There are three principal sections. First there is a
brief commentary on the vegetation of Quebec, espe-
cially in relation to the geographic and host distribution
of the wood-inhabiting fungi. Then 118 pages are
devoted to a discussion of the state of our knowledge
of the polypores, including their medicinal properties,
edibility, and traditional and commercial uses. The role
of these fungi as forest pathogens and their influence
on the management of forests are reviewed and various
tree defects caused by these fungi are depicted in color.
The second section of the book introduces the reader
to the taxonomy, nomenclature and classification of
the polypores, as well as their distinctive macroscopic
and microscopic features. The latter are in some in-
stances essential in naming specimens. This section
concludes with an explanation of the most common
means of identifying and naming a specimen, i.e., the
botanical dichotomous key, and a Key including over
400 taxa. About 120 of the 400 are mushrooms that
are briefly described in the key and 76 of them are
shown in a color photo. Many are truly wood-inhab-
iting fungi but a few are mycorrhizal (Lactarius and
Russula) and others are incidental inhabitants of well-
rotted woody debris.
The third and the major part of the book presents
essential information that allows recognition of 169
species, observations on their biology and ecology,
color pictures, and distribution maps. Readers should
be cautious in their interpretation of the distribution
maps because when I compared 8 maps with distri-
butions in two references from the bibliography, 1.e.,
2004
numbers 142 and 145, each map was deficient. Two
specific examples are (1) reference 142, titled Alba-
trellus in Michigan, includes A. caeruleoporus, A.
confluens, A. cristatus and A. peckianus but Michigan
is not shaded on the maps for those species, and (2)
shading on the map for Sistotrema confluens covers
southern Quebec and Nova Scotia but reference 145
notes its presence in those provinces as well as in
Michigan, North Carolina, New Hampshire, New York,
Vermont and Wisconsin.
Two new species, Auricularia americana Parm. et
I. Parm. ex Audet, Boulet et Sirard and Polyporus long-
iporus Audet, Boulet et Sirard, are proposed. Several
species are reported for the first time in North America,
for example, Antrodiella pallasii, Postia alni, P. folli-
culocystidiata, P. ptychogaster, Phellinus cinereus and
Polyporus tubaeformis. Although two names, Postia
minisculoides and P. subpendula, are proposed as new
combinations, if their basionyms, i.e., the initial name
Book REVIEWS
147
given to the fungus and its place of publication, are
not in the book the new combinations are not validly
published. There is a picture (plate 15 D) labeled Punc-
tularia strigosozonata, that shows a typical fruit body
of the orange crust fungus, Phlebia radiata.
The book concludes with a glossary containing ap-
proximately 250 terms with their English equivalent
and a definition that often includes a reference to a
page where the term is used or illustrated, an index of
French and English common names, an index of sci-
entific names, and a bibliography of 450 entries.
The book is recommended to mycologists, forest
pathologists, forest ecologists, and naturalists. It is a
significant contribution to our knowledge of the wood-
inhabiting fungi of eastern North America.
J. GINNS
1970 Sutherland Road, Penticton, British Columbia V2A 8T8
Canada
Manual of Vascular Plants of Northeastern United States and Adjacent Canada: Second Edition
By Henry A. Gleason and Arthur Cronquist. 2004. The New
York Botanical Garden Press, 200th Street and Kazimiroff
Boulevard, Bronx, New York 10458-5126 USA. 993 pages.
U.S.$69.00. Cloth.
The second edition of this most useful flora was
first printed in 1991. Subsequent printings have taken
place in 1993, 1996, 1998, 2000 and 2002. The seventh
printing which has a slightly larger page (15 cm x 23 cm,
rather than 14 cm x 21.5 cm) has a slightly larger type-
face. The text pages have exactly the same page numbers
as the earlier printings. Some corrections were made in
the 1993 volume. In 1999 nineteen individuals con-
tributed numerous corrections but these corrections
could not be included in the 2000 and 2002 printings
without having an electronic version. One was finally
made for the 2004 printing.
This new volume has an interesting but almost hid-
den drawing of a Tulip-tree, Liriodendron tulipifera,
on the front cover. The introductory pages start with a
Table of Contents which includes a list of the families
in taxonomic order with their page numbers. This is
followed by a Foreword by Patricia K. Holmgren and
Noel H. Holmgren and short bibliographies of Henry
Allan Gleason and Arthur Cronquist by Noel H.
Holmgren together with photographs of them. The
Glossary which preceded the synoptic keys in the
earlier printings now follows the main text. This is
followed by the Index to Common Names and the
Index to Scientific Names which in the earlier volumes
were combined.
This new volume is a most welcome step ahead
with the numerous changes and corrections, and The
New York Botanical Garden Press is to be congratulated
even though it is still called the Second Edition.
WILLIAM J. Copy
Biodiversity, National Program on Environmental Health,
Agriculture and Agri-Food Canada, Research Branch, Wm.
Saunders Building, Central Experimental Farm, Ottawa,
Ontario K1A 0C6 Canada
The Wild Orchids of North America, North of Mexico
By P. Martin. 2003. University Press of Florida, 15 Northwest
15th Street, Gainesville, Florida. USA. $27.95 paper,
U.S.$45.95 cloth.
This book is a special version of a check list. The
orchids included are all the recorded species found
above the U.S.—Mexican border north to the Arctic
and Greenland. This covers 223 species plus 24 sub-
species and varieties. Additionally, this takes in 103
growth and color forms, 24 hybrids, and introduced
species. The species are arranged alphabetically by sci-
entific name, so the first entry is the charming little
Spotted Orchid Amerorchis rotundifolia. The author
gives the genus, synonyms, misapplied names, typical
common name, references and range. The author also
adds any appropriate comments. For each species there
is a5 x 7 cm photograph of the flower and a line draw-
ing, generally of the whole plant. In some cases the line
drawing is of the flower only which is a duplication
that does not add information.
In addition to the over 60 species that can be found
in Canada, and the familiar genera (Platanthera,
Cyprepedium etc.), there are several genera that |
normally associate with the tropics (Vanilla, Laelia,
Epidendrum). While many of these are escapees from
cultivation, there are a number that are native species.
Not surprisingly, most of these tropical epiphytes are
to be found in Florida. Indeed, I was surprised to see
148
how many species of Vanilla (of vanilla ice-cream fame
from Vanilla planifolia) that are native to Florida.
The author uses the term “waif” to denote random
individual occurrence. An example of a waif is Laelia
rubescens, first seen in Florida in 1999. This abundant
and attractive Central American species is a popular
garden plant and a likely escapee. The accompanying
photograph shows a white blossom. All the wild L.
rubescens | have seen were pale lavender.
The species coverage and their current status are
both accurate and up-to-date. This book contains the
split between the Spotted Orchid, Cyprepedium gutta-
tum (Alaska and NWT), and the Yellow Spotted Orchid,
C. yatabeanum (Kodiak Island). It includes the New-
foundland orchis (Platanthera albida) of Newfoundland
and Greenland. The book does not contain any habitat
information, nor anything of the plants’ biology. Gen-
erally, nothing is given on abundance and the distribu-
THE CANADIAN FIELD-NATURALIST
Vol. 118
tions are very generic (e.g., Manitoba east to New-
foundland south to Texas and Georgia). It would be
exciting to see an expanded version of this book con-
taining descriptive text on habitat and biology, accom-
panied by useable range maps. This would create an
encyclopedia of North American orchids. In the mean-
time, this book is a very handy reference and will make
a good field guide.
The book’s size precludes it fitting a pocket, but it
will slip easily into your back pack. As well as the
usual glossary and bibliography, the author includes
a well-organized key. This, combined with the clear
format, makes it a no-nonsense, practical guide for
botanists, naturalists and orchid enthusiasts.
Roy JOHN
2193 Emard Crescent, Beacon Hill North, Ottawa, Ontario
K1iJ 6K5 Canada
Trees of the Carolinian Forest: A Guide to Species, Their Ecology and Uses
By Gerry Waldron. Boston Mills Press, 132 Main Street,
Erin, Ontario NOB 1TO Canada. 274 pages. $24.95.
The Carolinian zone of southern Ontario is home to
more than 1600 plant species. It is also the most dense-
ly populated area of the country. As a consequence,
Canada’s most biologically diverse forests are also
among the habitats most threatened by development.
Anyone with an interest in the appreciation and con-
servation of this natural heritage will do well to read
Gerry Waldron’s Trees of the Carolinian forest. Mr.
Waldron has succeeded in producing a beautiful book
that is at once a pleasure to read and quite informa-
tive. The subtitle, “A guide to species, their ecology
and uses” is somewhat misleading — this is much more
than a field guide. Waldron draws on a variety of his-
torical and scientific sources to set the scene: what is
the Carolinian zone? how is it related to other eco-
logical regions? and how have successive human cul-
tures altered this region? With the ecological context
established, Waldron treats each of 73 tree species
not as individuals but as members of a community.
The book starts with an ecological history of the
Carolinian zone, from glaciation through settlement
by indigenous and European humans up to the present.
While far from an presenting an exhaustive review of
post-glacial colonisation, Waldron includes enough
detail to distinguish his treatment from the usual cli-
chéd summary that appears in books of similar scope.
We learn of the massive hemlock dieback 5000 years
back, and that beech was averaging 20 kilometres per
century as it crept north. This is a fascinating subject,
and it’s a shame that Waldron includes no references
to his sources here. While in-text citations would be
overly pedantic, including a few key references such
as Pielou (1991) would be worthwhile.
Waldron uses quotations from the journals of early
settlers and survey crews to illustrate both the appear-
ance of the “virgin” forest and the attitudes of Euro-
peans to their new homeland. Once again, he piqued
my curiosity, but in this case there are perhaps no read-
ily accessible published sources he could refer the
reader to for further information.
A short discussion of the definition of the term
“Carolinian” follows. Waldron covers the topic in five
pages — a clearly presented summary of an important
concept. This is typical of the book as a whole. The
author quite capably distills complex ideas into simple
language, without sacrificing accuracy in the process.
With the context established, Waldron devotes some
forty pages to a discussion of biodiversity, ecological
communities, and our role in their protection, and
especially, their restoration. He obviously brings a lot
of experience to bear on the subject. Most books on
restoration focus on technical details — how, where,
and when to plant a tree, etc. Refreshingly, Waldron
starts by examining why (and why not) to plant trees
as part of a restoration. In a region where restoration
of endangered prairie habitat often begins with the
removal of trees planted as part of misguided natu-
ralization programs, this is an important discussion.
That said, he acknowledges the difficulty in pursuing
a “do-nothing” approach, and offers suggestions for
accelerating natural successional processes. These are
presented as ideas to consider, not as ready-made pre-
scriptions for restoration success.
And so it is that on page 112 of this tree guide that
the actual species treatments begin. Each species is
allotted two pages. This includes the usual description
of their habitat and appearance, with insights into their
use in restoration and urban plantings. Unfortunately,
Waldron has chosen to arrange the species alphabet-
ically by common name. This may simplify things for
the beginner, but it has the unfortunate consequence
of separating walnut (Juglans nigra) from butternut
(Juglans cinerea) and poplar from aspen (both Popu-
2004
lus). Taxonomic arrangements are a very useful tool
for learning about the relationship between species,
but only if we use them!
The book is rounded out with 32 colour plates.
These include a variety of habitat, habit, and close-up
photographs of Carolinian trees. Some of them are
quite instructive, such as the close-ups of the bark
cross-sections of red and white elm, or the collection
of acorns from different oak species. Others are simply
beautiful images of the authors favourite organisms.
One small improvement would be the inclusion of a
scale for the close up shots.
Taken as a whole, this book is an incredible resource
for naturalists in southern Ontario. It will serve equally
ENVIRONMENT
Book REVIEWS
149
well as an introduction to the ecology of the Carolin-
ian forest for the general naturalist and as an idea
book for restorationists and land managers. I look
forward to the publication of a companion volume on
the shrubs of the Carolinian forest, hinted at in the
introduction.
Literature Cited
Pielou, E. C. 1991. After the ice age: the return of life to glaciated
North America. University of Chicago, Chicago.
TYLER SMITH
5900 rue Monkland, Apartment 10, Montreal, Quebec,
H4A 1G1 Canada
Good News for a Change: How Everyday People are Helping the Planet
David Suzuki and Holly Dressel. 2003. Greystone Books,
#201 — 2323 Quebec Street, Vancouver, British Columbia
V5T 4S7 Canada. 399 pages. $24.95, U.S.$16.95
This is a paperback re-issue of Suzuki and Dressel’s
2002 book originally titled Good News for a change:
hope for a troubled planet. Either way, the book is
cleverly titled to attract readers who are tired of doom
and gloom environmental books. The concept is praise-
worthy: bring together in one place success stories of
the many and varied ways people around the world
are changing the way they do things, for the benefit
of their communities, their environment and their
offspring. At the same time, the authors do not shy
away from the bad news. Yes there are wonderful
changes taking place but they are up against very seri-
ous problems and a frightening inertia embedded in
our social and economic systems.
The authors have set a tremendous challenge for
themselves in tackling the full sweep of environmental
problems we face and in trying to represent emerging
solutions from around the planet. They organize this
unwieldy subject thematically with chapters on busi-
ness practices, democracy, biodiversity, water, food,
forests, fisheries, and air pollution. The final chapter
“Breaking out of the Box” addresses the effect of our
global culture on humans as natural beings and the
importance of reconnecting what we do with our deep-
est values. Most chapters focus on one or two case
studies examined in some depth with additional exam-
ples of related projects in other parts of the world.
Examples are drawn from village co-operatives, family-
run businesses, multi-national corporations, farms, in-
digenous societies and non-profit groups from such
diverse places as India, Africa, Germany, Brazil, USA,
Indonesia and many others. Also included are a list
of organizations to contact, detailed endnotes, a brief
bibliography and a reasonably detailed index. The
book is a little lax in explaining the political back-
ground to some of its examples, especially Canadian
ones, and a map plotting the locations for major exam-
ples would have been beneficial.
Throughout Good News there is an admirable effort
to synthesize, and several key themes are followed.
Aligning our activities with natural environmental
systems results in double dividends — the costs are
lower, the benefits are greater and extend beyond eco-
nomics. A resource is used sustainably when it is man-
aged by a stable community that is economically de-
pendent on it and exerts local control and local
ownership. Sustainable practices must be tailored to
the specific situation; the people who follow them are
humble and are constantly learning from their mis-
takes. Many small projects are more effective and more
efficient than a single large one. We are all indigenous
to this planet.
If I have any quibble with this book it is that there
isn’t enough of it. I want to know more about how
Judy Wicks manages to make a living (and a rather
substantial one) running a social activist restaurant. I
want to understand how a small check dam on an in-
termittent stream in India can reverse desertification
caused by forest removal. I want to hear from the
efforts that haven’t worked, because I don’t believe
as easy at the book makes it seem. There is no question
we need more books like this, perhaps ones targeted
at specific issues. Henry Mintzberg (1994) argues for
the importance of identifying “emergent strategies”
(new strategies that emerge spontaneously at any level
of an organization) and helping them spread. That in
essence is what Suzuki and Dressel have done.
Literature Cited:
Mintzberg, H. 1994. The Rise and Fall of Strategic Planning. Free
Press, Simon and Schuster, New York, USA. 454 pages.
CAROLYN SEBURN
Seburn Ecological Services, 920 Mussell Road, RR 1, Oxford
Mills, Ontario KOG 1S0 Canada
150
Whose Bird?
By Bo Boelens and M. Watkins. 2004. Yale University Press,
P.O. Box 209040, New Haven, Connecticutt 06520-9040
USA. x + 400 pages U.S.$35 paper.
Have you ever been curious as to who was the
Bonaparte of Bonaparte’s Gull fame? Was it really
the feared Corsican tyrant? Now you can get a book
that will answer that question and many more. The
authors have researched about 1400 people who have,
at one time or another, given their names to bird spe-
cies. There is a cameo biography for each individual.
As the book gives the accepted English names, there
is a very slight bias to the coverage. European and
American naturalists dominate the list, but to be fair
Professor Ijima (jima’s Warbler, Phylloscopus tjimae)
gets his credit. Montezuma does not fare as well. He
gets a single sentence biography stating he was Em-
peror of the Aztecs. Actually, Montezuma I, Emperor
of Mexico, was a remarkable man. He was a victorious
general before he succeeded his uncle as emperor in
1436. He is only recognized for his Quail, with no
mention of his strikingly handsome Oropendola. In
contrast, Californian Alberto Treganza (Treganza’s —
now Great Blue — Heron) gets almost a whole page.
Many of the names have fallen by the wayside. The
Bancroft’s Night Heron is now called by the more
descriptive name of Yellow-crowned Night Heron. The
loss of some names is. a benefit. | would have trouble
spelling and pronouncing Sjéstedt (Sjostedt’s Owlet,
now Barred Owlet). No disrespect to Mr. Helmut Sick
(Sick’s Manakin), but I think the Golden-crowned
Manikin would prefer its new name. However, I am
sad to see Lear’s Macaw is now an Indigo Macaw.
Edward Lear, mostly known for his nonsense poems,
was a remarkable Victorian bird artist who deserves a
memorial. William MacGillivray’s name lives on as
THE CANADIAN FIELD-NATURALIST
Vol. 118
MacGillivray’s Warbler (Oporornis tolmia) but his
son’s bird, MacGillivray’s Petrel, is now the Fiji Petrel,
but scientifically is Pseudobulwaria macgillivrayi (The
generic name honours the Reverend James Bulwer.).
Some of these names are still current. Thekla Lark,
named after the dying daughter of a German natural-
ist is still a Thekla Lark. Of the 17 species named for
the pioneering Dutch ornithologist Coenraad Temmink,
six still remain. I am delighted that the Adélie Penguin’s
name remains intact as it really suits this charming
bird. Be thankful that Admiral Jules-Sebastien-César
Dumont D’Urville named it for his wife and not
himself.
There are some odd stories in the book. I was par-
ticularly titivated by the tale of Colonel George
Montagu (Montagu’s Harrier) who was cashiered from
the British army for “provocative marital skirmishing”
and thereby took up the study of science. I will never
look at the harrier the same way again!
There are some names that are conspicuously absent.
Roger Tory Peterson, Peter Scott (Scott’s Oriole is
named for Winfield Scott) and James Fisher were
probably born too late in history. Linneus or Linné,
who invented the nomenclature system, was alive in
the right era, but remains un-honoured.
As well as the cameos, the authors have collected
together those people who shared a characteristic in
common, such as diplomats, Germans or those who
died of gunshot. Many of the entries have a black-
and-white portrait of the person featured. For those of
you who love trivia or are keen naturalists preferably
both, this is a fun book.
Roy JOHN
2193 Emard Crescent, Beacon Hill North, Ottawa, Ontario
K1J 6K5 Canada
Forest Dynamics and Disturbance Regimes: Studies from Temperate Evergreen-Deciduous
Forests
By Lee E. Frelich. 2002. Cambridge University Press, 40
West 20th Street, New York, New York 10011-4221 USA.
266 pages. GBP50 (U.S.$80).
Disturbance is ubiquitous in forest ecosystems.
Forested landscapes are best viewed as an integration
of climatic, biotic, edaphic and geomorphic processes
that determine the character of disturbance events
occurring Over a wide range of temporal and spatial
scales. Disturbed by the extremes of either catastroph-
ic, stand-replacing events that may include fire, in-
sect outbreak, and extensive windthrow, or periodic,
small-scale gap processes mediated by fungal patho-
gens, forests are in constant flux when viewed from a
landscape perspective. Such a wide range in the per-
iodicity, intensity and scale of disturbance events,
and the diversity of bio-edaphic interactions create a
complex, fluid, heterogeneous landscape.
Lee Frelich, founder and director of the University
of Minnesota Center for Hardwood Ecology, intro-
duces the reader to the significant disturbances that
have shaped, and continue to shape, the hemlock-
hardwood forests of the northern regions of the Lake
States (Minnesota, Wisconsin, and Michigan). For
the past two decades Dr. Frelich has dedicated himself
to understanding the stand- and forest-level dynamics
of these deciduous-to-boreal transition forests. He
forms part of a long tradition of university and govern-
ment (United States Forest Service) forest ecology
research, much of which is scattered in scientific jour-
nals and government reports. Forest Dynamics and
Disturbance Regimes provides for the first time, in an
engaging, well-illustrated, and synthetic format, the
fruit of this rich research legacy.
2004
“Under what conditions do forests change or stay
the same?” Thus might one summarize the intent of
this book. Introductory chapters set the scene by des-
cribing the Great Lakes temperate forests and their
disturbance regimes dominated by fire, wind, insect
outbreaks and mammalian herbivory. Of significance
to the practicing forest ecologist will be the chapter on
sampling and interpretative techniques used to detect
and interpret forest disturbance regimes. Emphasis is
placed on the use of tree radial increment patterns as
a valuable source of insight into stand disturbance
history.
Frelich emphasizes the critical role played by dis-
turbance in both stand development and forest suc-
cession. He properly distinguishes between stand
development and succession, both of which are often
confused in the literature. Disturbance will always ini-
tiate a new cycle of stand development in the regen-
erating, post-disturbance forest. However, disturbance
may or may not initiate a species change or a new
successional sequence.
Consideration is also given to the differing effects
of disturbance at both the stand- and landscape-level.
This distinction is important, especially given the wide
temporal and spatial scales at which disturbances may
occur. Furthermore, instability at the stand level may
be interpreted as stability at the landscape level. Inter-
pretation often depends on the scale of investigation.
A particular strength of this work is Frelich’s ability
to engage the complex interaction of different distur-
bances. Frelich not only introduces the wide diversity of
temporal and spatial patterns of forest change, but even
more importantly, highlights often counter-intuitive
insights into forest change and continuity. I found the
following particularly noteworthy: (1) the nonlinear
response of forest species composition to disturbance
severity, (2) the cause and development of patchy hard-
wood-softwood mosaics, (3) clarifying taxonomy of the
concept of old-growth, (4) how different forest types
BooK REVIEWS 15]
can exist on relatively homogeneous sites, and (5) the
multiple successional pathways open to any particu-
lar forest type. Frelich’s final chapter summarizes the
notion of forest stability. It provides conceptual models
of forest response to disturbance, 3-D models of suc-
cession in different forest types, and a final classifica-
tion of four different types of forest landscape.
This work is particularly important as humans con-
tinue to “disturb” forests, especially by commercial
forestry. Before any claims can be made about the
desirability of the changes created by human interven-
tions, it is essential to properly comprehend the range
of natural forest disturbance regimes and the associ-
ated changes in forest structure and tree species com-
position.
The book addressees the scientific community and
would properly of greatest interest to forest ecologists
and all students of forest change. The judicious mix
of empirical case studies, hypothetical examples and
conceptual models helps the reader to think “beyond
the box.” The many line drawings, flow charts and
black-and-white photographs help to clarify the dif-
ferent concepts.
As one is reminded in the subtitle, this book focuses
exclusively on the temperate evergreen-deciduous for-
ests (of the Lake States). While it is certain that many
of the concepts developed from research in this forest
type are applicable to other forest types, it is wise to
resist any quick and easy transfer of ideas. Forests grow
in conditions that span a wide ecological spectrum, a
situation that often resists our human tendency to
categorize and classify. Be that as it may, this book
provides rich and substantive insight into this well-
studied — and much-loved — forest region at the decid-
uous-boreal interface.
JOHN McCartny, S.J.
St. Mark’s College, University of British Columbia, 5935
Iona Drive, Vancouver, British Columbia V6T 1J7 Canada
Snowshoes & Spotted Dick; Letters from a Wilderness Dweller
By Chris Czajkowski. 2003. Harbour Publishing Co. Ltd.,
PO Box 219, Madeira Park, British Columbia VON 2HO
Canada. 298 pages. Paper U.S.$24.95
This book is a one-sided account of the wilderness
experiences of a woman of extraordinary independ-
ence, as she writes letters to a friend named Nick.
Chris Czajkowski is an author and wilderness guide
who has chosen a life of relative and geographic iso-
lation on remote property where she lives three quarters
of the year in the coast mountains of British Colum-
bia, 480 kilometres north of Vancouver. There is no
telephone or mail delivery and the radio only works
on clear days. The computer used while writing the
book draws the electricity required to function from
solar panels. The visitors to the eco-tourism business
“Nuk Tessli Alpine Experience” are brought in by float
plane, along with any supplies and news from the
outside world.
This, the fourth book by the same author, is her
account of the incredible effort to build a third cabin on
the property. Its format of letters scribed to a friend in
Germany is generously interspersed with some textual
description, a few black-and-white pictures and hand-
drawn sketches.
The reader is drawn in by expressive language evok-
ing in the imagination pictures of the breathtaking
vistas, and natural surroundings so that you feel almost
as though you have been there, perhaps as a visitor to
“Nuk Tessli”. The added mystery of “what is Spotted
Dick?” is a cute grab but is just a little overdone.
The easy flow of the language makes the 298 pages
an easy read, despite the occasional construction jargon.
sy
The actual process of building a log cabin in the woods,
particularly in such a remote location, is fascinating.
The cabin is built in several steps, over numerous
months, using hand tools, chainsaws, and, occasion-
ally, some friends.
There are a few drawbacks from the enjoyment of
this book though, especially without having read the
first three. The first is that in this book there are a
number of interesting stories that are alluded to but
not told in detail because they’ve been recorded in
the previous books. The second is that the letters are
all to Nick and because it does not include the letters
written from him, it feels a bit like being in the same
room with someone on the phone — you hear half the
conversation and although you get the gist of the
THE CANADIAN FIELD-NATURALIST
Vol. 118
whole, you feel the missing of the other half. The third
and most perplexing is the lack of description of the
characters or their relationship with each other. The
reason this is perplexing is because the author herself
describes this criticism received from a book review-
er — and then simply passes it off with “The trouble
is, I live with the people I write about. Experience
has shown that no matter how innocuous a portrait I
paint, the subject will find something about which he
or she is unhappy.” While I am sure this could be
true, the book would earn a wider audience if it were
not written for those people alone.
DAWN BURNETT
Jacques Whitford Limited, 1 Union Street, Elmira, Ontario
N3B 3J9
Natural Grace: The Charm, Wonder, & Lessons of Pacific Northwest Animals & Plants
By William Dietrich. 2003. University of Washington Press,
1326 Fifth Avenue, Suite 555, Seattle, Washington 98101-
2604 USA. 236 pages. U.S.$19.95
Natural Grace is a contemporary example of the
medieval book of beasts called a bestiary. Bestiaries
were very popular during the Medieval Period, and
focused on the life of nature as a model or paradigm
for human behavior. These books were not scientific
in the contemporary sense of the term, but instead
combined religious and moral teaching with a close
observation of nature, zoological commentaries, and
fabulous and fictitious creatures. Rather than being
studied in and of itself, nature was considered symbol-
ic of both the virtue and moral life of human beings.
While Deitrich’s work certainly provides the reader
with a more sophisticated scientific understanding of
nature, the subtitle of the book betrays its “bestiary”
lineage as the reader is invited to appreciate the charm,
wonder, and lessons of a variety of creatures and
natural phenomena.
This collection of essays is adapted from William
Dietrich’s popular articles in the Seattle Times’ North-
west Magazine. The author divides his work among
four themes: (1) the common and ubiquitous creatures
that we often take for granted, (2) the itty-bitty world
that ranges from soil to spiders, (3) the rhythmic,
clockwork world of tectonics and tides, and finally,
(4) the iconic symbols of the Pacific Northwest includ-
ing, among others, the bald eagle and the killer whale
or orca.
Dietrich is gifted with the contemplative eye. Follow
his gaze and you will enter a world of delight and
amazement. We live side by side with other creatures
and are immersed within the workings of nature. But
often, we are oblivious to the ways of our environs, so
intent and fascinated are we with our own creations
and fabrications. Dietrich pries apart our fabricated
world and invites us to direct our gaze out beyond the
confines of culture. He calls us to a long loving gaze
on the other of nature.
This contemplative gaze is a virtue that strengthens
with time and practice. Dietrich is a patient and humor-
ous guide, gently leading the reader to grow in knowl-
edge of the natural world; knowledge, not simply of
the biological or physical facts, but of the beauty, sig-
nificance, and yes, even mystery inherent in the sub-
ject of our gaze. Of special interest is the manner by
which the author weaves together culture and nature.
Whether it be the forces of nature that define the
boundaries of human culture and provide the myriad
free ecological services that allow us our cities and
farms, or the manner in which particular species have
become embedded in our folk and cultural lore, the
reader is left with the knowledge that we are depend-
ent on the “others” of nature far beyond our physical
survival.
Human ignorance instills fear, and fear breeds vio-
lence and destruction. Natural Grace sets a contrary
path. Knowledge of the other, of nature, can lead to
intimacy, and intimacy can be the foundation of love.
Love, in turn, leads to mutuality, care, and concern for
the other. Dietrich’s melodious writing can indeed lead
one to greater love of nature and hopefully, action on
behalf of nature.
This book is a lovely blend of nature and culture,
of scientific vulgarization and social lore. You will
learn much about the natural history of the Pacific
Northwest. As well, I think, you will learn about how
we (and maybe you yourself) relate to the natural
world, and how that relationship has changed with
time, and how it may or must change in the future.
Given Dietrich’s place of habitation (Seattle), this
book focuses on the State of Washington, with excur-
sions south to Oregon and north to British Columbia.
So, if you call the Pacific Northwest your home, you
will learn much about your “neighbours.” However,
regardless of one’s geography, Dietrich’s work is more
a work of perspective, rather than of content. His
actors live and work in the Pacific Northwest, but the
perspective shared is universal. No matter where you
2004
live, the long, loving, contemplative gaze on the real
is always a possibility.
The 12" century Cistercian monk, Saint Bernard
of Clairvaux, once said; “I have discovered that you
will find far more in the forests than in books; trees
and stones will teach you that which you cannot learn
from any master.” Turn a discerning eye to the crea-
Book REVIEWS
153
tures and processes that surround you and you will
enter a world of marvel and beauty. Let Natural Grace
be your companion and guide.
JOHN McCarthy, S.J.
St. Mark’s College, University of British Columbia, 5935
Iona Drive, Vancouver, British Columbia V6T 1J7 Canada
Tales from the Underground: A Natural History of Subterranean Life
By David W. Wolfe. 2001. Perseus Publishing, 5500 Central
Avenue, Boulder, Colorado 80301 USA. 221 pages. $27.50
Tales from the Underground is a MUST read for
any naturalist interested in what’s happening under
our feet. The book is engaging, well-written, and filled
with information that is truly awesome.
In the introduction, author David Wolfe, Associate
Professor of Plant Ecology at Cornell University, in-
vites his “subterranean-impaired” readers to use their
imaginations and join him on a dive trip into a mys-
terious world scientists are only just beginning to un-
derstand. Wolfe launches the journey with a description
of the various soil “profiles”, also known as layers or
horizons, and the organisms that inhabit them. Some
of the life forms I had never heard of; others I had
never thought about in the way Wolfe describes them.
Take plants, for example. Wolfe starts by praising
their display of foliage aboveground. He then points
out that plants are unique because they simultane-
ously inhabit both the surface and sub-surface realms.
He calls them the “great mediators between the two
realms”, and explains their functions both above and
below the ground, with a focus on their buried other
half: roots.
In Part I of the book, “Ancient Life’, Wolfe covers
a lot of ground. He discusses theories of the origin of
life, the basic elements necessary for the evolution of
life, Earth’s advantage as a life-generating planet, and
speculation pointing to the subterranean realm as the
place where life began. He also introduces “extremo-
philes”, creatures that live in severe conditions thou-
sands of feet underground, where pressure and tem-
peratures are extraordinarily high, and where there is
neither light nor oxygen — the postulated setting for
the beginning of life.
Wolfe also describes Carl Woese’s discovery of the
amazing genetic diversity of these extremophiles, and
discusses how that discovery changed the universal
tree of life. Originally composed of bacteria, plants,
fungi, animals and protozoa, the tree of life now has
only three branches — bacteria, archaea (the extremo-
philes) and eukarya (with plants and animals as two
small twigs). It’s a fascinating and humbling picture.
In Part I, “Life Support for Planet Earth”, Wolfe
dedicates an entire chapter to Charles Darwin and the
lasting influence of the renowned scientist’s meticu-
lous and painstaking work. Wolfe also portrays certain
inconspicuous subterranean creatures and the impor-
tant roles they play in cycling essential elements and
facilitating the flow of energy — processes that sustain
life on this planet. He also discusses the dual roles
played by soil with respect to plant and animal dis-
eases; some soil microbes cause diseases, while others
provide powerful antidotes.
The third part of the book, “The Human Factor”,
describes the enormous footprint of Homo sapiens on
the planet. Wolfe tells the sobering, appalling story
of human activities and their devastating impacts on
wildlife such as prairie dogs, black-footed ferrets, and
burrowing owls, and on soil integrity in general. Des-
criptions of soil erosion and the 1930s dust bowl crisis
are particularly gripping.
Yet despite the doom and gloom, Wolfe ends on an
optimistic note. The very last sentence of the book
reads, “It is my hope that as more of us become aware
of the life beneath our feet, and its relevance to our
well-being, we will be inclined to work together to
maintain the biological integrity of the underground,
and preserve some of what we find there for future
generations” — words we have heard before in one form
or another, but good to see repeated in this context.
Tales from the Underground is David Wolfe’s first
book, and I hope it isn’t his last. He has a pleasant and
easy-to-read writing style, and manages to convey sci-
entific concepts so that even a non-scientific type like
me can understand. Tales from the Underground has
found a permanent place on my bookshelves.
R. SANDER-REGIER
RR5 Shawville, Quebec JOX 2YO Canada
154
NEw TITLES
+Available for review * Assigned for review
Zoology
* Amphibian Decline: An integrated analysis of multi
stressor effects. By Greg Linder. 2004. SETAC North Amer-
ica, 1010 North 12th Avenue, Pensacola, Florida. U.S.$98
Cloth.
Annotated Checklist of Birds of Chile. By M. Marin. 2004.
Lynx Edicions, Barcelona, Spain. 144 pages. U.S.$15.75 [in
English and Spanish].
Biology of Sharks and their Relatives. By J. Carrier, J. Mu-
sick and M. Heithus. 2004. CRC Press, 2000 NW Corporate
Boulevard, Boca Raton, Florida. U.S.$99.95.
* Birds of Belize. By H. L. Jones. 2004. University of Texas
Press, Austin, Texas. 317 pages, U.S.$60.00 Cloth, $34.95
Paper.
Birds of South Asia. By P. Rasmussen and J. Anderton. 2004.
Lynx Edicions, Barcelona, Spain. U.S.$95 Cloth.
Birds of Spain. 2004. Lynx Edicions, Barcelona, Spain. 296
pages. U.S.$49 [in English and Spanish].
Birds of the Raincoast. By H. Thommasen and K. Hutchings.
2004. Harbour Publishing, P.O. Box 219, Madeira Park, Brit-
ish Columbia. 260 pages. U.S.$24.95.
The Exotic Amphibians and Reptiles of Florida. By W.
Meshaka, B. Buttergield and J. Hauge. 2004. Krieger Pub-
lishing P.O. Box 9542 Melbourne, Florida 32902-9452. 166
pages. U.S.$34.50.
* Hawks and Owls of the Great Lakes Region & Eastern
North America. By C. Earley. 2004. Firefly Books Ltd., 3680
Victoria Park Avenue, Toronto, Ontario, M2H 3K1. 128 pages.
$16.95 Paper, $24.95 Cloth.
+ Orca — Visions of the Killer Whale. By Knudtson. 2004.
Greystone Books, Vancouver, British Columbia. xvii +110
pages, $19.95.
Pacific Reef and Shore. By R. Harbo. 2004. Harbour Pub-
lishing, P.O. Box 219, Madeira Park, British Columbia. 80
pages. U.S.$9.95.
Reproductive Biology and Early Life History of Fishes in
the Ohio River Drainage. By T. Simon and R. Wallus. 2004.
CRC Press, 2000 NW Corporate Boulevard, Boca Raton,
Florida U.S.$119.95.
* Self-Portrait with Turtles: A Memoir. Edited by David M.
Carroll. 2004. Houghton Mufflin Co., 222 Berkeley Street,
Boston, Massachusetts 02116. 192 pages. 40 black-and-white
line drawings and halftones. $23.00 Hardcover.
Botany
* Arboretum America: a Philosophy of the Forest. By Diana
Beresford-Kroeger. 2003. University of Michigan Press,
839 Greene Street, P.O. Box 1104, Ann Arbour, Michigan.
196 pages. U.S.$52.50.
Botanical Latin: Fourth Edition. By William T. Stearn.
1992 [Re-issued as a paperback 2004] Timber Press, 133 SW
2nd Avenue, Suite 450, Portland, Oregon, USA. 560 pages.
Paperback, U.S.$29.95.
* Manual of Vascular Plants of Northeastern United States
and Adjacent Canada. By H. Gleason. 2004. New York
THE CANADIAN FIELD-NATURALIST
Vol. 118
Botanical Gardens, 200" Street and Kazimiroff Boulevard,
Bronx, New York. 993 pages. U.S.$69.00.
The Orchid in Lore and Legend. By Luigi Berliocchi. 2000
[Re-issued as a paperback 2004] Edited by Mark Griffiths.
2000 Timber Press, 133 SW 2nd Avenue, Suite 450, Portland,
Oregon, USA. 200 pages. Paperback, U.S.$19.95.
The Secrets of Wildflowers. By J. Saunders. 2004. The Lyons
Press, 246 Goose Lane, P.O. Box 480, Guilford, Connecticut.
304 pages. U.S.$24.95.
Wildflowers of the Seacoast in the Pacific Northwest. By
J. Trelawny. 2004. Harbour Publishing, P. O. Box 219,
Madeira Park, British Columbia. 80 pages. U.S.$12.95.
Environment
Arctic National Wildlife Refuge. By S. Banerjee. 2004.
Harbour Publishing, P.O. Box 219, Madeira Park, British
Columbia. 176 pages. U.S.$36.95.
+ The Bird Almanac. By D. Bird. 2004. Key Porter Books,
70 The Esplanade, Toronto, Ontario, Canada. xvii + 460
pages, not illustrated. $24.95.
* Dancing at the Dead Sea — Tracking the World’s Envi-
ronmental Hotspots. By Alanna Mitchell. 2004. Key Porter
Books, 70 The Esplanade, Toronto, Ontario MSE 1R2 Canada.
259 pages. $26.95.
Estuarine Research, Monitoring and Resource Protection.
By M. Kennish. 2004. CRC Press, 2000 NW Corporate
Boulevard, Boca Raton, Florida. U.S.$119.95.
Important Transboundary Belarussian-Lithuanian and
Lithuanian-Russian Wetlands. By L. Raudonikis, A. Skura-
tovich, L. Baléiauskas, E. Drobelis, D. Grishanov. 2003.
Botanikos institutas, Vilnius, Lithuania.
* The History of Ornithology in Virginia. By D. Johnston.
2004. University of Virginia Press, P.O. Box 400318,
Charlottesville, Virginia. x + 219 pages. U.S.$35.
The Lewis and Clark Columbia River Water Trail: A Guide
for Paddlers, Hikers, and Other Explorers. By Keith G.
Hay. 2004. Timber Press, 133 SW 2nd Avenue, Suite 450,
Portland, Oregon, USA. 264 pages. Paperback, U.S.$19.95.
* Politics of the Wild - Canada & Endangered Species.
Edited by K. Beazley and R. Boardman. 2004. Oxford
University Press, 70 Wynford Drive, Don Mills, Ontario, Can-
ada. x + 254 pages, not illustrated. $29.95.
* A Primer of Ecological Genetics. By J. Conner and D.
Hartt. 2004. Sinauer Associates, Box 407, Sunderland, Massa-
chusetts, USA. 207 pages. U.S.$34.95.
+ Resource and Environmental Management in Canada.
Edited by B. Mitchell. 2004. Oxford University Press, 70
Wynford Drive, Don Mills, Ontario. x + 600 pages, $29.95.
* Whose Bird? By B. Boleus and M. Watkins. 2004. Yale
University Press. 384 pages. U.S.$35.00 paper.
Children’s books
Saving Birds: Heroes around the world. By P. Salmansohn
and S. Kress. 2004. Tilbury House, Gardiner, Maine. 40 pages.
U.S.$16.95.
King Of Fish: The Thousand Year Run of Salmon. By E.
Bauer. 2003. Voyageur, Stillwater, Minnesota. 160 pages.
U.S.$29.95.
News and Comment
Point Pelee Natural History News 3(4)
The Winter 2003 issue, volume 3, number 4, pages 53-68,
contains: Point Pelee: Its Evolution and Structure (Alan S.
Trenhaile) — Noteworthy Bird Records: September to Novem-
ber 2003 (Alan Wormington) — More Cave Swallows: The
Fall of 2003 (Alan Wormington) — Point Pelee Christmas Bird
Count: December 15, 2003 (Sarah E. Rupert) — Fox Squirrels
at Point Pelee: 1977, 1990 and 1997 (Alan Wormington) —
In the Field (Ross’s Gull: Second Record for Point Pelee;
“Harlan’s” Red-tailed Hawk: New to Point Pelee).
The Point Pelee Natural History News was edited by Alan
Wormington (e-mail: wormington@juno.com). Editorial Assis-
COSEWIC Assessment Results November 2003
This update on Canadian Species at Risk issued by the
Committee on the Status of Endangered Wildlife in Canada
(COSEWIC) is 44 pages and contains: About COSEWIC,
(mandate, membership, definitions) — Summary Tables
[COSEWIC species designated in five “risk” categories and
in Not at Risk, and Data Deficient categories (Tables 1-3)] —
Results of November 2003 COSEWIC meeting (Tables 4-5)
— COSEWIC Assessment Results — Explanation of sym-
bols — Species examined in five “risk” categories (Table 6),
Not at Risk (Table 7), and Data Deficient (Table 8) — Record
tants were Gordon D. Harvey and Michelle T. Nicholson; web
site www.wincom.net/~fopp/Natural_History_News.htm. This
is the last issue as the Board of Directors of the publisher,
The Friends of Point Pelee, has decided to terminate the pub-
lication due mainly to the lack of material being submitted.
All past issues are available in the Nature Nook Book Store
in Point Pelee National Park’s Visitor Centre or by mail from
the Friends of Point Pelee, 1118 Point Pelee Drive, Leaming-
ton, Ontario N8H 3V4 Canada; phone 519-326-6173; e-
mail: fopp@ wincom.net.
of Status Re-examinations — Record of Name Changes.
Listed are 12 extinct, 21 extirpated, 160 endangered, 108 threat-
ened, and 140 of special concern. Of the 441 forms in these
categories, 65 are mammals, 58 birds, 31 reptiles, 19 amphib-
ians, 78 fishes, 16 arthropods, 19 molluscs, 140 vascular plants,
9 mosses, and 6 lichens. In addition, 32 forms have been
considered and found not at risk, and 29 to be data deficient.
This publication is available from COSEWIC Secretariat,
Canadian Wildlife Service, Environment Canada, Ottawa,
Ontario K1A 0H3. See Web site: http://www.cosewic.gc.ca.
Froglog: Newsletter of the Declining Amphibian Populations Task Force (61)
Number 60, February 2004. Contents: A Workshop on the
Amphibians of Madagascar at Giand (Franco Andreone) —
Amphibian Colonization of Mitigation Wetlands in Nebraska
(Mark M. Peyton) — Annual Meeting Report from Canada
(David Galbraith) — A Study of the Plethodontid Salamander
Populations at Raccoon Creek State Park, Pennsylvania (Jen-
nifer D. Haney and Mary S. Kostalos) — Reports on DAPTF
Seed Grants — Froglog Shorts — New Book on Amphibian
Declines (Amphibian Declines: An Integrated Analysis of Mul-
tiple Stressor Effects. 2003. SETAC Press, Pensacola, Florida:
http://www.setac.org/pubs. html).
Froglog is the bi-monthly newsletter of the Declining
Amphibian Populations Task Force of The World Conservation
Union (IUCN)/Species Survival Commission (SSC) and is
supported by The Open University, The World Congress of
Herpetology, and Arizona State University. The newsletter is
edited by John W. Wilkinson, Department of Biological Sci-
ences, The Open University, Walton Hall, Milton Keynes,
MK7 6AA, United Kingdom; e-mail: daptf@open.ac.uk. Fund-
ing for Froglog is underwritten by the Detroit Zoological
Institute, P. O. Box 39, Royal Oak, Michigan 48068-0039,
USA. Publication of issue 61 was also supported by Peace
Frogs www.peacefrogs.com and by RANA and the US
National Science Foundation grant DEB-0130273.
The Boreal Dip Net/L’Epuisette Boreal: Newsletter of the Canadian Amphibian and Reptile
Conservation Network — Reseau Canadien de Conservation des Amphibiens et des Reptiles
8(1) January 2004
Contents: Editor’s Note: thanks to sponsors TD Bank
Financial Group, TD Friends of the Environment, The Pelee
Island Winery, Parks Canada [Kerrie Serben] — A note
about our acronym [David Galbraith] — CARCNET/RECCAR
2003: The Pelee Isand Experience [David Galbraith] —
Summary of Species at Risk Proceedings from the 8th Annual
Meeting of CARCNET/RECCAR and the 3rd Annual Pelee
Island Winery Endangered Species Festival (ESF) [Kim
Barrett and Ben Porchuk] — The Lake Erie Watersnake: A
23-year Perspective on Microevolution, Population Status,
and Recovery Planning [Richard B. King] — Loving Nature
to Death [Ron Brooks] — Another Leap into Learning [Sara
L. Ashpole] — Books to Get: Turtles [Anita Baskin-Salzberg
and Allen Salzberg]; A guide to creating vernal ponds —
Endangered Northern Leopard Frog Reintroduced into East
Kootenay After 20 Year Disappearance — Frogs and Toads
of Canada CD — Current CARCNET/RECCAR Board of
Directors — New Species of Salamander Found in Revel-
stoke [Larry. Halverson] — Paper on Traffic Mortality and
Turtles [reviewed by David Seburn] — Coming soon...
CARCNET 2004 September 24-27 Edmonton — Member-
ship in CARCNET/ RECCAR.
LDS)
156
For information on membership in the Canadian Amphibian
and Reptile Conservation Society/Reseau Canadien de Con-
servation des Amphibiens et des Reptiles ($10 students, $16
non-students] contact Bruce Pauli, Canadian Wildlife Service,
THE CANADIAN FIELD-NATURALIST
Vol. 118
National Wildlife Research Centre, Carleton University, Raven
Road, Ottawa, Ontario K1A 0H3. Web site: http://www.carc
net.ca/
Annotated List of the Arctic Marine Fishes of Canada
In 2004 Fisheries and Oceans Canada, Central and Arctic
Region, Winnipeg, Manitoba, printed a limited number of
copies of the Annotated List of the Arctic Marine Fishes of
Canada by B. W. Coad and J. D. Reist as Canadian Manu-
script Report of Fisheries and Aquatic Sciences 2674, iv +
112 pages. A primary list covers the 189 species represent-
ing 115 genera in 48 families of marine and anadromous fishes
in Canadian Arctic and marine waters. Given under scien-
tific name, authority, and description date, are the Common
Name, Provinces/Territories of occurrence, Ecozone, Distribu-
tion (ocean and extralimital), Numbers, Size (maximum), and
Biology (depth, food, commercial importance). An extralimitial
list gives 83 species occurring in adjacent areas that might
eventually be recorded in Canadian Arctic waters annotated
as eastern (eastern Davis Strait, southwest Greenland) and
western (western Beaufort Sea of Alaska from Point Barrow
Marine Turtle Newsletter (103)
January 2004. 32 pages: ARTICLES: Behavior of Green Sea
Turtles in the Presence and Absence of Recreational Snork-
ellers — Turtle Strandings in the Southern Eritrean Red Sea
— First Confirmed Occurrence of Loggerhead Turtles in
Peru — A Harness for Attachment of Satellite Transmitters
on Flatback Turtles — Notes: Nesting of the Hawksbill Turtle
in Shidvar Island, Hormozgan Provance, Iran — MEETING
REPORTS — OBITUARIES (Henry H. Hildebrand 1922-2003;
C. Robert Shoop 1935-2003) — ANNOUNCEMENTS — NEWS
& LEGAL BRIEFS — RECENT PUBLICATIONS.
eastwards). A brackish water list gives 36 species whose life
is usually spent entirely in fresh waters but which may enter
estuaries and seashore pools in the Canadian Arctic. There
are 3 tables (species by province and territory, by ecozones,
and by distribution (Alaska, Atlantic, Eurasia)); 2 maps (Can-
adian Arctic waters and ecozones with this area); and two
appendicies: one giving an alphabetical listing of scientific
names of families with common names in English, French,
Inuktitut and Inuvialuktun and one giving an alphabetical
listing of species by scientific name with notation of new to
Arctic, new to Canada, and page number in text.
Copies of this report are available from Fisheries and
Oceans Canada Central and Arctic Region, Winnipeg, Mani-
toba R3T 2N6 Canada: e-mail reistj@dfo-mpo.ge.ca [Cata-
logue number Fs 97-4/26/2674E, ISSN 0706-6473].
The Marine Turtle Newsletter is edited by Brendan J.
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Group, School of Biological Sciences, University of Exeter,
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Ontario Natural Heritage Information Centre Science and Information Newsletter 9(1)
Winter 2004
Contents of this 20 page issue: FEATURE ARTICLES: Decade
of Achievement (NHIC 10" anniversary celebrated 9 Decem-
ber 2003) — A Decade of Ontario Botanical Dsicoveries;
2003 PROGRAM HiIGLicuts: NHIC Staff Participate in James
Bay Coastal Vegetation Study — Notes on the Vegetation
and Flora of Flooding River Shores — A Profile of Natural
Areas Recently Added to the Natural Areas Database; 2003
ProJEcT HIGHLIGHTS: NHIC Conducts Turtle Surveys —
NHIC Coordinates Odonata and Reptile Surveys — Update
on the Great Lakes Conservation Blueprint Projects —
Identifying Key Natural Areas and Linkages in Southern
Ontario — NHIC’s Southern Region Element Occurrence
Prioritization Project; NEws AND NorTEs: Species at Risk: A
Diversity of Designations — What’s in a Name? Changes to
the Provincial Amphibian and Reptile Lists — NHIC Attends
Pelee Island Events — NatureServe Canada and Parks Agency
sign MOU — NatureServe Participates with CWS on Spe-
cies at Risk Information Needs Analysis — Additions to the
COSEWIC list — Minister visits NHIC; Book REvVIEws:
NHIC STAFF INFORMATION.
Mailing address for Natural Heritage Information Centre,
Ontario Ministry of Natural Resources, 300 Water Street,
2nd Floor, North Tower, P.O. Box 7000, Peterborough, On-
tario K9J 8M5, Canada; www.mnr.gov.on.ca/MNR/nhic.cfm.
Web page: http://www.mnr.gov.on.ca/MNR/nhic.html
2004 NEWS AND COMMENT 157
Erratum Canadian Field-Naturalist 117(1)
Ballard, Warren B., Matthew A. Cronin, Martin D The abbreviation for concentrations in micrograms per
5 9 . 5 a . x z ;
Robards, and William A. Stubblefield. 2003. Heavy gram of dry weight should be corrected in two places.
, ‘ ; . x 0 as J. c rd ae 5 te pS) =f; k Pa ; Ore
metal concentrations in Arctic Foxes, Alopex lagopus, in On page 120 “mg/g” left column line 18, and right
the Prudhoe Oil Field, Alaska. Canadian Field-Naturalist column line 21, should be “g/g”.
117(2): 119-121.
Erratum Canadian Field-Naturalist 117(2)
Lindquist, E. S., C. F. Aquadro, D. McClearn, and K J. 117(2): 184-189.
McGowan. 2003. Field identification of the mice On page 4, Figure 1, 1A was repeated for 1B. The correct
Peromyscus leucopus noveboracensis and P. maniculatus 1B is shown below with IA.
gracilis in central New York. Canadian Field-Naturalist
Distance from P. leucopus
Distance from P. leucopus
O 4 2 38 4 5 6
Distance from P. maniculatus
Distance from P. maniculatus
FiGurRE 1. Classification of P. |. noveboracensis and P. m. gracilis using the discriminant-function coefficients given in Table
2. Figure la shows the classification of adults only. Figure 1b shows the classification of adults and juveniles. Open
and closed symbols denote P. m. gracilis and P. |. noveboracensis, respectively. In Figure 1b, P. m. gracilis is indicated
by open circles and squares (adult and juvenile, respectively), and P. |. noveboracensis by closed triangles and stars
(adult and juvenile, respectively).
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158
TABLE OF CONTENTS (concluded) Volume 118 Number 1
Record high wolf, Canis lupus, pack density L. DAVID MECH AND SHAWN TRACY
Extraordinary size and survival of American Black Duck, Anas rubripes, broods
JERRY R. LONGCORE AND DANIEL G. MCAULEY
Observations of interactions between Puma, Puma concolor, and introduced
European Red Deer, Cervus elaphus, in Patagonia WERNER T. FLUECK
Premiéres mentions de la Couleuvre mince, Thamnophis sauritus septentrionalis, au Québec
JEAN-FRANCOIS DESROCHES ET RICHARD LAPARE
Book Reviews
ZooLoGy: Amphibian Decline: An Integrated Analysis of Multiple Stressor Effects — Birds of Africa:
From of Seabirds to Seedeaters — The Firefly Encyclopedia of Birds — Birds of Belize — Herpetology:
Third Edition — Lizards: Windows to the Evolution of Diversity — Raptors of Western North America
— Raptors of Eastern North America — Turtles and Tortoises — What Good are Bugs? Insects in the
Web of Life — Belugas in the North Atlantic and Russian Arctic — The Firefly Encyclopedia of Insects
and Spiders
Botany: Biotic Forest Communities of Ontario — Les champignons des arbres de |’est de l’ Amerique du
Nord — Manual of Vascular Plants of Northeastern United States and Adjacent Canada: Second Edition
— The Wild Orchids of North America, North of Mexico — Trees of the Carolinian Forest: A Guide to
Species, Their Ecology and Uses
ENVIRONMENT: Good News for a Change: How Everyday People are Helping the Planet — Whose Bird?
— Forest Dynamics and Disturbance: Studies from Temperate Evergreen-Deciduous Forests —
Snowshoes & Spotted Dick: Letters from a Wilderness Dweller— Natural Grace: The Charm, Wonder,
& Lessons of Pacific Northwest Animals & Plants — Tales from the Underground: A Natural History
of Subterranean Life
NEw TITLES
News and Comment
Point Pelee Natural History News 3(4) — COSEWIC Assessment Results November 2003 — Froglog (61) —
The Boreal Dip Net 8(1) — Annotated List of the Arctic Marine Fishes of Canada — Marine Turtle News-
letter (103) — Ontario Natural Heritage Information Centre Science and Information Newsletter 9(1)
Winter 2004 — Erratum: The Canadian Field-Naturalist 117(1) — Erratum:The Canadian Field-
Naturalist 117(2)
Advise to Contributors
Mailing date of the previous issue 117(4): 16 September 2004
2004
PA
129
138
146
149
153
THE CANADIAN FIELD-NATURALIST Volume 118 Number 1 200
——_—— Ore NET EE UUE
125 Years’ Anniversary:
The Ottawa Field-Naturalists’ Club: origins and history DANIEL F. BRUNTON l
Articles
Continuing environmental change — an example from Nova Scotia EDMUND S. TELFER 39)
Habitat segregation among songbirds using the southern boreal
mixedwood forest ENID E. CUMMING 45
Effects of mid-winter snow depth on stand selection by Wolverines, Gulo gulo luscus,
in the boreal forest JONATHAN D. WRIGHT AND JESSICA ERNST 56
Wolverine, Gulo gulo luscus, resting sites and caching behavior in the boreal forest
JONATHAN D. WRIGHT AND JESSICA ERNST 61
Seasonal home ranges of Raccoons, Procyon lotor, using a common feeding site in rural eastern
Ontario: rabies management implications SARAH C. TOTTON, RICHARD C. ROSATTE,
ROWLAND R. TINLINE, AND LAuRA L. BIGLER 65
Status of marine turtles in British Columbia waters: a reassessment
DONALD F. MCALPINE, STAN A. ORCHARD,
KELLY A. SENDALL, AND RON PALM 2
Introduced marine species in the Haida Gwaii (Queen Charlotte Islands) region,
British Columbia N. A. SLOAN AND P. M. BARTIER Vil
Ruby-throated Hummingbird, Archilochus colubris, entanglements in burdock
(Arctium spp.) at Delta Marsh, Manitoba HEATHER L. HINAM, SPENCER G. SEALY,
AND Topp J. UNDERWOOD 85
Multiple mating results in multiple paternity in Richardson’s Ground Squirrels,
Spermophilus richardsonii JAMES F. HARE, GLENDA Topp, AND WENDY A. UNTEREINER 90
Demographic patterns and limitations of wolves, Canis lupus, in and near Pukaskwa
National Park, Ontario S. ANNE FORSHNER, PAUL C. PAQUET, FRANK G. M. BURROWS,
GRAHAM K. NEALE, AND KEITH D. WADE 95
Estimation of seed bank and seed viability of the Gulf of Saint Lawrence Aster,
Symphyotrichum laurentianum (Fernald) Nesom — Joni FE. KEMP AND CHRISTIAN R. LACROIX 105
Consumption of shrews, Sorex spp., by Arctic Grayling,
Thymallus arcticus JONATHAN W. Moore AND G. J. KENAGY Hi
Unusual behavior by Bison, Bison bison, toward Elk, Cervus elaphus, and Wolves, Canis lupus
L. Davip MEcH, RICK T. MCINTYRE, AND DOUGLAS W. SMITH 115
r
Notes
Morphology of female Woodland Caribou, Rangifer tarandus caribou,
in Saskatchewan W. JAMES RETTIE 119
Occurrence of parasitoid wasps in the egg sacs of Pardosa moesta and Pardosa sternalis
(Araneae, Lycosidae) in southern Idaho LisA M. COBB AND VINCENT A. CoBB 12D
The Northern True Katydid, Pterophylla camellifolia (Insecta: Orthroptera: Pseudophyllidae),
at Ottawa, Ontario STEPHEN J. DARBYSHIRE 124
(continued on inside back cover)
ISSN 0008-3550
The CANADIAN
— FIELD-NATURALIST
Published by THE OTTAWA FIELD-NATURALISTS’ CLUB, Ottawa, Canada
Volume 118, Number 2 April-June 2004
The Ottawa Field-Naturalists’ Club
FOUNDED IN 1879
Patrons
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Cover: Brown Bear, Ursus arcts, watches Gray Wolf, Canis lupus, in the Katmai National Park and Preserve in southwest Alaska.
See paper by Smith, Partridge, and Shoen pages 247-250 (Kent Fredrikson photograph).
The Canadian Field-Naturalist Uxiijeees2y
Volume 118, Number 2 April-June 2004
Morphology and Population Characteristics of Vancouver Island Cougars,
Puma concolor vancouverensis
STEVEN F. WILSON!, APRYL HAHN, AARON GLADDERS, KAREN M. L. Gou, and DAvip M. SHACKLETON
Wildlife Research Group, Agroecology, Faculty of Agricultural Sciences, University of British Columbia, 270-2357 Main
Mall, Vancouver, British Columbia V6T 1Z4 Canada
'Present address: EcoLogic Research, 406 Hemlock Avenue, Gabriola Island, British Columbia VOR 1X1 Canada
Wilson, Steven F., Apryl Hahn, Aaron Gladders, Karen M. L. Goh, and David M. Shackleton. 2004. Morphology and population
characteristics of Vancouver Island Cougars, Puma concolor vancouverensis. Canadian Field-Naturalist 118(2): 159-163.
Cougars are a management concern on Vancouver Island because they are a top predator and because there have been frequent
attacks on humans on the island. However, little is known about Cougar ecology in the Pacific Northwest of North America.
We studied Cougar morphology and population characteristics as part of a larger study in two areas on Vancouver Island. We
derived a multivariate measure of body size to describe changes with age and sex. Body size was similar in the two study
areas. Survival rates for adult females were higher than those reported elsewhere; however, hunters avoided shooting females
in general, and radio-collared Cougars in particular. Litter size at first detection was lower than reported in many other
studies and may be related to food availability.
Key Words: Cougars, Puma concolor vancouverensis, morphology, survival, mortality, natality, Vancouver Island, British
Columbia.
The Mountain Lion, or Cougar (Puma concolor van-
couverensis), 1s one of the two main large predatory
carnivores in the forests of Vancouver Island, British
Columbia, Canada. It also has a long history of inter-
actions with humans as a nuisance (livestock predation)
and as a game species (Beier 1991). The incidence of
Cougar attacks on humans in North America is also
highest on the island. However, little is known about
the ecology of Cougar in this part of its range, mainly
because this subspecies inhabits dense forests typical
of coastal British Columbia. We examined Cougar mor-
phology and population characteristics in two study
areas on Vancouver Island to investigate the effects of
age, sex, and location on body size, and to determine
survival rates and reproductive characteristics.
Methods
Research was conducted on a 700-km? area near
Northwest Bay (NWB), British Columbia, and on a
1000-km? area centred on the Adam and Eve River
valleys (AE) approximately 300 km northwest of NWB
(Figure 1). Principal habitats at NWB consisted of
different seral stages of Douglas Fir (Pseudotsuga men-
ziesii), Western Hemlock (Tsuga heterophylla), and
Western Redcedar (Thuja plicata) forests. The AE
study area was more rugged and dominated by exten-
sive stands of unlogged forest, particularly at higher
elevations. Habitats at lower elevations were dominated
by Western Hemlock and Western Redcedar while spe-
cies at higher elevations included Mountain Hemlock
(Tsuga mertensiana) and Yellow Cedar (Chamaecy-
paris nootkatensis). Understory vegetation on both
study areas was typically dense and consisted of Salal
(Gaultheria shallon), ferns (several genera) and Vac-
cinium species communities. Both study areas had
cool summers and mild winters, with temperatures of
0-10°C for 4-6 months/year and annual precipitation
of 1700-5000 mm/year (Meidinger and Pojar 1991).
AE was cooler and wetter, with a greater proportion
of precipitation falling as snow.
Cougars were captured between 4 March 1991 and
1 September 1996 at NWB and from 18 April 1997 to
12 September 1998 at AE. Local houndsmen were
contracted to track and tree Cougars. Treed Cougars
that could safely be immobilized were darted with a
mixture of ketamine hydrochloride (3 mg/kg estimat-
ed total weight) and medetomidine hydrochloride (0.1
mg/kg). Cougars were sexed, measured (see below),
and aged according to tooth replacement and wear, and
by gum recession (Ashman et al. 1983; Laundré et al.
2000). Adult Cougars were fitted with VHF radio col-
lars (Telonics, Inc., Mesa, AZ). Immobilizations were
reversed with atipamezole (0.15 mg/kg). Morphologi-
cal data from hunter-killed Cougars in and near AE
were also included in our analyses.
159
160
126° W 124° W
50° N
Bay (NWB)
FiGureE |. Location of cougar study areas on Vancouver
Island, British Columbia, Canada.
Morphological measurements taken included: total
weight (using a 100 kg spring balance to the nearest
1 kg), neck circumference at the base of the skull, chest
circumference immediately behind the front legs,
body length from nose to base of tail, tail length from
base to tip of the last vertebrae (all to the nearest cm
with a cloth tape measure), canine length from
gumline to tip, and front and rear pad widths (to the
nearest mm with a cloth tape measure; AE only).
We used principal component analysis (PCA) to
derive a single variable to represent body size, based
on the correlation matrix of morphological variables
(Statistica 1995). We used this body size measure in-
stead of total weight to describe the size of Cougars
because it was less condition-dependent that using
total weight alone. Where Cougars were captured >1
time, we included data from only the most recent
capture. We used an analysis of covariance to test for
differences in body size (log-transformed) between
sex and study area, using age as a covariate. We also
calculated means (+2 SE) for each morphological
variable (by sex), but excluded Cougars <2 years old
to minimize skews in distributions caused by the
smaller body sizes of juvenile Cougars.
We calculated survival estimates with the staggered
entry design of Pollock et al. (1989), which is based
on the Kaplan-Meier product limit estimator (Kaplan
and Meier 1958). This method estimates annual sur-
vival rate as the product of weekly survival rates (1 —
d/r), where d is the number of animals that die and r
THE CANADIAN FIELD-NATURALIST
Vol. 118
is the number of animals “at risk” in a weekly period.
Cougars carrying functioning radio collars comprised
the “‘at risk” sample for each week. The design was
“staggered entry” because not all Cougars carried col-
lars at the same time. Cougars were added to the week-
ly sample as they were collared, and were removed as
they died, had their collars removed, or when their col-
lars stopped functioning. Analysis started with the
collaring of the first Cougars in the two study areas.
Annual survival estimates were based on 52 consecu-
tive, seven-day periods.
There were sufficient data to analyse adult female
Cougar survival; however, sample sizes were small,
and the length of the study was relatively short in
relation to the life expectancy of Cougars. Therefore,
our estimates should be interpreted with caution.
We report the reproductive characteristics of col-
lared females anecdotally because data were insuffi-
cient to calculate population growth rates; specifical-
ly, we had few data on birth intervals and survival to
maturity. We report litter sizes (42 SE) when they were
first seen, so litter sizes at birth may have been larger,
although in at least three litters, kittens were seen when
<10 days old (eyes not open).
Results
Thirty Cougars were measured at NWB (17 females
and 13 males) and 26 at AE (15 females and 11 males).
We used total weight, neck and chest circumfer-
ence, and total length (body length + tail length) in
the final PCA to derive a body size variable. All four
variables loaded strongly and positively on the first
axis, which explained 83% of the variation in the
dataset. As a result, we used the first PCA axis as the
index of body size (Table 1). We did not include canine
length and body and tail lengths as separate variables
in the analysis because doing so did not significantly
increase the variation described in the first axis.
Body size differed between males and females
(P < 0.000), but not between study areas (P = 0.736;
Figure 2). Differences between males and females were
also evident in univariate means of the morphologi-
cal measurements (Table 2).
Mean survival rates were similar for collared Cou-
gars on both study areas (Table 3). Known causes of
female mortality at NWB included intraspecific kill-
ings (2) and animal control (3). The cause of one fe-
male mortality at NWB and both female mortalities at
AE were unknown. Two mortalities of collared male
TABLE |. Correlation between morphological variables and the first principal component axis (also known as “factor load-
ings”). The axis (based on the correlation matrix) was used as an index to describe body size of Vancouver Island Cougars
in subsequent analyses.
Factor loadings of morphological variables
Neck Chest
0.889 0.927
Total Weight
0.994
Body length
Eigenvalue
3.314
% variation explained
0.878 82.8
2004
WILSON, HAHN, GLADDERS, GOH, and SHACKLETON: VANCOUVER ISLAND COUGARS 16]
Males:
y = 1.45Ln(x) - 0.54
R? = 0.70
Females: e
6 y = 0.52Ln(x) - 1.09
R? = 0.34
UF T
0 2 4
T li
6 8 10
Age (years)
FiGure 2. Relationship between body size (derived from the principal component analysis on morphological measurements,
see text) and age for male and female Cougars in the two Vancouver Island study areas. Logarithmic trend lines are
presented for males (squares @) and females (diamonds @) , pooled by study area. The body size measurement was
used because it was less condition-dependent than using total weight alone.
Cougars were investigated at AE; one was shot by hunt-
ers and the other was suspected to have been shot
illegally.
At NWB, mean litter size at first detection was 1.9
+ 0.1 (n= 16). One female was known to have a litter
of three kittens, and there were 12 other litters of two
kittens and 3 of one kitten when first observed. Fe-
males were known or suspected to give birth during all
months from March-October. Consecutive litters were
recorded for two females; each had litters 21 and 23
months apart.
Litter size at AE was 1.8 + 0.7 (n = 5). There was
one litter of three, and two litters each of one and two
kittens. Females gave birth in January, August, and
September. No collared females at AE had more than
one litter during the study period.
Discussion
Results presented in this paper are based on small
absolute sample sizes; however, Cougars are rare and
secretive, and inferences about their morphology and
behaviour must often be based on few animals. The
TABLE 2. Means and standard errors of morphological measurements taken on captured Vancouver Island Cougars.
Males
Measurement n Mean
Total Weight (kg) 13 Ss
Neck (cm) 12 39.5
Chest (cm) 12 VS)
Body length (cm) 13 128.2
Tail Length (cm) 13 73.0
Front pad Width (mm) 9 57.9
Hind pad Width (mm) 9 50.4
Canine Length (mm) 10 28.6
Females
2 SE n Mean 2 SE
Si 22 39.1 Pel
3.0 23 394 13}
3.5 23 65.4 1.6
6.6 23 120.9 Bill
4.5 23 ORI 3}
1.9 12 Syl I)
33 12 37.9 9.1
es) 23 26.8 2.0
162
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 3. Annual and mean survival rates of female Vancouver Island Cougars collared in two study areas: Northwest Bay
(NWB) and Adam and Eve rivers (AE). Annual estimates were based on a staggered-entry design, starting with the first
Cougars collared at NWB and AE in March 1991 and April 1997, respectively.
Study Area Year n
NWB 1991-1992
1992-1993
1993-1994
1994-1995
1995-1996
AE 1997-1998
1998-1999
1999-2000
ISSAP Sy Sap ays
densities of Cougars in our study areas also suggest
that significant proportions of the populations were
captured (2.6-7.3 Cougars/100 km? at NWB and 1.4-
2.0 Cougars/100 km? at AE; S. Wilson, unpublished
data). Our sample sizes were similar to, or larger than,
those in many comparable studies (e.g., n = 22,
Hemker et al. 1984; n = 68, Ross and Jalkotzy 1992;
n= 76, Lindzey et al. 1994; n = 34, Spreadbury et al.
19962 n=13;, Prankhin;et ‘al. 1999: n= 21, Pierce;ct
al. 2000).
Few researchers have published Cougar morpholog-
ical characteristics (c.f Kohlmann and Green 1999;
Grigione et al. 2002); however, mean measurements
of Vancouver Island Cougars in this study were smaller
than those reported by Cowan and Guiguet (1965) for
14 adult male (mean total length 241 cm, tail length
89 cm, mean total weight 73 kg) and 7 adult female
(mean total length 206 cm, tail length 79 cm, mean
total weight 46 kg). Vancouver Island Cougars are
slightly smaller than those found elsewhere in British
Columbia (Cowan and Guiguet 1965).
Survival estimates are critical for population man-
agement, but few studies report them. Using the same
method and similar sample sizes, Lindzey et al. (1988)
reported mean survival rates (S = 0.731) for female
Cougars in a largely unhunted population in southern
Utah that were lower than those we calculated for
Vancouver Island Cougars (mean for both study areas
S = 0.885). Hunting is an important component of
mortality in Cougar populations where hunting is al-
lowed (Hemker et al. 1984; Logan et al. 1986; Ross
and Jalkotzy 1992). The Vancouver Island population
is no exception; however, we were in frequent contacts
with hunters in our study areas and know they often
treed radio-collared cougars but chose not to shoot
them, even though we did not request this. This might
have inflated the survival rates calculated for radio-
collared Cougars. Researchers and managers should
be aware of this bias when calculating survival esti-
mates from similar radio telemetry studies where
hunters “lend a hand” by not shooting study animals.
Survival -2 SE +2 SE Mean
1
1
0.75 0.47 1
0.82 0.56 1
0.88 0.64 1 0.89
0.80 0.53 1
1
0.83 0.50 ff 0.88
Animal control by British Columbia Wildlife Branch
Control Officers was a significant source of human-
caused mortality at NWB, where the human popula-
tion density was higher than at AE. Intraspecific killing
has been reported as an important source of mortality
elsewhere (Lindzey et al. 1988; Spreadbury et al. 1996),
but in our study it was detected only at NWB where
Cougar population density was significantly higher than
at AE.
Litters in both of our study areas were smaller than
those reported in southeastern British Columbia
(x = 3.1; Spreadbury et al. 1996), southwestern Al-
berta (x = 2.2; Ross and Jalkotzy 1992), Wyoming
(x = 2.7; Logan et al. 1986), and southern Utah
(x = 2.4; Lindzey et al. 1994). Other studies have
recorded births in most months of the year (Ross and
Jalkotzy 1992; Lindzey et al. 1994), with a peak in
late summer and early fall (Lindzey et al. 1994). Our
observations at AE were similar. The pattern was dif-
ferent at NWB, with no births recorded in winter and
no obvious peaks in births during the spring-fall period.
Columbia Black-tailed Deer (Odocoileus hemionus
columbianus) are the Vancouver Island Cougars’ pri-
mary prey. Indices of deer abundance declined 55%
from 1991-1996 at NWB and 38% from 1995-1999 at
AE (British Columbia Ministry of Environment, Lands
and Parks, unpublished data); therefore, small litter
sizes among Vancouver Island Cougars may be a result
of low food availability. Also, Black-tailed Deer are
smaller than mainland Mule Deer (Odocoileus hemi-
onus; Shackleton 1999). This highlights the importance
of maintaining prey populations in management of
Cougars on Vancouver Island.
Acknowledgments
This research was supported by Forest Renewal
British Columbia, British Columbia Ministry of Envi-
ronment, Lands, and Parks (MELP), Habitat Conserva-
tion Trust Fund, Science Council of British Columbia,
MacMillan Bloedel Limited, TimberWest Limited,
Western Forest Products Limited, BC Hydro, Mountain
2004
Equipment Co-op, and the University of British Col-
umbia. We thank M. DeLaronde, S. Foster, D. Koshow-
ski, J. Leo, R. Ramcharita, H. Robinson, C. Wainwright,
K. Wickert, and local houndsmen for assistance with
fieldwork. For logistic support we also thank G. Brun-
ham, K. Brunt, T. Hamilton, D. Janz, and H. Schwantje
of MELP, as well as many staff of MacMillan Bloedel
Limited in Nanaimo and Campbell River, British
Columbia, and of TimberWest Limited in Nanaimo,
B.C. S. Kohlmann, F. Scott and D. Nagorsen made
helpful comments on the manuscript. This paper is
dedicated to the memory of the late K. Atkinson, who
conceived and supported the project from the outset.
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M. Wickersham. 1983. The mountain lion in Nevada.
Nevada Department of Fish and Game, Federal Aid in
Wildlife Restoration Final Report W-48-15.
Beier, P. 1991. Cougar attacks on humans in the United States
and Canada. Wildlife Society Bulletin 19: 403-412.
Cowan, I. McT., and C. J. Guiguet. 1965. The mammals of
British Columbia. British Columbia Provincial Museum
Handbook Number 11, Victoria, British Columbia. 414
pages.
Franklin, W. L., W. E. Johnson, R. J. Sarno, and J. A.
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color patagonica in southern Chile. Biological Conservation
90: 33-40.
Grigione, M. M., P. Beier, R. A. Hopkins, D. Neal, W. D.
Padley, C. M. Schonewald, and M. L. Johnson. 2002.
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for mountain lions (Puma concolor). Animal Conservation
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Hemker, T. P., F. G. Lindzey, and B. B. Ackerman. 1984.
Population characteristics and movement patterns of cou-
gars in southern Utah. Journal of Wildlife Management
48: 1275-1284.
Kaplan, E. L., and P. Meier. 1958. Nonparametric estimation
from incomplete observations. Journal of the American
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Kohlmann, S. G., and R. L. Green. 1999. Body size dynam-
ics of cougars (Felis concolor) in Oregon. Great Basin
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Laundré, J. W., L. Hernandez, D. Streubel, A. Altendorf,
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Lindzey, F. G., Ackerman, B. B., Barnhurst, D., and
Hemker, T. P. 1988. Survival rates of mountain lions in
southern Utah. Journal of Wildlife Management 52: 664-
667.
Lindzey, F. G., W. D. Van Sickle, B. B. Ackerman, D. Barn-
hurst, T. P. Hemker, and S. P. Laing. 1994. Cougar popu-
lation dynamics in southern Utah. Journal of Wildlife
Management 58: 619-624.
Logan, K. A., L. L. Irwin, and R. Skinner. 1986. Character-
istics of a hunted mountain lion population in Wyoming.
Journal of Wildlife Management 50: 648-654.
Meidinger, D. V., and J. Pojar. 1991. Ecosystems of British
Columbia. Special Report Series 6, British Coiumbia
Ministry of Forests, Victoria, British Columbia. 330 pages.
Pierce, B. M., V. C. Bleich, and R. T. Bowyer. 2000. Social
organization of mountain lions: does a land-tenure system
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Pollock, K. H., S. R. Winterstein, C. M. Bunck, and P. D.
Curtis. 1989. Survival analysis in telemetry studies: the
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Ross, P. I., and M. G. Jalkotzy. 1992. Characteristics of a
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Shackleton, D. M. 1999. The Hoofed Mammals of British
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Spreadbury, B. R., K. Musil, J. Musil, C. Kaisner, and J.
Kovak. 1996. Cougar population characteristics in south-
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Received 7 May 2001
Accepted 5 November 2004
Conservation Evaluation of Lemmon’s Holly Fern, Polystichum
lemmonii, a Threatened Fern in Canada”
GEORGE W. DoucLas!: 2
‘Conservation Data Centre, British Columbia Ministry of Sustainable Resource Management, Terrestrial Information
Branch, P.O. Box 9993 Stn Prov Govt, Victoria, British Columbia V8W 9R7 Canada
> Current address: Douglas Ecological Consultants Ltd., 6230 North Road, Duncan, British Columbia V9L 6K9 Canada
Douglas, George W. 2004. Conservation evaluation of Lemmon’s Holly Fern, Polystichum lemmonii; a threatened fern in
Canada. Canadian Field-Naturalist 118(2): 164-168.
In Canada, Lemmon’s Holly Fern, Polystichum lemmonii, is restricted to the Baldy Mountain area on the eastern side of the
Okanagan River valley in south-central British Columbia. This population represents the northern limits of the species
which ranges south through northern Idaho, Washington and Oregon to northern California. In British Columbia, P. lemmonii
is associated with ultramafic rocky ridges within a montane forest at an elevation of 1900 m. The population in the Baldy
Mountain area is relatively small, unprotected and potentially imperilled by mining exploration, forest road construction or
wildfires.
Key Words: Lemmon’s Holly Fern, Polystichum lemmonii, threatened, distribution, population size, British Columbia.
Lemmon’s Holly Fern, Polystichum lemmonii
Underw. [taxonomy and nomenclature follow Douglas
et al. (1998a, b; 2000)], is a member of a cosmopolitan
genus of over 175 species (Smith and Lemieux 1993;
Wagner 1993). It is one of eight Polystichum species
occurring in British Columbia (Ceska 2000) and nine
occurring in Canada (Cody and Britton 1989; Wagner
1993). Generally, American authors treated P. lem-
monii as a synonym of P. mohrioides (Bory) C. Presl.
until Wagner (1979) demonstrated that the North Am-
erican plant was different from the South American
plant. Polystichum lemmonii was first recorded in
Canada by Cody and Britton (1984).
Polystichum lemmonii 1s an evergreen, perennial,
tufted fern arising from a short, stout rhizome (Figure
1; Ceska 2000). The decumbent to ascending fronds
are 10-40 cm long, 3-7 cm wide and 2-pinnate. The
20-35 pinnae on each side of the rachis are ovate with
rounded pinnules. The ultimate segments are entire
or weakly toothed. The round sori are attached near
the midvein with entire or minutely toothed indusia.
In British Columbia, P. lemmonii may be confused
with either Kruckeberg’s Holly Fern (P. kruckebergii)
or Mountain Holly Fern (P. scopulinum). It may be
* The field work for the Polystichum lemmonii project was
funded by the British Columbia Conservation Data Centre.
The results appear in the British Columbia Conservation
Data Centre database and a rare plant manual (Douglas
et al. 2002). This information formed the basis for a
Committee on the Status of Endangered Wildlife in Canada
status report (Douglas 2003*) and the subsequent assess-
ment of threatened (COSEWIC 2003*). The present paper
also includes more recent information that will be used
in a National Recovery Strategy for P. lemmonii (Doug-
las 2005).
FiGurE 1. Mlustration of Polystichum lemmonii (line
drawing from Ceska 2000).
164
2004
———~
KAMLOOPS
SPENCES BRIDGE
ARMSTRONG
Sw
PRINCETON PENTICTON
KEREMEOS |
) BRITISH
‘& . COLUMBIA
FIGURE 2. The small square indicates the location of
Polystichum lemmonii in British Columbia.
DOUGLAS: LEMMON’S HOLLY FERN IN CANADA 165
distinguished from the latter two species by the lack
of spines on the teeth of the ultimate segments of the
pinnae (Hitchcock et al. 1969; Wagner 1993; Ceska
2000).
North American and Provincial Ranges
Polystichum lemmonii ranges from south-central
British Columbia, sporadically south through Wash-
ington and Oregon to northern California (Smith and
Lemieux 1993; Wagner 1993). In Canada, it is known
only from the Baldy Mountain area in the Okanagan
River valley in south-central British Columbia (Figure
2; Ceska 2000; Douglas et al. 2002).
Habitat
In western North America, Polystichum lemmonii
occurs on sites where ferromagnesian or ultramafic
rocks outcrop (Kruckeberg 1969; Wagner 1993). There
are a number of ultramafic rock outcrops in western
British Columbia but only the two small, adjacent
ridges, at an elevation of 1900 m, in the Baldy Moun-
tain area support the latter species (Figure 3). These
dunite rock outcrop habitats are also characterized by
shallow soils thus creating xeric microclimates that
exclude many nearby species adapted to more mesic
microclimates or non-ultramafic soils (Figure 4). These
ridges, therefore, have a typically depauperate ultra-
mafic flora and lack a tree cover in contrast to the
FicureE 3. Aerial view of the ultramafic east ridge. Most Polystichum lemmonii plants occur on the north side
of these east-west oriented ridges. The west ridge is slightly longer.
166
surrounding montane forests. The most prominent
species on the ridge include Common Juniper (Juni-
perus communis), Indian’s Dream (Aspidotis densa),
Alpine Sandwort (Minuartia obtusiloba) and Yarrow
(Achillea millefolium).
Biology
There is a limited amount of information on the
biology and ecology of Polystichum lemmonii. The
ultramafic habitat, however, has been well-studied by
Kruckeberg (1969). Plants of ultramafic substrates
are adapted to tolerate low levels of calcium, nitro-
gen, phosphorus and molybdenum and high levels of
magnesium, chromium and nickel (Kruckeberg 1969).
Wagner (1979) has provided some genetic informa-
tion. P. lemmonii is a tetraploid (2n = 82) and thought
to be one of the parents of both P. kruckebergii and P.
scopulinum.
Sporophytes of P. lemmonii, as with most evergreen
fern species, often retain significant numbers of mature
spores over the winter that are then released the fol-
lowing spring (Farrar 1976). PR. lemmonii also grows
vegetatively by subterranean rhizome elongation
often resulting in large clumps of clones. Because of
the dry site conditions, which are not ideal for spore
germination or gamete fertilization, most reproduction
is probably by rhizome elongation (Walker 1979).
Prothalli were not observed at the site.
Long-distance dispersal of spores of P. lemmonii is
evident by the distance to the nearest locations of the
species in the adjacent state of Washington in the
United States. P. lemmonii occurs in the Twin Sisters
Range of Washington and in the Wenatchee Mountains
(Kruckeberg 1969), a distance of about 205 km to the
southwest and 225 km to the south of Baldy Moun-
tain, respectively. The Tulameen River ultramafic site,
where both P. kruckebergii and P. scopulinum occur
(Kruckeberg 1969; Douglas and Labrecque 2003%*),
does not contain P. lemmonii even though the Tula-
meen River site is halfway between Baldy Mountain
and the Twin Sisters Range. Reproduction of P. lem-
moni at the Baldy Mountain area is evident since about
30 percent of the 853 plants counted were relatively
young (plant tufts less than four cm wide).
Population Attributes
The population of P. lemmonii occurs on two adja-
cent, rocky ridges. The ridges, which are about 280 and
200 m long by 50 m wide, are separated by a distance
of 160 m. A 2001 count of all plants in the popula-
tion by the author revealed a total of 853 plants over
0.72 ha. A collection by D. M. Britton in 1987 (at
Department of Agriculture, Ottawa) mentions a popu-
lation size of “perhaps a thousand plants”. This would
indicate that the population has remained relatively
stable for at least 15 years.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Provincial, National and Global Ranks
The British Columbia Conservation Data Centre
has ranked this species as S1 and placed it on the
British Columbia Ministry of Sustainable Resource
Management Red-list (Douglas et al. 2002). This is
the most critical category for imperilled rare native
vascular plants in British Columbia. A rank of S1 is
considered “critically imperilled because of extreme
rarity (5 or fewer occurrences or very few remaining
individuals) or because of some factors making it
especially vulnerable to extirpation or extinction”
(Douglas et al. 2002). Since the species is restricted
to British Columbia, the National rank is N1. Globally,
Polystichum lemmonii is ranked G4 and is frequent to
common in its range and apparently secure.
Threats and Protection
The most direct threat to Polystichum lemmonii is
mining exploration. At the present time the entire
area is occupied by active mining claims and explora-
tion could occur with short notice. Additional threats
include the potential use of the rock outcrop for forest
road construction and the possibility of intense wild-
fires. Extremely high forest fuel loads in the the area
may lead to wildfires similar to that experienced in
the region in 2003. Introduced species are of no con-
cern at this site due to the ultramafic properties of the
soils.
The population in the Baldy Mountain area is on
public land but is not part of a protected area. It is
conceivable that this area could qualify as a Wildlife
Habitat Area but this status has yet to be proposed.
Polystichum lemmonii could be a candidate species
for protection under the provincial Wildlife Amend-
ment Act as it is currently Red-listed by the British
Columbia Conservation Data Centre.
Evaluation
The British Columbia Conservation Data Centre
considers Polystichum lemmonii to be threatened/en-
dangered in British Columbia (Douglas et al. 2002)
and the Committee on the Status of Endangered Wild-
life in Canada has assessed the species as threatened
(COSEWIC 2003). Just over 850 plants are known
from a single site in Canada at the Baldy Mountain
area of south-central British Columbia. The prognosis
for this species is not good since ultramafic rock out-
crops often attract mineral exploration and the entire
area is covered by active mineral claims. These rock
outcrops could also be of potential use as a quarry for
road building materials. The extremely high forest fuel
loads in the adjacent area could also support wildfires.
Establishment of a Wildlife Habitat Area and removal
of the active mineral claims would remove the major
threats at the site.
2004
DOUGLAS: LEMMON’S HOLLY FERN IN CANADA
167
FicureE 4. Polystichum lemmonii plants are conspicuous among the low vegetation on the ultramafic soils.
Acknowledgments
I would like to thank Kathy Paige for her partici-
pation in the fieldwork and Louise Bacon and Jenifer
Penny for office assistance. Graham Nixon, British
Columbia Geological Survey, kindly provided infor-
mation on ultramafic rock types.
Documents Cited (marked * in text)
COSEWIC. 2003. COSEWIC assessment and status report
on Lemmon’s holly fern Polystichum lemmonii in Canada.
Committee on the Status of Endangered Wildlife in Can-
ada. www.cosewic.gc.ca, Ottawa, Ontario. 13 pages
Douglas, G. W. 2003. COSEWIC Status report on Lemmon’s
holly fern Polystichum lemmonii in Canada, in COSEWIC
assessment and status report on Lemmon’s holly fern
Polystichum lemmonii in Canada. Committee on the Status
of Endangered Wildlife in Canada. www.cosewic.gc.ca,
Ottawa, Ontario. 13 pages.
Douglas, G. W., and J. Labrecque. 2003. COSEWIC Status
report on Mountain Holly Fern or Polystic des Rochers,
Polystichum scopulinum in Canada. Unpublished report.
Ottawa, Ontario. 20 pages.
Douglas, G. W. 2005. National Recovery Strategy for Lem-
mon’s Holly Fern (Polystichum lemmonii). In preparation.
Ottawa, Ontario.
Literature Cited
Ceska, A. 2000. Pteridophytes. Pages 260-343 in Illustrated
flora of British Columbia. Volume 5. Dicotyledons (Salica-
ceae through Zygophyllaceae) and Pteridophytes. Edited
by G. W. Douglas, D. Meidinger and J. Pojar. British
Columbia Ministry of Environment, Lands and Parks and
British Columbia Ministry of Forests. Victoria, British
Columbia. 427 pages.
Cody, W. J., and D. M. Britton. 1984. Polystichum lemmonii,
a rock shield-fern new to British Columbia and Canada.
Canadian Field-Naturalist 98: 375.
Cody, W. J., and D. M. Britton. 1989. Ferns and fern allies
of Canada. Agriculture Canada Research Branch, Publica-
tion 1829/E. Ottawa, Ontario. 430 pages.
Douglas, G. W., D. Meidinger, and J. L. Penny. 2002. Rare
native vascular plants of British Columbia. Second edition.
Province of British Columbia. Victoria, British Columbia.
359 pages.
Douglas, G. W., D. Meidinger, and J. Pojar. 2000. Illus-
trated flora of British Columbia. Volume 5. Dicotyledons
(Salicaceae through Zygophyllaceae) and Pteridophytes.
British Columbia Ministry of Environment, Lands and
Parks and British Columbia Ministry of Forests. Victoria,
British Columbia. 389 pages.
Douglas, G. W., G. B. Straley, and D. Meidinger. 1998a.
Illustrated flora of British Columbia. Volume 1. Gymno-
sperms and Dicotyledons (Aceraceae through Asteraceae).
British Columbia Ministry of Environment, Lands and
Parks and British Columbia Ministry of Forests. Victoria,
British Columbia. 436 pages.
Douglas, G. W., G. B. Straley, D. Meidinger, and J. Pojar.
1998b. Illustrated flora of British Columbia. Volume 2.
Dicotyledons (Balsaminaceae through Cuscutaceae). Bri-
168
tish Columbia Ministry of Environment, Lands and Parks
and Ministry of Forests. Victoria, British Columbia. 401
pages.
Farrar, D. L. 1976. Spore retention and release from over-
wintering fronds. American Fern Journal 66: 49-52.
Hitchcock, C. L., A. Cronquist, M. Ownbey, and J. W.
Thompson. 1969. Vascular plants of the Pacific Northwest.
Part 1. Vascular Cryptogams, Gymnosperms and Mono-
cotyledons. University Washington Press, Seattle, Wash-
ington. 914 pages.
Kruckeberg, A. R. 1969. Plant life on serpentine and other
ferromagnesian rocks in northwestern North America.
Syesis 2: 14-114.
Smith, A. R., and T. Lemieux. 1993. Dryopteridaceae. Pages
91-94 in The Jepson manual: Higher plants of California.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Edited by J. C. Hickman. University of California Press.
Berkeley, California. 1400 pages.
Wagner, D. H. 1979. Systematics of Polystichum in western
North America north of Mexico. Pteridologia 1: 1-64.
Wagner, D. H. 1993. Polystichum. Pages 290-299 in Flora
of North America North of Mexico — Volume 3. Magno-
liophyta: Magnoliidae and Hamamelidae. Edited by Flora
of North America Editorial Committee. Oxford University
Press Inc. New York, New York. 475 pages.
Walker, T. G. 1979. The cytogenetics of ferns. In The experi-
mental Biology of ferns. Edited by A. F. Dyer. Academic
Press, London, England.
Received 15 October 2002
Accepted 1 September 2004
Conservation Evaluation of the Pacific Population of Tall Woolly-heads,
Psilocarphus elatior, an Endangered Herb in Canada*
GEORGE W. DouGLas! and JEANNE M. ILLINGWORTH?
‘Conservation Data Centre, British Columbia Ministry of Sustainable Resource Management, Terrestrial Information Branch,
P.O. Box 9993 Stn Prov Govt, Victoria, British Columbia V8W 9R7 Canada
23537 Savannah Ave., Victoria, British Columbia V8X 1S6 Canada
Current address: Douglas Ecological Consultants Ltd., 6230 North Road, Duncan, British Columbia V9L 6K9 Canada
Douglas, George W., and Jeanne M. Illingworth. 2004. Conservation evaluation of the Pacific population of Tall Woolly-
heads, Psilocarphus elatior, an endangered herb in Canada. Canadian Field-Naturalist 118(2): 169-173.
In Canada, Psilocarphus elatior occurs in British Columbia, Alberta and Saskatchewan. This paper examines the status of
the Pacific populations located on southeastern Vancouver Island in southwestern British Columbia. The Pacific population
consists of 12 recorded sites of which only five have been confirmed since 1993. In British Columbia, P. elatior is
associated with dried beds of vernal pools and other open, moist depressions at lower elevations. In British Columbia, P.
elatior populations occur in large numbers at only two of the seven locations.
Key Words: Tall Woolly-heads, Psilocarphus elatior, endangered, distribution, population size, British Columbia.
Tall Woolly-heads, Psilocarphus elatior (A. Gray)
A. Gray” [Taxonomy and nomenclature follows Doug-
las (1998) and Douglas et al. (1998; 1999a, c; 2001a
b), is a member of a genus of five species which occur
in the Americas (Cronquist 1950). It is one of three
species occurring in British Columbia and Canada
(Douglas 1998).
Psilocarphus elatior is a small, erect, annual plant
up to 15 cm tall (Figure 1; Douglas 1995, 1998). The
opposite leaves are silky-hairy, linear-oblong, entire
on the margins and 1.2 to 3.5 mm long. The flowers
form solitary spherical heads in the leaf axils or at the
tips of the stems or leaf branches. The flowers lack
involucres but have involucral-like leaves at their bases.
Each of the outer (female) threadlike ray flowers has
a well developed, 2.4 to 3.8 mm long receptacle bract.
These bracts have a translucent appendage below the
summit.
In British Columbia, P. elatior may be distinguished
from Slender Woolly-heads (P. tenellus var. tenellus)
by its erect habit, larger heads and receptacular bracts.
In the field, young specimens of P. elatior may also be
confused with young specimens of Lowland Cudweed
(Gnaphalium palustre). Close examination will reveal
* Field work for the Psilocarphus elatior project was fund-
ed by the British Columbia Conservation Data Centre.
The results appear in the British Columbia Conservation
Data Centre database and a rare plant manual (Douglas et
al. 2002). These data formed the basis for a Committee on
the Status of Endangered Wildlife in Canada status report
(Douglas, et al. 1999b) and the subsequent assessment of
endangered (COSEWIC 2004*) for the Pacific population.
The present paper also includes more recent information
from research funded by the British Columbia Conserva-
tion Data Centre.
that most of the leaves of the latter are alternate and the
flower heads have densely woolly involucres, broader
ray flowers and a non-spherical shape.
North American and Provincial Ranges
Psilocarphus elatior ranges from southwestern Brit-
ish Columbia, southeastern Alberta and southwestern
Saskatchewan in Canada, south through Idaho, Wash-
ington and Oregon to northern California (Cronquist
1955; Scoggan 1979; Morefield 1993; Douglas 1998).
In British Columbia, it is restricted to south-eastern
Vancouver Island in south-western British Columbia
(Figure 2; Douglas 1998; Douglas et al. 2002).
Habitat
Psilocarphus elatior inhabits dried beds of vernal
pools, ephemeral lake edges (Figure 3) and other open
moist, often disturbed sites at lower elevations. The
sites are often level and generally slightly depressed.
Psilocarphus elatior is not found within particular
communities and often occupies sites where other spe-
cies are sparse. There does not appear to be a consis-
tent association with other plants.
The Somenos Lake locality near Duncan supports
the largest and most vigourous population of P. elatior
(Table 1). The plants grow on the moist shoreline of
the lake and appear when the lake level recedes in late
spring or early summer. Major associates at this site
include Slender-beaked Sedge (Carex athrostachya),
One-sided Sedge (C. unilateralis), Brass Buttons
(Cotula coronopifolia) and Skunkweed (Navarretia
squarrosa).
At Uplands Park, in the Municipality of Uplands
near Victoria, five subpopulations occur in a large
ephemeral meadow. Associated species include Bent-
grass (Agrostis sp.), California Oatgrass (Danthonia
169
170 THE CANADIAN FIELD-NATURALIST
Figure 1. Illustration of Psilocarphus elatior (line drawing
by Elizabeth J. Stephen in Douglas [1995, 1998]).
californica), Toad Rush (Juncus bufonis), Perennial
Ryegrass (Lolium perenne) and Small Hop-clover
(Trifolium dubium). Introduced species are more abun-
dant here than at the Somenos Lake site and appear
to be increasing yearly.
The Christmas Hill site, although smaller than the
previous two sites, is in relatively good condition.
Native species in this habitat include Carolina
Meadow-foxtail (Alopecurus carolinianus), Green-
sheathed Sedge (Carex feta), Heterocodon (Hetero-
codon rariflorum), and Scouler’s Popcornflower
(Plagiobothrys scouleri).
The two remaining populations, at Scafe Hill and
Cattle Point, occur in small depressions. These popu-
lations are probably the least stable of the extant pop-
ulations. The Cattle Point populations are absent dur-
ing some years but the seed bank appears to remain.
Psilocarphus elatior is considered to be a vernal
pool specialist (Keeley and Zedler 1998). They define
vernal pools as “precipitation-filled seasonal wetlands
inundated during periods when temperature is suffi-
cient for plant growth, followed by a brief water-
logged-terrestrial stage and culminating in extreme
desiccating soil conditions of extended duration”. The
Vol. 118
f ss
L PORT
VANCOUVER “iw ‘fp
ISLAND
O
UCLUELET
SIDNEY
FIGURE 2. The location and status of Psilocarphus elatior
sites in British Columbia (0 — extirpated sites, e — re-
cently confirmed sites, Hi — present status unknown).
species is able to outcompete grassland species due
to its tolerance of inundation and aquatic/wetland
species due to its tolerance of soil desiccation and heat
during summer drought.
Biology
Other than general habitat information, there is little
in the literature regarding the biology and ecology of
Psilocarphus elatior. It is likely, however, that this
plant shares many of the same traits that are typical
of the genus.
2004
DOUGLAS AND ILLINGWORTH: PACIFIC POPULATION OF TALL WOOLLY-HEADS 17]
Ficure 3. A dense population of Psilocarphus elatior on the edge of Somenos Lake. The prominent sedge is Carex athrostachya.
This site is usually submerged until late spring.
Lack of structures attractive to insects and animals,
and an interpretation of the floral structure indicate
these inconspicuous, woolly annuals may self-polli-
nate. Cronquist (1950) suggested that in the genus
Psilocarphus, the position of the receptacular bracts,
together with the position of the corolla and stigmas,
effectively guide these latter structures towards the
central flowers. Since it is the central flowers alone that
produce pollen, and since the wool and leaves sur-
rounding the head appeared to prevent pollen loss by
wind, self-pollination is indicated. It is also possible
that pollen may not be essential for seed-production
and that asexual reproduction may be occurring, al-
though chromosome counts would be necessary to
verify this.
Seed dispersal also appears limited. Since the ach-
enes are much smaller than the enclosing bracts, the
only obvious means of dispersal is by water or wind.
Table 1. Locations and Population Sizes for Psilocarphus elatior in British Columbia.
Collection Site Last
Observation
Cloverdale (Victoria) 1887
Cedar Hill (Victoria) 1887
Ucluelet 1909
Roberts Bay (Sidney) 1913
Swartz Bay (Sidney) 1931
Francis-King Regional Park (Victoria) 1962
University of Victoria (Victoria) 1966
Cattle Point, Uplands Park (Victoria) 1993
Scafe Hill (Victoria) 1996
Uplands Park (Victoria) 1998
Christmas Hill (Victoria) 2001
Somenos Lake (Duncan) 2002
Collector/ Population
Observer (no./area)
Macoun Extirpated
Macoun Extirpated
Macoun Extirpated
Macoun Extirpated
Groh Extirpated
Melburn Unknown
Turner Extirpated
Ryan 200/10 m?
Roemer 20/? m?
Douglas 40 000+/1 200+ m?
Douglas & Penny 450/72 m?
Douglas & Douglas 100 000+/45 m?
172
The plant’s habitat in vernal pools may also permit the
bracts and achenes to be transferred by the muddy
feet of waterfowl and other animals (Cronquist 1950).
Further studies are required to determine many as-
pects of the population dynamics of P. elatior includ-
ing the average life-cycle of the species, the frequency
and requirements for seed germination and survival,
and its competitive ability with other species.
Population Attributes
Psilocarphus elatior has been recorded from 12 sites
in southwestern British Columbia (Table 1). Five of
these have been confirmed since 1993. The status of
the remaining populations is unknown and many are
believed extirpated. Population areas range from 10 m?
to over 1200 m? while numbers of plants range from
20 to over 100 000. In the majority of cases, popula-
tion trend analysis is not available because of limited
demographic data.
Provincial, National and Global Ranks
Provincially, P. elatior is ranked S2 by the British
Columbia Conservation Data Centre (Douglas et al.
2002) which indicates this species to be “imperiled
because of rarity (typically 6-20 extant occurrences or
few remaining individuals) or because of some fac-
tor(s) making it vulnerable to extirpation or extinction.”
Nationally the species is ranked N3, while globally
it has a rank of G5. The latter rank indicates it is
“frequent to common to very common; demonstrably
secure and essentially ineradicable under present con-
ditions”.
Threats and Protection
Habitat destruction is the greatest threat to the exist-
ing populations of Psilocarphus elatior. Some sites
occur in areas subjected to heavy pedestrian tram-
pling or are at risk from private development. Threats
to the continued survival of this species are compound-
ed by the lack of biological and ecological information
which create difficulties in site management.
Four of the P. elatior populations are partially pro-
tected by their location in municipal or regional parks
or special protected areas (Somenos Lake). The latter
probably has the greatest degree of protection since it
is administered by British Columbia Parks and falls
under the Park Act. Most of the municipal or regional
parks receive little active management at the present
time, at least with respect to their rare plants. Park
enhancement projects, road and trail developments and
heavy recreational use by humans often result in the
destruction of the native vegetation and rare plant spe-
cies. Psilocarphus elatior could be a candidate species
for protection under the provincial Wildlife Amendment
Act as it is currently Red-listed by the British Colum-
bia Conservation Data Centre (Douglas et al. 2002).
Most of the populations contain small numbers of
plants. Once a population becomes small, it becomes
THE CANADIAN FIELD-NATURALIST
Vol. 118
more susceptible to demographic and environmental
variation and loss of genetic variability. In some cases,
small populations are at risk of inbreeding depres-
sion, genetic drift and loss of fitness (Primack 1998).
Evaluation
The British Columbia Conservation Data Centre
considers Psilocarphus elatior to be threatened/endan-
gered in British Columbia (Douglas et al. 2002a) and
the Committee on the Status of Endangered Wildlife
in Canada has assessed the species as endangered
(COSEWIC 2003). Most of the populations are small
and not viable. With limited knowledge of the plants
biological and ecological requirements, this species is
vulnerable to extirpation in British Columbia. Without
research on growth requirements and further demo-
graphic information, the stability of the present popu-
lations will remain unknown. Studies are also neces-
sary to determine if the present habitats are necessary
for the successful growth of P. elatior or if these plants
are simply outcompeted elsewhere. The limited num-
ber of individuals also reduces the potential for gen-
etic variation which may be necessary to respond to
environmental changes in the future.
Acknowledgments
We thank Sylvia Douglas, Jenifer Penny, and
Michael Ryan for their field assistance.
Documents Cited (marked * in text)
COSEWIC. 2004. Canadian Species at Risk. Committee on
the Status of Endangered Wildlife in Canada.
www.cose wic.gc.ca, Ottawa, Ontario. 13 pages.
Douglas, G. W., J. Gould, and J. M. Illingworth. 1999. Status
report on the Tall woolly-heads, Psilocarphus elatior (A.
Gray) A. Gray. Unpublished report. Committee on the
Status of Endangered Wildlife in Canada, Ottawa. 19 pages.
Literature Cited
Cronquist, A. 1950. A review of the genus Psilocarphus.
Research Studies of the State College of Washington 18:
71-89.
Cronquist, A. 1955. Vascular plants of the Pacific Northwest.
Part 5: Compositae. University of Washington Press, Seat-
tle, Washington. 343 pages.
Douglas, G. W. 1995. The sunflower family (Asteraceae) of
British Columbia. Volume 2 — Astereae, Anthemideae,
Eupatoreae and Inuleae. Royal British Columbia Museum,
Victoria, British Columbia. 393 pages.
Douglas, G. W. 1998. Asteraceae. Pages 96-392 in Illustrat-
ed flora of British Columbia. Volume 1. Gymnosperms and
Dicotyledons (Aceraceae through Asteraceae). Edited by
G. W. Douglas, G. B. Straley, D. Meidinger, and J. Pojar.
British Columbia Ministry of Environment, Lands and
Parks and British Columbia Ministry of Forests, Victoria,
British Columbia.
Douglas, G. W., D. Meidinger, and J. L. Penny. 2002. Rare
native vascular plants of British Columbia. Second edition.
Province of British Columbia, Victoria, British Columbia.
358 pages.
2004
Douglas, G. W., D. Meidinger, and J. Pojar. 1999a. Illus-
trated flora of British Columbia. Volume 3. Dicotyledons
(Diapensiaceae through Onagraceae). British Columbia
Ministry of Environment, Lands and Parks and British
Columbia Ministry of Forests, Victoria, British Columbia.
Douglas, G. W., D. Meidinger, and J. Pojar. 1999b. Illus-
trated flora of British Columbia. Volume 4. Dicotyledons
(Orobanchaceae through Rubiaceae). British Columbia
Ministry of Environment, Lands and Parks and British Col-
umbia Ministry of Forests, Victoria, British Columbia.
427 pages.
Douglas, G. W., D. Meidinger, and J. Pojar 2001a. Illus-
trated flora of British Columbia. Volume 6. Monocotyle-
dons (Acoraceae through Najadaceae). British Columbia
Ministry of Sustainable Resource Management and British
Columbia Ministry of Forests, Victoria, British Colum-
bia. 361 pages.
Douglas, G. W., D. Meidinger, and J. Pojar 2001b. Ilus-
trated flora of British Columbia. Volume 7. Monocotyle-
dons (Orchidaceae to Zosteraceae). British Columbia
Ministry of Sustainable Resource Management and British
Columbia Ministry of Forests, Victoria, British Columbia.
379 pages.
Douglas, G. W., G. B. Straley, D. Meidinger, and J. Pojar.
1998. Illustrated flora of British Columbia. Volume 1.
DOUGLAS AND ILLINGWORTH: PACIFIC POPULATION OF TALL WOOLLY-HEADS
173
Gymnosperms and Dicotyledons (Aceraceae through
Asteraceae). British Columbia Ministry of Environment,
Lands and Parks and British Columbia Ministry of Forests,
Victoria, British Columbia. 436 pages.
Keeley, J. E., and P. H. Zedler. 1998. Characterization and
global distribution of vernal pools. /n Ecology, conserva-
tion, and management of vernal pool ecosystems: Proceed-
ings from a 1996 Conference. Edited by C. W. Witham,
E. T. Bauder, D. Belk, W. R. Ferren Jr., and R. Ornduff.
California Native Plant Society. Sacramento, California.
Morefield, J. 1993. Psilocarphus. Page 329 in The Jepson
manual: higher plants of California. Edited by J. C. Hick-
man. University of California Press, Berkeley, California.
1400 pages.
Primack, R. B. 1998. Essentials of Conservation Biology.
24 Edition. Sinauer Associates Inc. Sunderland, Massa-
chusetts.
Scoggan, H. J. 1979. The flora of Canada. Part 4 — Dico-
tyledoneae (Loasaceae to Compositae. National Museum
of Natural Sciences, Ottawa, Ontario. Publication in Botany
Number 7. Pages 1117-1711.
Received 15 October 2002
Accepted | September 2004
Conservation Evaluation of Howell’s Triteleia, Triteleia howellii, an
Endangered Lily in Canada*
GEORGE W. DouGLas!:? and JENIFER L. PENNY!
‘Conservation Data Centre, British Columbia Ministry of Sustainable Resource Management, Terrestrial Information
Branch, P.O. Box 9993 Stn Prov Govt, Victoria British Columbia V8W 9R7 Canada
? Current address: Douglas Ecological Consultants Ltd., 6230 North Road, Duncan, British Columbia V9L 6K9 Canada
Douglas, George W., and Jenifer L. Penny. 2004. Conservation evaluation of Howell’s Triteleia, Triteleia howellii, an
endangered lily in Canada. Canadian Field-Naturalist 118(2): 174-178.
In Canada, Triteleia howellii is restricted to Quercus garryana stands and grass-dominated meadows on southeastern Van-
couver Island in southwestern British Columbia. Nine sites have been confirmed in recent years while three other sites are
considered extirpated. These Canadian sites represent the northern range limits of 7: howellii. Threats to existing populations
vary in intensity. Although most populations are protected to a certain extent from direct habitat destruction, introduced species
pose a serious potential threat to the continued existence of most populations. Managing sites for 7: howellii is difficult because
little information is available regarding the general biology of this species.
Key Words: Howell’s Triteleia, Triteleia howellii, endangered, distribution, population size, British Columbia.
Howell’s Triteleia, Triteleia howellii (S. Wats.)
Greene [taxonomy and nomenclature follow Douglas
et al. (1998a, b; 1999a, b; 2000, 2001a, b)], some-
times treated as T. grandiflora Lindl. var. howellii (S.
Wats.) Hoover, is a member of a genus of 14 species
in North America (Keator 1993). Three species occur
in British Columbia and Canada (Scoggan 1979; Pojar
2001).
Triteleia howellii is a perennial herb from a deep,
straw-coloured, fibrous-scaly, nearly globe-shaped,
bulb-like corm (Figure 1; Pojar 2001). The erect, flow-
ering stem is 20-50 cm tall with one or two smooth,
slender, linear basal leaves. The leaves are 20-40 cm
long, 3-8 mm wide, sheathed at the base and have en-
tire margins. The flowers consist of six whitish to blue,
vase-shaped to narrowly bell-shaped, fused segments
forming a 1.5-2 cm long tube. The corolla lobes, which
are about as long as the tube, are in two, spreading,
petal-like whorls, about as long as the tube. The outer
three are broadly lanceolate, the inner three are oblong-
egg-shaped and all are slightly ruffled. The fruit con-
sists of a stalked, egg-shaped capsule containing black
rounded seeds.
Triteleia howellii is similar in appearance to its close
relative 7: grandiflora. It is distinguished from the latter
* The field work for the Triteleia howellii project was funded
by the British Columbia Conservation Data Centre. The
results appear in the British Columbia Conservation Data
Centre database and a rare plant manual (Douglas et al.
2002). This information formed the basis for a Committee
on the Status of Endangered Wildlife in Canada status
report (Douglas 2003*) and the subsequent assessment of
Endangered (COSEWIC 2003*). The present paper also
includes more recent information, funded by the Nature
Conservancy of Canada and the Habitat Conservation Trust
Fund, that will be used in a National Recovery Strategy
for T: howellii (Douglas and Smith 2005).
by its flat filaments which are attached at the same level
on the perianth tube (Pojar 2001). The filaments of 7:
grandiflora, in contrast, are not flat and are attached
at two levels on the perianth tube.
North American and Provincial Ranges
Triteleia howellii ranges from southwestern British
Columbia, south through Washington and Oregon to
northern California (Barkworth 1977a; Keator 1993).
In Canada, 7: howellii is known only from southeast-
ern Vancouver Island (Figure 2; Pojar 2001; Douglas
et al. 2002).
Habitat
In British Columbia T- howellii occurs on rock out-
crops, in Garry Oak (Quercus garryana) woodlands,
Garry Oak/Arbutus (Arbutus menziesii) stands and
occasionally in highly disturbed sites dominated by
weeds in private yards and on roadsides. In the highly
disturbed sites, dominants include Orchard Grass (Dac-
tylis glomerata), Cheat Grass (Bromus tectorum), Com-
mon Vetch (Vicia sativa), Rip-gut Brome (Bromus
rigidus), Soft Brome (B. hordeaceus), Perennial Rye-
grass (Lolium perenne), and Pacific Sanicle (Sanicula
crassicaulis var. crassicaulis), all introduced except
for Sanicula.
At the highest quality site, in the Quercus garryana
woodland at the Cowichan Garry Oak Preserve, the
habitat is classified as a Quercus garryana/Dactylis
glomerata plant community (Douglas et al. 2002*)
and is characterized by deep, dark soils up to a metre in
depth. It is likely that prior to understory dominance
by D. glomerata in this (Figure 3), and other Quercus
stands of the region, this plant community would have
fallen within the Q. garryana/California Brome (Bro-
mus carinatus) community type (Roemer 1972). An
174
2004
FiGure 1. Illustration of Triteleia howellii (Line drawing in
Pojar 2001).
extremely rich low shrub and herb stratum is present
during the spring. The most prominent species in the
Cowichan Garry Oak Preserve Garry Oak stand are
Sanicula crassicaulis var. crassicaulis and Dactylis
glomerata (Douglas et al. 2002*). Other species with
DOUGLAS AND PENNY: HOWELL’S TRITELEIA IN CANADA
Wes
x
Ay 9
Fie: \ comoxS SER 3
ie Nil ¢
AV f =, South
g T Wellington
NANAIMO*\4>
\
VANCOUVER
ISLAND
FiGureE 2. Distribution of Triteleia howellii in British Col-
umbia (o — extirpated sites, e — recently confirmed
sites).
moderate to high constancies associated with T. how-
ellii include Common Camas (Camassia quamash),
Bromus spp., Broad-leaved Shooting-star (Dodecatheon
hendersonii_ ssp. hendersonii), Cleavers (Galium
aparine), and Common Snowberry (Symphoricarpos
albus). A marked change in composition takes place
by mid-summer. Many of the conspicuous native plants
(e.g., Great Camas (Camassia leichtlinii), C. quamash,
Dodecatheon hendersonii, and Yellow Montane Violet
(Viola praemorsa ssp. praemorsa)) have completed
their yearly life cycle and have essentially disappeared.
Perennial grasses that were not recognizable or had
not initiated growth in the spring and numerous intro-
176
THE CANADIAN FIELD-NATURALIST
TABLE |. Locations and population sizes for Triteleia howellii in Canada
Collection Last
Site Observation
Oak Bay (Victoria) 1912
Saanich Arm (Victoria) 1919
Witty’s Lagoon Regional Park (Metchosin) 1999
Gordon Head (Saanich) 1999
Cowichan Garry Oak Preserve (Duncan) 1999
Cowichan River Estuary (Duncan) 2001
Thetis Lake Regional Park (View Royal) 2002
Uplands Park (Victoria) 2003
Mt. Tzuhalem, base of (along Khenipsen Road) 2003
Albert Head Lagoon Regional Park (Metchosin) 2003
Horth Hill Regional Park (North Saanich) 2003
Beacon Hill Park (Victoria) 2004
Somenos Lake (Duncan) 2004
Williams Head Road (Metchosin) 2004
duced annuals, well adapted to the drier soils, domi-
nate the understory. At this time, Dactylis glomerata
and Vicia species are the most prominent species
with greatly increased mean covers. Other prominent
species in mid-summer include the native grasses,
Bromus carinatus and Alaska Oniongrass (Melica
subulata), and the introduced grasses, Barren Brome
(Bromus sterilis) and Kentucky Bluegrass (Poa pra-
tensis).
Triteleia howellii also occurs in a Quercus garryana
— Arbutus menziesii stand. The shrub layer is more
prominent at this site and is dominated by Tall Oregon-
grape (Mahonia aquifolium) and Oceanspray (Holo-
discus discolor). Major associates include Hairy
Honeysuckle (Lonicera hispidula), Bromus rigidus,
Galium aparine, Small-flowered Nemophila (Nemo-
phila parviflora) and Hedgehog Dogtail (Cynosurus
echinatus).
Biology
There is little information known about the biology
or ecology of Triteleia howellii throughout its range.
Reproduction is by division of the corm, by produc-
tion of numerous cormlets, and by seed (Barkworth
1977b).
Population Attributes
Triteleia howellii has been collected at 14 sites in
Canada, all of which are located on southeastern
Vancouver Island (Table 1). Of the 14 sites, 11 have
been confirmed since 1999 while the status of the re-
maining three sites is unknown and are likely extir-
pated. Population areas range from small (one m7) to
over three or four hectares, while plant numbers range
from a single plant to over 430 plants (Table 1). Little
information is available on population trends. The sites
that have recently been examined show the populations
Vol. 118
Collector/ Population
Observer (no./area)
Beaven Extirpated
Newcombe Extirpated
Douglas & Penny 43/200 m?
Fontaine 51/5 m?
Douglas 430/3-4 ha
Douglas 62/3 m?
Ceska 1/1 m?*
Penny & Fairbarns Not seen since 1917,
2003 search
unsuccessful, probably
extirpated
Janszen 6/.05 m?*
Roemer 8/2 m?
Janszen 3/1 m?*
Fairbarns ca 200/12 m?
Douglas & Richards 90/140 m?
Milne 14/?m?
are apparently stable although numbers of flowering
plants may vary.
Provincial, National and Global Ranks
The British Columbia Conservation Data Centre has
ranked this species S2 and placed it on the British
Columbia Ministry of Sustainable Resource Manage-
ment red-list (Douglas et al. 2002). This is the most
critical category for imperilled rare native vascular
plants in British Columbia. A rank of S2 is consid-
ered “critically imperilled because of rarity (typically
6-20 extant occurrences or few remaining individuals)
or because of some factor(s) making it vulnerable to
extirpation or extinction.” Since the species is restrict-
ed to British Columbia, the National rank is N2. Glo-
bally, Triteleia howellii is ranked G3G4, indicating
that, although the presently known sites are less than
100, it is more likely that this species is frequent to
common in its range and apparently secure.
Threats and Protection
The most direct and immediate threat to Triteleia
howellii is habitat destruction. This is of particular con-
cern in the grass-dominated meadows often associ-
ated with the Quercus garryana communities that are
restricted to the southeastern side of Vancouver Island
and some of the Gulf Islands. This type of vegetation
was much more common before colonization by
European settlers. This destruction has continued to
the present resulting in the elimination of almost all
sites occurring outside parks or ecological reserves.
Historically, Q. garryana communities and grass-
dominated meadows have always been heavily influ-
enced by human activity, especially fires. Roemer
(1972) believed that without human interference some
of these stands would have eventually been replaced
by Douglas-fir forests.
2004
DOUGLAS AND PENNY: HOWELL’S TRITELEIA IN CANADA
177
FiGure 3. Habitat of Triteleia howellii in a Quercus garryana stand in the Cowichan Garry Oak Preserve near Quamichan
Lake. Dactylis glomerata is the dominant grass in this late summer photo.
The suppression of fire within the past century may
also have contributed to the decrease of Triteleia how-
ellii populations. Most of the sites in which T: howellii
has been collected were likely maintained in the past
as a result of periodic fires, both natural and unnatural.
In the past, aboriginal peoples probably set fire to
these stands to maintain them as an important habitat
for wildlife (Roemer 1972). Since that time, these sites
have experienced little disturbance, resulting in the in-
vasion and expansion of many other species, especial-
ly introducted grasses.
The introduction of European species has resulted
in substantial, and probably irreversible, changes not
only to the grass-dominated meadows associated with
Quercus garryana, but also to the rocky xeric sites
north and west of Victoria where Triteleia howellii
has been collected in the past. One of the most devas-
tating species is Scotch Broom (Cytisus scoparius),
which has become a dominant shrub on xeric, exposed
sites throughout much of southeastern Vancouver
Island and the Gulf Islands. Much of the vegetation
is now dominated by introduced grasses. These species
include Early Hairgrass (Aira praecox), Sweet Vernal-
grass (Anthoxanthum odoratum), Cynosurus echinatus
and Dactylis glomerata.
Some of the populations contain very few plants.
Once a population becomes small, it becomes more
vulnerable to demographic and environmental vari-
ation and loss of genetic variability. In some cases,
small populations are at risk of inbreeding depression,
genetic drift and loss of fitness (Primack 1998).
The population with the best protection is located at
the Cowichan Garry Oak Preserve where the general
public is excluded. This five-hectare stand near Quami-
chan Lake on Vancouver Island represents the best
example of a Quercus garryana woodland in the prov-
ince and probably one of the best in the Pacific North-
west. The stand contains a relatively low number of
exotic species and has active management plans in
place. This site also contains the largest known popu-
lation of T; howellii in the province (Douglas et al.
2002*).
A number of Triteleia howellii populations are also
in small regional parks in the Greater Victoria area.
These include populations at Beacon Hill, Witty’s
Lagoon, Thetis Lake, and Horth Hill. Most of these
parks receive little active management at the present
time, at least with respect to their rare plants. Park
enhancement projects, road and trail developments
and heavy recreational use by humans often result in
the destruction of the native vegetation and rare plant
species.
Triteleia howellii could be a candidate species for
protection under the provincial Wildlife Amendment
178
Act as it is currently red-listed by the British Colum-
bia Conservation Data Centre. One of the populations
(Somenos Lake) of T: howellii is protected by the Park
Act since it is currently administered by Parks BC.
Evaluation
The British Columbia Conservation Data Centre
considers Triteleia howellii to be threatened/endangered
in British Columbia (Douglas et al. 2002a) and the
Committee on the Status of Endangered Wildlife in
Canada has assessed the species as endangered
(COSEWIC 2003). About 1000 flowering plants have
been recorded in recent years from 11 locations. Only
four of these populations can be considered viable since
the remaining populations cover areas of less than 5 m?.
The prognosis for this species may not be good since,
since only one population, at the Cowichan Garry Oak
Preserve, is included in an active management plan.
Acknowledgments
We thank Sharon Hartwell, Marie Fontaine, and
Lora May Richards for their assistance with field work.
We also thank Adolf and Oluna Ceska, Matt Fairbarns,
Moralea Milne and Hans Roemer for information on
populations at several sites.
Documents Cited
COSEWIC. 2003. COSEWIC assessment and status report
on Howell’s Triteleia, Triteleia howellii in Canada. Com-
mittee on the Status of Endangered Wildlife in Canada.
www.cosewic.gc.ca, Ottawa, Ontario. 16 pages
Douglas, G. W. 2003. COSEWIC Status report on Howell’s
Triteleia, Triteleia howellii in Canada, in COSEWIC as-
sessment and status report on Howell’s Triteleia, Triteleia
howellii in Canada. Committee on the Status of Endan-
gered Wildlife in Canada. www.cosewic.gc.ca, Ottawa,
Ontario. 16 pages.
Douglas, G. W., J. L. Penny, and R. E. Maxwell. 2002b.
Composition, phenology, stand structure and soils of a
Quercus garryana (Garry Oak) woodland community at
Quamichan Lake, Vancouver Island, British Columbia.
British Columbia Conservation Data Centre, Ministry of
Sustainable Resource Management, Victoria, British
Columbia. 52 pages.
Douglas, G. W., and S. J. Smith. 2005. National multi-species
recovery strategy for species at risk in Garry Oak wood-
lands. In preparation. Ottawa, Ontario.
Literature Cited
Barkworth, M. E. 1977a. The taxonomic status of Brodi-
aea howellii Watson (Liliaceae). Northwest Science 51:
139-148.
Barkworth, M. E. 1977b. Intraspecific variation in Brodi-
aea douglasii Watson (Liliaceae). Northwest Science 51:
79-90.
Douglas, G. W., D. Meidinger, and J. L. Penny. 2002a.
Rare native vascular plants of British Columbia. Second
edition. Province of British Columbia. Victoria, British
Columbia. 359 pages.
Douglas, G. W., D. Meidinger, and J. Pojar. 1999a. Illus-
trated flora of British Columbia. Volume 3. Dicotyledons
THE CANADIAN FIELD-NATURALIST
Vol. 118
(Diapensiaceae through Onagraceae). British Columbia
Ministry of Environment, Lands and Parks and British
Columbia Ministry of Forests, Victoria, British Colum-
bia. 423 pages.
Douglas, G. W., D. Meidinger, and J. Pojar. 1999b. Illus-
trated flora of British Columbia. Volume 4. Dicotyledons
(Orobanchaceae through Rubiaceae). British Columbia
Ministry of Environment, Lands and Parks and British
Columbia Ministry of Forests, Victoria, British Colum-
bia. 427 pages.
Douglas, G. W., D. Meidinger, and J. Pojar. 2000. Illus-
trated flora of British Columbia. Volume 5. Dicotyledons
(Salicaceae to Zygophyllaceae) and Pteridophytes. British
Columbia Ministry of Environment, Lands and Parks and
British Columbia Ministry of Forests, Victoria, British
Columbia. 389 pages.
Douglas, G. W., D. Meidinger, and J. Pojar. 2001a. Illus-
trated flora of British Columbia. Volume 6. Monoco-
tyledons (Acoraceae to Najadaceae). British Columbia
Ministry of Environment, Lands and Parks and British
Columbia Ministry of Forests. Victoria, British Columbia.
361 pages.
Douglas, G. W., D. Meidinger, and J. Pojar. 2001b. Illus-
trated flora of British Columbia. Volume 7. Monocotyle-
dons (Orchidaceae to Zosteraceae). British Columbia
Ministry of Sustainable Resource Management and British
Columbia Ministry of Forests, Victoria, British Columbia.
379 pages.
Douglas, G. W., G. B. Straley, and D. Meidinger. 1998a.
Illustrated flora of British Columbia. Volume 1. Gymno-
sperms and Dicotyledons. (Aceraceae through Astera-
ceae). British Columbia Ministry of Environment, Lands
and Parks and British Columbia Ministry of Forests,
Victoria, British Columbia. 436 pages.
Douglas, G. W., G. B. Straley, D. Meidinger, and J. Pojar.
1998b. Illustrated flora of
British Columbia. Volume 2. Dicotyledons. (Balsaminaceae
through Cuscutaceae). British Columbia Ministry of Envi-
ronment, Lands and Parks and British Columbia Ministry
of Forests, Victoria, British Columbia. 401 pages.
Keator, G. 1993. Triteleia. Pages 1206-1208. In The Jepson
manual: Higher plants of California. Edited by J. C.
Hickman. University of California Press. Berkeley, Cali-
fornia. 1400 pages.
Pojar, J. 2001. Liliaceae. Pages 270-318. Jn Illustrated flora
of British Columbia. Volume 6. Monocotyledons (Acora-
ceae to Najadaceae). Edited by G. W. Douglas, D. Meid-
inger, and J. Pojar. British Columbia Ministry of Environ-
ment, Lands and Parks and British Columbia Ministry of
Forests, Victoria, British Columbia. 361 pages.
Primack, R. B. 1998. Essentials of Conservation Biology.
2™4 Edition. Sinauer Associates Inc. Sunderland, Massa-
chusetts.
Roemer, H. L. 1972. Forest vegetation and environments of
the Saanich Peninsula, Vancouver Island. Ph.D. thesis. Uni-
versity of Victoria, Victoria, British Columbia. 405 pages.
Scoggan, H. J. 1979. The flora of Canada. Part 4. Dicotyle-
doneae (Loasaceae to Compositae). National Museum of
Natural Sciences, Ottawa, Ontario. National Museum of
Natural Sciences Publications in Botany (7): 1117-1710.
Received 15 October 2002
Accepted | September 2004
Conservation Evaluation of Small-flowered Lipocarpha, Lipocarpha
micrantha (Cyperaceae), in Canada
TYLER W. SmITH!, GEORGE W. DOUGLAS? AND ALLAN G. HARRIS?
'Royal Botanical Gardens, P. O. Box 399, Hamilton, Ontario L8N 3H8 Canada
Present address: Plant Science, McGill University, Raymond Building, 21 111 Lakeshore Road, Ste. Anne de Bellevue,
Quebec H9X 3V9 Canada
Conservation Data Centre, British Columbia Ministry of Sustainable Resource Management, Terrestrial Information
Branch, P. O. Box 9993 Station Provincial Government, Victoria, British Columbia, V8W 9R7 Canada
Present address: Douglas Ecological Consultants Ltd., 62030 North Road, Duncan, British Columbia V9L 6K5 Canada
3Northern Bioscience, 136 S. Hill Street, Thunder Bay, Ontario P7B 3V1 Canada
Smith, Tyler W., George W. Douglas, and Allan G. Harris. 2004 Conservation Evaluation of Small-flowered Lipocarpha,
Lipocarpha micrantha (Cyperaceae), in Canada. Canadian Field-Naturalist 118(2): 179-184.
In Canada, Lipocarpha micrantha has been documented at eight locations in Quebec, Ontario, and British Columbia. Four of
these populations have apparently been extirpated. The remaining populations, ranging from 120 to approximately 40000
plants, are all northern disjuncts from the main range of this species. Threats to these populations include water level
regulation and shoreline development. Considering the threats to the habitat of Lipocarpha micrantha, and the small size of
most of the remaining populations, it has been designated an Endangered species in Canada.
Key Words: Small-flowered Lipocarpha, Lipocarpha micrantha, British Columbia, Ontario, Quebec, endangered, distribution,
population size.
Small-flowered Lipocarpha, Lipocarpha micrantha
(Vahl.) G. Tucker, is the only member of a mainly trop-
ical genus to occur in Canada. While it appears under
this name in the Flora of North America (Tucker 2002),
some recent treatments place it in the genus Hemicar-
pha Nees (Gleason and Cronquist 1991). Lipocarpha,
including Hemicarpha, is generally accepted as a dis-
tinct genus. However, taxonomic clarification of closely
related genera in the Cyperaceae may require nomen-
clatural revisions, pending the outcome of ongoing
research (Muasya et al. 2002).
Lipocarpha micrantha is a caespitose annual sedge,
2-20 cm tall with narrow (0.5 mm) leaves up to 10 cm
long. The 1 to 3 subsessile flower spikes are borne at
the top of the stem. The spikes are ovoid, 2—6 mm long,
with numerous perfect flowers concealed behind spi-
rally imbricate scales. The inflorescence is subtended
by 2 to 3 leaf-like bracts, the lowest of which looks
like a continuation of the stem (Figure 1: Hitchcock
et al. 1969; Gleason and Cronquist 1991; Douglas
and Ceska 2001; Tucker 2002).
The densely tufted plants resemble the seedlings of
many other sedge species that occur in the same habitat.
In Canada Lipocarpha micrantha is perhaps most simi-
lar in aspect to Awned Cyperus (Cyperus squarrosus
L.), another small annual sedge. Lipocarpha micrantha
is distinguished from this and all other Cyperus spe-
cies by its spirally arranged flowers.
Biology
Lipocarpha micrantha is only visible during a short
period each year. It germinates in late summer, when
dropping water levels expose the open sandy habitat
it requires. Flowering and fruiting occur in August and
September. High water levels may prevent germination
from occurring, with the population remaining dormant
until appropriate conditions occur. We do not know
how long dormant seeds may remain viable, but field
observations suggest they can persist at least two years.
Migrating waterfowl may be a vector for long-distance
dispersal.
Distribution
Lipocarpha micrantha ranges from Brazil to Canada.
North of Mexico, the main range extends from Texas,
north to northwestern Ontario, and east to the east coast
of the United States. Disjunct populations have been
recorded east and west of the main range, in Alabama,
Arizona, British Columbia, California, Florida, Ken-
tucky, Maine, New Mexico, New York, North Carolina,
and Quebec (Tucker 2002).
In Canada, Lipocarpha micrantha occurs at Osoyoos
Lake and Okanagan Lake in British Columbia (Figure
2), and at Rainy Lake and Lake of the Woods in north-
western Ontario (Figure 3). Populations along the De-
troit River in southern Ontario and along the north shore
of Lake Champlain in Quebec have been extirpated.
Habitat
Lipocarpha micrantha grows on sandy beaches and
interdunal swales that are subject to seasonal flooding,
but are protected from high waves or strong currents.
It is usually found in areas of very sparse vegetation,
and apparently is intolerant of competition from other
plant species. These habitat conditions are maintained
by fluctuating water levels. While Lipocarpha micrantha
179
180
THE CANADIAN FIELD-NATURALIST
Vol. 118
Ficure 1. Illustration of Lipocarpha micrantha (Line drawing by permission from Hitchcock et al. 1969).
requires seasonal low water levels to germinate and
flower, periodic high water is required to prevent
more vigorous species from dominating its shoreline
habitat (see Keddy and Reznicek 1986 for a discussion
of the relationship between water level fluctuations
and wetland vegetation).
Common associates of Lipocarpha micrantha in-
clude a variety of Cyperus, Bidens, and Salix species.
Cyperus squarrosus has been noted as an associate at
every station in Canada.
Population Trends and Limiting Factors
Of eight documented populations (Ceska and Ceska
1980; Oldham and Crins 1988; Sabourin et al. 1992*;
Oldham 1996; Harris et al. 2000*; Oldham 2000; Smith
et al. 2002*) of Lipocarpha micrantha in Canada,
only four persist (Table 1).
The Lake Champlain population, in Missisquoi Bay,
Quebec, was discovered in 1953 (Louis-Alphonse
3458, specimen at MT; herbarium acronyms follow
Holmgren et al. 2003*), and was documented through-
out the 1950s. However, a search in 1989 failed to find
any plants (Sabourin et al. 1992*). Most recently, TWS
searched the site in 2002 but did not find any plants
despite the presence of appropriate habitat and moder-
ate water levels. This site is adjacent to a campground
and recreational activity may have contributed to the
demise of this population. Water quality may also have
been a factor, as a river flowing into Lake Champlain
at this location smells strongly of raw sewage.
2004
—~
——
———> \
SMITH, DOUGLAS, AND HARRIS: SMALL-FLOWERED LIPOCARPHA 181
KAMLOOPS
SPENCES BRIDGE
I
i) aw
m4
7
_) \ENDERBY
_/ ARMSTRONG
/
. Okanagan ;
Z
Te
camoce
KEREMEOS,
BRITISH
COLUMBIA
NE
Lake . j
Ree
NCETON ~y PENTICTON J
On
Ficure 2. Distribution (stars) of Lipocarpha micrantha in British Columbia.
The oldest records of Lipocarpha micrantha in Can-
ada are collections from the Detroit River shoreline,
south of Windsor, Ontario, in 1892 (Macoun 28668,
specimen at CAN) and 1901 (Macoun 7594, speci-
mens at TRTE, GH). The populations represented by
these collections have presumably been destroyed by
shoreline development. The only recent records from
this region are from the vicinity of Holiday Beach Con-
servation Area, near Amherstburg. This population was
discovered in 1984, when 15 plants were observed
(Oldham and Crins 1988). The population was still
present in 1987 (Sabourin et al 1992*), but no plants
were found during two searches by TWS in 2001. The
habitat at Holiday Beach has been seriously degraded:
dense mats of algae covered the beach, except in areas
where it had been cleared away by heavy machinery.
182 THE CANADIAN FIELD-NATURALIST Vol. 118
TABLE |. Locations and Population Sizes for Lipocarpha micrantha in Canada.
Site Last Observer (Last Population
Observation Searcher) (number/area)
Osoyoos Lake (British Columbia) 1980 Ceska Extirpated
Osoyoos Lake, 2001 Douglas 30 000-50 000/2.3ha
Osoyoos Indian Reserve (British Columbia)
Okanagan Lake, 2002 Klinkenberg 120/2 m?*
Sun Oka Beach Provincial Park (British Columbia)
Sable Island (Ontario) 2001 Harris 1 800/0.4ha
Poundnet Bay (Ontario) 2000 (see text) Harris 75/0.00lha
Holiday Beach (Ontario) 1987 (2001 ) Oldham (Smith) Extirpated
Detroit River (Ontario) 1901 Macoun Extirpated
Missisquoi Bay (Quebec) 1957 (2002 ) Louis-Alphonse Extirpated
(Smith)
The Lake of the Woods population, at Sable Island,
Ontario, was discovered in 1995, and several thousand
plants were noted at that time (Oldham, personal com-
munication 2001). Surveys in 2001 documented approx-
imately 1800 plants. The long sandspit island provides
large areas of suitable habitat in Sable Island Prov-
incial Nature Reserve.
As a consequence of the ephemeral nature of its
habitat and its ability to remain dormant in unfavour-
able years, Lipocarpha micrantha may persist un-
detected at locations searched thoroughly by botanists.
An unsuccessful search during highwater, when much
potential habitat is temporarily unavailable, is there-
fore not justification for declaring a population extir-
pated. This was the case at Poundnet Bay on Rainy
Lake, Ontario, in 2001, where water levels were well
above average. No Lipocarpha micrantha plants were
found there during 2001 A population of 75 plants
was discovered at this location in 2000. When water
levels return to average or below this area will provide
habitat for Lipocarpha micrantha. It is known from
several beaches on the Minnesota side of Rainy Lake.
Lipocarpha micrantha was first documented on
Osoyoos Lake, British Columbia, by Ceska and Ceska
(1980). Of the two populations noted, one has been
eradicated by shoreline development. The British Col-
umbia Conservation Data Centre has been monitor-
ing the second population since 1991. In 2001 a total
of between 30 000 and 50 000 plants were invento-
ried. This is the highest recorded population at that site,
and it is the largest population in Canada. The high
number is attributed to excellent growing conditions,
and also to the higher search intensity in 2001. If con-
ditions remain stable at this site the population should
continue to thrive. However, local development plans
at the site, including a casino and marina, would likely
destroy about 50 to 60% of the remaining habitat. A
third, small (20 plants over 2 m*) population was dis-
covered on the shoreline of Okanogan Lake in 2002.
Special Significance of the Species
Lipocarpha micrantha has very specific habitat
requirements: open, sandy shorelines, protected from
strong waves, with limited competition from other
plants. It is extremely sensitive to alteration of both
water levels and shoreline structure. As such it may
be an important indicator of wetland quality.
Protection
Lipocarpha micrantha has a NatureServe (2002*)
global rank of G5 or “secure”. In the United States,
Lipocarpha micrantha is listed as Endangered in
Connecticut, Maryland, New Jersey, New York, and
Pennsylvania, and it is listed as Threatened in Maine
and Ohio (United States Department of Agriculture,
Natural Resources Conservation Service 2002*). In
Canada, Lipocarpha micrantha is ranked as N1 or
“critically imperilled”, and is listed as Threatened in
Ontario (NHIC, 2003*) and Endangered/Threatened
in British Columbia (Douglas et al. 2002).
Both extant Ontario populations of Lipocarpha
micrantha are in a Provincial Nature Reserve and a
Provincial Conservation Reserve. As such they are pro-
tected from shoreline development, but are subject to
water level regulation. The extant populations in British
Columbia occur on an Indian Reserve (Osoyoos Lake
Indian Reserve #1) and in a Provincial Park (Sun Oka
Beach Provincial Park). There is currently no specific
provincial rare species legislation in place for the pro-
tection of endangered/threatened vascular plants in
British Columbia. At the federal level the Species at
Risk Act protects COSEWIC-listed plants on federal
lands (which includes Indian Reserves). It also empow-
ers the federal government to protect habitat outside
federal lands if the province fails to protect listed spe-
cies or their habitat; these mechanisms are discretionary.
Evaluation of Status
The status of Lipocarpha micrantha in Canada is
precarious. The largest, apparently stable, population
at Osoyoos Lake in British Columbia is threatened by
planned development. Should this development proceed,
approximately half of the remaining Lipocarpha mic-
rantha plants in Canada will be physically destroyed,
and the remaining habitat may no longer support the
species. The two remaining Ontario populations are
2004
SMITH, DOUGLAS, AND HARRIS: SMALL-FLOWERED LIPOCARPHA
183
FiGure 3. Distribution of Lipocarpha micrantha in Ontario and Quebec. Sable Island is shown as a circle, Ponies: Bay as
a triangle. Squares denote extirpated populations.
relatively small, both in number and area, and there-
fore are vulnerable to environmental disturbance. If
development at any of the remaining populations pro-
ceeds without consideration for this species it will very
likely be extirpated from Canada. In particular, altera-
tion of natural water level cycles could result in the
destruction of the habitat required by Lipocarpha mic-
rantha. The authors’ recommendation that Lipocarpha
micrantha be uplisted to Endangered was accepted by
COSEWIC in November 2002.
Acknowledgments
The authors gratefully acknowledge the following
people for assistance with this report. Kara Brodribb,
Wasyl Bakowsky, Dan Dufour, Rob Foster, Ron Hall,
Erica Oberndorfer, Mike Oldham, Kathy Paige, Amy
Tesselin, and Christine Thuring assisted with field sur-
veys. Wasyl Bakowsky, Brian and Rose Klinkenberg,
Jim Meeker, Mike Oldham, Tony Reznicek and David
Szymanski provided location and habitat data. Erica
Oberndorfer, Jenifer Penny and Shyanne Smith assist-
ed with the production of maps and compilation of
status data. Graham Rose (Big Creek Hunt Club) gra-
ciously granted access to their properties for survey
work. This paper is based on a status report submitted
to the Committee On the Status of Endangered Wildlife
in Canada (COSEWIC), September 2001. The distri-
bution map for Ontario and Quebec, Figure 3, was
provided by COSEWIC. Funding was provided by
COSEWIC, the George Cedric Metcalf Foundation,
Royal Botanical Gardens, and the British Columbia
Conservation Data Centre.
Documents Cited
Harris, A. G., M. J. Oldham, R. F. Foster, and W. D.
Bakowsky. 2000. Preliminary life science inventory of
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Holmgren, P. K, N. H. Holmgren, and L. C. Barnett. 2003.
Index Herbariorum [web application]. Updated October 1,
2003. New York Botanical Garden, Bronx, New York.
Available at: http://www.nybg.org/bsci/ih/ih.html.
Natural Heritage Information Centre. 2003. Natural Heri-
tage Information Centre Database (http://www.mnr.gov.
on.ca/MNR/nhic/data.cfm). Natural Heritage Information
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NatureServe 2002. NatureServe Explorer: An online ency-
clopedia of life [web application]. 2002. Version 1.6. Arling-
ton, Virginia, USA: NatureServe. Available at http://www.
natureserve.org/explorer.
Sabourin, A., M. J. Oldham, and D. Paquette. 1992.
Status report on the Small-flowered Lipocarpha, Lipocarpha
micrantha (syn. Hemicarpha micrantha) in Canada. COSE-
WIC, Ottawa, Ontario.
184
Smith, T. W., G. W. Douglas, and A. G. Harris. 2002.
Update COSEWIC Status Report on Small-Flowered Lipo-
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United States Department of Agriculture, Natural Re-
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base, Version 3.5 (http://plants.usda.gov). National Plant
Data Centre, Baton Rouge, Louisiana.
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Columbia Ministry of Forests. Victoria, British Columbia.
361 pages.
Douglas, G. W., D. Meidinger, and J. L. Penny. 2002.
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Received 13 November 2003
Accepted 5 April 2004
Immobilization of Clover-trapped White-tailed Deer, Odocoileus
virginianus, with Medetomidine and Ketamine, and Antagonism with
Atipamezole
JosHUA J. MILLSPAUGH!, BRIAN E. WASHBURN!, TAMARA M. MEYER?, JEFF BERINGER?, and LONNIE P.
HANSEN?
‘Department of Fisheries and Wildlife Sciences, University of Missouri, 302 Anheuser-Busch Natural Resources Building,
Columbia, Missouri 65211 USA
*Missouri Department of Conservation, Conservation Research Center, 1110 South College Avenue, Columbia, Missouri
65201 USA
Millspaugh, Joshua J., Brian E. Washburn, Tamara M. Meyer, Jeff Beringer, and Lonnie P. Hansen. 2004. Immobilization of
Clover-trapped White-tailed Deer, Odocoileus virginianus, with medetomidine and ketamine, and antagonism with
atipamezole. Canadian Field-Naturalist 118(2): 185-190.
We evaluated the effectiveness of immobilizing Clover-trapped White-tailed Deer (Odocoileus virginanus) with medeto-
midine hydrochloride (HCl) and ketamine HCI during winter and summer by monitoring immobilization intervals and vital
signs. In winter, we captured deer in Clover traps in | 4-ha research enclosure for relocation to another on-site enclosure (n = 5).
In summer, we captured free-ranging deer in Clover traps to attach radio-collars (n = 4). We administered an estimated 0.055
mg/kg medetomidine HCI and 2.5 mg/kg ketamine HCI to adult (> 1.5 years of age) deer and 0.06 mg/kg medetomidine HC]
and 2.5 mg/kg ketamine HCl to subadult (< 1.5 years of age) deer. We used an intramuscular injection of atipamezole HC] as the
antagonist at a rate of 0.275 mg/kg for adults and 0.3 mg/kg for subadults > 30 minutes post-induction. Mean induction time in
winter was 11.2 minutes (SE = 2.5, range = 5.4 — 24.2) and 6.5 minutes (SE = 0.8, range = 6.2 — 7.5) in summer. After atipame-
zole HCl injection, the mean time to walking was 17.1 minutes (SE = 3.5, range = 7.5 — 41.5 minutes) in winter and 11.3 minutes
(SE = 3.8, range = 4.7 — 13.5) in summer. Rectal temperature was relatively constant throughout immobilization; however
rectal temperatures of 5 deer (7 = 3 in winter; n = 2 in summer) exceeded 40°C, a sign of hyperthermia. Respiration rate and pulse
rate peaked at about 20 minutes post-medetomidine HCI and ketamine HCl injection, then generally declined thereafter. No
mortalities were observed in our study. Medetomidine HCI and ketamine HCI doses for Clover-trapped White-tailed Deer pro-
vided satisfactory induction times, sufficient level of anesthesia for short-distance relocation or radio-collar Eucte alee and
were effectively reversed with an IM injection of atipamezole HCl.
Key words: White-tailed Deer, Odocoileus virginianus, atipamezole, capture, chemical restraint, Clover trap, deer, ketamine,
immobilization, medetomidine, Missouri.
White-tailed Deer (Odocoileus virginianus) have
been chemically immobilized with Telazol® (1:1 tile-
tamine hydrochloride (HCl) and zolazepam HCl) and
xylazine HCI (Schultz et al. 1992; Kilpatrick and Spohr
1999), ketamine HCl and xylazine HCI (Mech et al.
1985; Farley et al. 1986; Kreeger et al. 1986; Ballard et
al. 1998; Kilpatrick and Spohr 1999), etorphine and
xylazine HC] (Presnell et al. 1973; Presidente et al.
1973; Nielsen 1982), xylazine HCI alone (Gibson et
al. 1982), phencyclidine HCl (Dean et al. 1973), and
succinylcholine chloride (Wesson et al. 1974; Jacobsen
et al. 1976). Kreeger (1996) recommended 4.4 mg/kg
Telazol® and 2.2 mg/kg xylazine HCl to immobilize
White-tailed Deer; 0.125 mg/kg yohimbine HCl was
the recommended antagonist. Recently, Kilpatrick and
Spohr (1999) used a 4.8:3.9 mg/kg dose of Telazol®:
xylazine HCI to dart free-ranging White-tailed Deer.
Alternative drugs recommended by Kreeger (1996)
include ketamine HCl and xylazine HCl, etorphine,
xylazine alone (for calm deer only), and a combina-
tion of medetomidine HCI and ketamine HCl.
Medetomidine HCl depresses the central nervous
system and acts similarly to xylazine HC] (Jalanka and
Roeken 1990), but with greater affinity to alpha,-
adrenoreceptors (Klein and Klide 1989; Jalanka and
Roeken 1990; Kreeger 1996). Ketamine HCl, an anes-
thetic, is often combined with a tranquilizer or seda-
tive to improve induction and recovery (Haigh 1982;
Kreeger 1996). Medetomidine HCl and ketamine HC]
alone or in combination with other drugs have been suc-
cessfully used to immobilize a diversity of large ungu-
lates including Reindeer (Rangifer tarandus tarandus)
(Ryeng et al. 2001, 2002), Mule Deer (Odocoileus
hemionus) (Caulkett et al. 2000), Mule Deer/White-
tailed Deer hybrids (Caulkett et al. 2000), Sika Deer
(Cervus nippon) (Tsuruga et al. 1999), gemsbok (Oryx
gazella) (Grobler et al. 2001), Roan Antelope (Hippo-
tragus equinus) (Citino et al. 2001), Blue Duiker
(Cephalophus monticola) (Bailey et al. 1995), Moose
(Alces alces) (Arnemo 1995), Tigers (Panthera tigris)
(Miller et al. 2003), Impala (Aepyceros melampus) (Bush
et al. 2004), European Mink (Mustela lutreola) Four-
nier-Chambrillon et al. 2003) and Red Deer (Cervus
elaphus) (Arnemo et al. 1994).
Notable among the advantages listed in these and
other studies is the ability to reverse medetomidine HC]
185
186
with an intramuscular (IM) injection of atipamezole
HCl (Tsuruga et al. 1999; Haulena et al. 2000). Atipa-
mezole HCI is an extremely efficient alpha,-adren-
ergic antagonist compared with yohimbine HCl and
tolazoline HCl (Kreeger 1996) and effectively reverses
medetomidine HCl in many wildlife species (Tsuruga
et al. 1999; Haulena et al. 2000; Grobler et al. 2001).
If medetomidine HCl and ketamine HC] were as effi-
cient and safe as other immobilizing agents (e.g., Tela-
zol® and xylazine HCl) and if an IM injection of ati-
pamezole HCI was a safe and effective antagonist, this
combination could prove efficacious in field studies.
Our objective was to determine the effectiveness and
safety of immobilizing Clover-trapped White-tailed
Deer with medetomidine HCI and ketamine HCI, and
the feasibility of reversing this combination with an IM
injection of atipamezole HCl, during winter and sum-
mer by monitoring immobilization intervals and vital
signs. To our knowledge, an evaluation using mede-
tomidine HCI and ketamine HCl to immobilize free-
ranging White-tailed Deer and antagonism by ati-
pamezole HCI has not been previously published.
Methods
Our review of the medetomidine HCI and ketamine
HCl combination took place in winter and summer
2001. In summer and winter, we trapped White-tailed
Deer in Clover traps (McCullough 1975). During win-
ter we trapped deer at the Charles W. Green Conser-
vation Area, located near Ashland, Missouri. Traps
were baited with corn, set each evening, and checked
at sunrise. All winter-trapped and immobilized deer
(n = 5) were captured within a 4-ha research enclo-
sure for relocation to another on-site 4-ha enclosure.
These deer were not habituated to humans.
In summer, we trapped White-tailed Deer at the
Thomas S. Baskett Wildlife Research and Education
Area, located near Ashland, Missouri. Traps, baited
with salt, alfalfa, and corn, were set each evening and
checked at sunrise. We captured and immobilized
summer-trapped deer (n = 4) for purposes of radio-
collar attachment. These deer were free-ranging ani-
mals and not habituated to humans.
In winter and summer, we immobilized adult deer
(> 1.5 years of age) (n = 2 in winter; n = 3 in sum-
mer) using an estimated 0.055 mg/kg medetomidine
HCl and 2.5 mg/kg ketamine HCI; 0.06 mg/kg mede-
tomidine HCI and 2.5 mg/kg ketamine HCI was ad-
ministered to subadult deer (< 1.5 years of age) (n = 3
in winter; n = 1 in summer). Adult deer, estimated to
be 60 kg, were given 3.3 mg of | mg/ml Domitor®
(medetomidine HCl; Orion Corporation, Orion—
Farmos, Espoo, Finland) and 150 mg of 100 mg/ml
Ketaset® (ketamine HCl; Fort Dodge Laboratories,
Inc., Fort Dodge, Iowa, USA). Subadult deer, estimat-
ed to be 30 kg, were given 1.8 mg of 1 mg/ml mede-
tomidine HCl and 75 mg of 100 mg/ml ketamine HCl.
We injected drugs IM into the biceps femoris with a
THE CANADIAN FIELD-NATURALIST
Vol. 118
hand syringe. Sex and age (adult or subadult) were
recorded and during winter each deer was marked with
a plastic cattle ear tag in one ear for later identification.
In summer, deer were fitted with radio-transmitters.
Following sedation in winter and summer, we ap-
plied an ophthalmic ointment and blindfolded the deer.
In winter, we relocated deer to a different on-site 4-ha
enclosure. Two or three field assistants placed the sed-
ated deer into the rear of a vehicle (range from 100 to
300 m away), which was driven to the release enclo-
sure (< | km driving distance). Each deer was carried
into the enclosure (< 30 m away), and placed in a ster-
nal recumbent position.
We reversed the medetomidine HCI and ketamine
HCI combination with an IM injection of Antisedan®
(atipamezole HCI; Orion Corporation, Orion—Farmos,
Espoo, Finland) into the biceps femoris with a hand
syringe at a rate of 0.275 mg/kg (16.5 mg of 5 mg/ml
atipamezole HCl) for adults and 0.3 mg/kg (9 mg of
5 mg/ml atipamezole HCl) for subadults. We visually
monitored all deer until they departed the area.
During winter and summer, we attempted to monitor
immobilization intervals and vital signs at 5-minute
intervals. For all deer, we recorded time of medetomi-
dine HCI and ketamine HCl injection, induction (time
from injection to time animal was handled), atipame-
zole HCl administration, “head up” (time when the
animal first lifted its head), “standing” (time when
the animal first stood up), and “walking” (time when
the animal successfully departed the area). We also
recorded respiration rate (breaths/minute), rectal tem-
perature (°C), and pulse rate (beats/minute) at 5-min-
ute intervals beginning at the time of medetomidine
HCI and ketamine HCl injection for respiration rate
and beginning 10 minutes post-medetomidine HCl and
ketamine HCl injection for temperature and heart rate.
Results
Nine deer (1 = 5 in winter, including 2 female sub-
adults, 1 male subadult, | female adult, and 1 male
adult; n = 4 in summer, including 3 adult females and
1 female subadult) were immobilized using the drug
combination described above and either relocated or
equipped with a radio-collar. No mortality has been
observed 10 months post-winter immobilization and
5 months post-summer immobilization.
Mean induction time was 11.2 minutes (SE = 2.5,
range = 5.4 — 24.3) in winter and 6.5 minutes (SE = 0.8,
range = 6.2 — 7.5) in summer. Time to atipamezole HCl
injection averaged 54.4 minutes (SE = 3.7, range = 37.7
— 79.2) in winter and 33.4 (SE = 1.3, range = 30.4 —
33.8) in summer. After atipamezole HCl injection, the
mean time to head up was 11.4 minutes (SE = 2.9,
range = 4 — 27.5) in winter and 9.3 minutes (SE = 0.7,
range = 8.4 — 9.9) in summer. Mean time to standing
was 15.9 minutes (SE = 3.6, range = 4.4 — 41) in win-
ter and 10.5 minutes (SE = 3.2, range = 4.7 — 12.3) in
summer. The mean time to walking was 17.1 minutes
2004 MILLSPAUGH, WASHBURN, MEYER, BERINGER, AND HANSEN: IMMOBILIZATION OF WHITE-TAILED DEER 187
(SE = 3.5, range = 7.5 — 41.5 minutes) in winter and
11.3 minutes (SE = 3.8, range = 4.7 — 13.5) in summer.
With the exception of rectal temperatures, other
vital signs were considered normal (Table 1). Rectal
temperatures were stable from 10 — 30 minutes post-
medetomidine HCl and ketamine HCl injection in
summer and winter (Table |). Temperatures of 1 sub-
adult female captured in winter were 37.4°C and 36.2°C
at 70 and 110 minutes post-induction, respectively;
thus, she was within 1.2°C of becoming hypothermic
(defined as < 35°C; Kreeger 1996; DelGuidice et al.
2001). No attempt was made to increase body temper-
ature of this individual prior to antagonism with atipa-
mezole HCl. After atipamezole HCI administration,
it took that individual 41.5 minutes to depart, the max-
imum time observed in our study. Rectal temperatures
of 5 deer (n = 3 in winter, m = 2 in summer) exceeded
40°C, a sign of hyperthermia. No attempt was made
to decrease body temperature of these animals prior to
antagonism. Respiration rates showed little variability
in summer and winter and were generally in the upper
20’s to low 30’s (breaths/minute) (Table 1) peaking
at about 20 minutes post-medetomidine HCl and
ketamine HCl injection. Pulse rates peaked about 20
minutes post-medetomidine HCl and ketamine HCl
injection at 95 beats/minute (SE = 3.6) in winter and
103 beats/minute (SE = 1.4) in summer and declined
thereafter to 74 beats/minute (SE = 5.6) in winter and
88 beats/minute (SE = 3.1) in summer at 30 minutes
post-medetomidine HCI and ketamine HCl injection
(Table 1). No other adverse side effects were noted.
During summer captures, response to IM injection
of atipamezole HCl was predictable, as previously
described by Jalanka and Roeken (1990). Within 3 —
6 minutes of atipamezole HCl injection, “ear-twitch-
ing” occurred, followed by leg extensions after an addi-
tional 3 — 6 minutes, and “head up” 2 minutes there-
after. Standing followed within another 2 minutes and
the animal departed almost immediately with good
muscle coordination.
Discussion
Medetomidine HCl] and ketamine HCl doses for
Clover-trapped deer provided satisfactory induction
times, produced a sufficient level of anesthesia for
short-distance relocation or radio-collar attachment,
and were effectively reversed with an IM injection of
atipamezole HCI. Small dosage volume, ease of prepa-
ration and predictable responses to sedation and to
the antagonist make this combination a useful alterna-
tive to drug combinations that may require prolonged
recovery.
Medetomidine HCl and ketamine HCl provided
induction times similar to those reported in other
studies and with other drugs. For 13 captive White-
tailed Deer in Minnesota, it took 2 to 35 minutes (medi-
an = 8, SE = 1.2) from the time of xylazine HCI and
ketamine HCl administration before deer lost the ability
to stand (Mech et al. 1985). Our mean induction time
in winter (x = 11.2 minutes, SE = 2.5, range = 5.4 —
24.3, n = 5) was about double the median time of 6.2
minutes (range = 0.5 — 17.3) reported by Jalanka and
Roeken (1990) for 28 captive White-tailed Deer housed
at the Helsinki Zoo, but similar to our summer mean
time of 6.5 minutes (SE = 0.8, range = 6.2 — 7.5). In
the Helsinki Zoo study, deer were given an average
of 61 ug/kg (SD = 14, median = 58, range = 37 — 98)
medetomidine HCI and a mean ketamine HCI dose of
1.6 mg/kg (SE = 0.3, median = 1.5, range = 1 — 2.3).
The time to walking after the IM injection of ati-
pamezole HCI was similar to that for deer in other
studies reversed with yohimbine HCl, but was less
TABLE |. Mean + SE (N) vital signs of White-tailed Deer immobilized with medetomidine hydrochloride (HCl) and ketamine
HCl, and antagonized with atipamezole HCl during winter and summer 2001 in mid-Missouri for purposes of relocation
(winter) and radio-collar attachment (summer). Adults were immobilized with 0.055 mg/kg medetomidine HCI and 2.5
mg/kg ketamine HCl and subadults were immobilized with 0.06 mg/kg medetomidine HCl and 2.5 mg/kg ketamine HCl.
Adults were antagonized with 0.275 mg/kg of atipamezole HCI and subadults were antagonized with 0.03 mg/kg of atipamezole
HCI. We have not reported data where information was collected on < 2 deer. Time 0 is the time of medetomidine HCI and
ketamine HCl injection.
Winter Summer
Time Respiration Rate Pulse Rate Temperature Respiration Rate Pulse Rate Temperature
(minutes) (breaths/minute) (beats/minute) (c) (breaths/minute) (beats/minute) (°C)
0 PH pd =e PEMA G)) — - 23 + 1.4 (4) - ~
5 DifeD) 7D) -3)()) - - 23 + 2.2 (4) - -
10 28.8 + 2.9 (5) 87 +3.6(4) 41.1405 (2) 31+2.4 (4) 98+2.0(4) 39.9+ 1.2 (4)
15 29.6 + 3.2 (5) 88 +43(4) 40.9+0.8 (4) 31+2.2(4) 101+1.9(4) 39.8414 (4)
20 SI =n 244) 94.7+3.6(3) 40.62 1.2 (3) 30+2.6(4) 103+1.9(4) 39.8+1.4(4)
25 Posy \oe2 Syil (G) 86 +3.5(4) 404+1.2 (4) 30+3.1(4) 101424(4) 39.6+1.3 (4)
30 29.3 + 3.6 (4) Ase) 16\(2) wae 3 9-3 -t ile 9 (2) 32 + 2.9 (4) 88+3.1(4) 39.3+1.2 (4)
35 24 +2.4(2) Diet) ED (2) - 24 + 0.0 (2) ~ =
40 - — ~ 24 + 0.0 (2) - ~
45 Syd" Tes 3}5) (3) - - — — =
50 PR: a2 3)3} (8) - 40.1 + 1.2 (2) - - -
188
variable. An intravenous injection of yohimbine HCl
following xylazine HCl and ketamine HCl immo-
bilization resulted in an adult male walking in 1.5 min-
utes (SE = 0.5, n = 2 immobilizations) to 26.5 minutes
(SE = 11.5, n = 4 immobilizations) for an adult fe-
male (Mech et al. 1985). For 22 White-tailed Deer
(18 free-ranging captured using drop nets and 4 cap-
tive) immobilized with xylazine HCl and ketamine
HCl, an IM injection of yohimbine HCI produced a
mean recovery time of 11.6 minutes (SE = 2.3)
(Wallingford et al. 1996). Hsu and Shulaw (1984) used
an IV injection of yohimbine HCI and reported a mean
recovery time of 4.4 minutes (SD = 5.4 minutes) for
xylazine HCl-immobilized deer.
With the exception of rectal temperature, the vital
signs observed in this study were within the normal
range of reported values for White-tailed Deer. Mautz
and Fair (1980) reported pulse rates of a 46-kg adult
White-tailed Deer female in July that was lying, stand-
ing/walking, and running at 65, 74, and 106 beats per
minute, respectively. Pulse rates observed in this study
were similar to predicted walking pulse rates of White-
tailed Deer (Moen 1978: 722), yet higher than those
rates reported by Jalanka and Roeken (1990: 267).
Rectal temperatures of five deer were above 40°C, a
sign of hyperthermia (Kreeger 1996). Average rectal
temperatures in our study in winter (39.3°C at 30
minutes, SE = 1.9, n = 2) and summer (39.3°C at 30
minutes, SE = 1.2, n = 4) are similar to the maximum
rectal temperatures reported by DelGuidice et al.
(2001:1151) for White-tailed Deer captured by Clover
trap and immobilized with xylazine HCI and ketamine
HCI during the winter in Minnesota. Also in Minne-
sota, Rogers et al. (1987) reported rectal temperatures
of two female free-ranging White-tailed Deer fawns in
all seasons during various activities ranged between
38.2° and 40.1°C. Rectal temperatures of 3 adult male
White-tailed Deer in Mississippi, averaged 39.3°C
during late August and September and 38.6°C in
early December (Demarais et al. 1986). As suggested
by DelGiudice et al. (2001), corrective actions (i.e.,
packing snow around the animal) should be taken
when immobilized animals become hyperthermic.
Consequently, rectal temperatures should be monitored
and protocols should be established to determine when
corrective actions should begin (DelGiudice et al.
2001).
Both medetomidine HCl and ketamine HCl have
wide safety margins, produce calm inductions in several
artiodactyls, are safe for humans (Jalanka and Roeken
1990), and have not caused any apparent detrimental
effects in pregnant females (Jalanka 1993). Few adverse
side effects were noted by Jalanka and Roeken (1990)
after 1240 immobilizations with medetomidine HCl,
ketamine HCl, and antagonism with atipamezole HCl.
Worth noting, some ruminants became resedated be-
tween 30 and 240 minutes post-IV reversal with ati-
pamezole HCI (Jalanka and Roeken 1990) and unre-
THE CANADIAN FIELD-NATURALIST
Vol. 118
markable ruminal tympany was common in ruminants
prior to atipamezole HCI administration (Jalanka and
Roeken 1990; Jalanka 1993).
A disadvantage of the medetomidine HCl, ketamine
HCl, and atipamezole HC] combination is cost. In U.S.
currency, cost to immobilize each adult deer was
$34.72 ($32.76 for medetomidine HCI and $1.96 for
ketamine HCl) and $18.85 for each subadult deer
($17.87 for medetomidine HC] and $0.98 for ketamine
HCl). Atipamezole HCI cost $33.22 per adult deer and
$18.14 for each subadult deer. In contrast, Kilpatrick
and Spohr (1999) reported a cost of $8.44/deer for
Telazol® and xylazine HCl immoblized deer and $6.34/
deer for ketamine HCI and xylazine HCI without lyo-
philizing costs. With lyophilizing, costs were $10.05/
deer for Telazol® and xylazine HCl and $16.49 for
ketamine HCl and xylazine HCI (Kilpatrick and Spohr
1999). Consequently, use of medetomidine HCl, keta-
mine HCl, and atipamezole HCI may be cost-prohib-
itive in studies requiring immobilization of many ani-
mals. However, given the desirable properties discussed
above, including rapid reversal that requires less man-
power time, these desirable qualities may outweigh
drug costs. Also, the ability to administer an antagonist
IM may be advantageous in field studies (Wallingford
et al. 1996). We recommend researchers investigate
the utility of reversing the less costly and popular
Telazol®/xylazine HCl and ketamine HCl/xylazine
HCl combinations with an IM injection of atipame-
zole HCl.
The combination of medetomidine HCl, ketamine
HCl, and atipamezole HCl reported herein provided
an effective level of anesthesia for Clover-trapped
White-tailed Deer. We recommend the use of 0.055
mg/kg medetomidine and 2.5 mg/kg ketamine HCl to
immobilize adult Clover-trapped White-tailed Deer
and 0.06 mg/kg medetomidine HCl and 2.5 mg/kg
ketamine HC] for subadults. Furthermore, we recom-
mend 0.275 mg/kg and 0.3 mg/kg of atipamezole,
injected IM, to reverse this combination in adults and
subadults, respectively.
Acknowledgments
We thank R. Houf, T. Mong, and numerous volun-
teers for their assistance in the field. Missouri Depart-
ment of Conservation, Conservation Research Center,
provided Clover traps. A University of Missouri Res-
earch Board grant, the University of Missouri, and the
Missouri Department of Conservation supported this
project.
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Journal of Wildlife Diseases 9: 336-341.
190
Rogers, L. L., A. N. Moen, and M. L. Shedd. 1987. Rectal
temperatures of 2 free-ranging white-tailed deer fawns.
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THE CANADIAN FIELD-NATURALIST
Vol. 118
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Received 2 March 2002
Accepted 3 October 2004
reer
Predation on Two Mule Deer, Odocoileus hemionus, by a Canada Lynx,
Lynx canadensis, in the Southern Canadian Rocky Mountains
Dore Poszic!, CLAYTON D. Apps?, and ALAN Disb?
' Alhardstr. 15, 28757 Bremen, Germany
? Aspen Wildlife Research Inc., 2708 Cochrane Road N.W., Calgary, Alberta T2M 4H9 Canada (corresponding author)
3 Parks Canada, P. O. Box 220, Radium Hot Springs, British Columbia VOA 1MO0 Canada
Poszig, Dérte, Clayton D. Apps, and Alan Dibb. 2004. Predation on Two Mule Deer, Odocoileus hemionus, by a Canada
Lynx, Lynx canadensis, in the southern Canadian Rocky Mountains. Canadian Field-Naturalist 118(2): 191-194.
A male Canada Lynx (Lynx canadensis) killed two Mule Deer (Odocoileus hemionus) in the southern Canadian Rocky
Mountains in January 1999 and made use of the kills for 28 days. Canada Lynx predation on ungulates has been reported but
is rare, and accounts have been brief. We detail the lynx behaviour associated with the kills and their consumption. An infra-
red monitor and attached camera were used to register daily activity at the kill site. We speculate on the factors that may have
influenced this opportunistic predation event.
Key Words: Canada Lynx, Lynx canadensis, infrared monitor, Mule Deer, Odocoileus hemionus, predation, British Columbia.
The Canada Lynx (Lynx canadensis), hereafter
referred to as lynx, preys mainly on Snowshoe Hares
(Lepus americanus) and other small mammals, but
rare accounts of ungulate predation have been noted
(e.g., Saunders 1963; van Zyll de Jong 1966; Parker
et al. 1983; Stephenson et al. 1991). However, these
accounts do not describe lynx behaviour associated
with the kills or their consumption. We give a detailed
description of two Mule Deer (Odocoileus hemionus)
kills made by a lynx and its subsequent use of them
for 28 days. The observations were made in the course
of an in-depth field study of lynx ecology in the south-
ern Canadian Rocky Mountains of southeastern British
Columbia and southwestern Alberta.
While snow-tracking on 18 January 1999, we found
two Mule Deer that had been killed by a radio-col-
lared adult male Canada Lynx in Kootenay National
Park, British Columbia (51° N, 116° W). One was a
doe aged by cementum annuli to be 3.5 years, and we
estimated the other deer to be a fawn (teeth not com-
pletely erupted). The kills were separated by a distance
of 10 m and were located at 1580 m elevation on a
15° slope of northwest aspect in a closed-canopy forest
of Lodgepole Pine (Pinus contorta), Engelmann Spruce
(Picea engelmannii), and Subalpine Fir (Abies lasio-
carpa). The understory was sparse, although the imme-
diate area around the kill site had some woody debris
to a depth of about | m and some conifer thickets. The
snow depth at the site was 90 cm and lynx penetration
was 9-14 cm.
The fawn apparently was killed on 14-15 January,
judging from daily radio-telemetry fixes of the lynx
and accumulated snow cover. The shoulders, rib cage,
part of the neck, upper front legs and organs had been
consumed. The front and rear had been severed and lay
twisted and partially cached in a hollow in the snow.
The doe was killed on 18 January between about 1300
and 1500 h. On initial inspection, no snow had accu-
mulated on the carcass, and the blood had not yet co-
agulated or frozen. The deer was found lying on its side
with legs extended, and no part had yet been consumed.
Teeth of both deer were in good condition, and no
deformities of their legs or hooves were apparent. The
doe appeared to be in good physical condition. Both
deer had major wounds on the dorsal side of their necks,
and the spacing of obvious tooth-punctures matched
that of a lynx (Figure 1). The cause of death of the
fawn could not be determined because it had been con-
sumed to a great extent and was not intact. On the doe,
several puncture wounds were located in two small
areas on the dorsal to slightly lateral area of the neck,
10-15 cm behind the ears. Claw marks on the deer’s
back and shoulders suggested that the lynx had leapt
onto the deer and had been “riding” while biting it.
Evidence of predation of the fawn was obscured by
recent snow, but old blood stains 2 m from the carcass
suggested that it had been killed and not scavenged.
When removing the mandible of the fawn, we found
pieces of undigested Subalpine Fir in its mouth, sug-
gesting that the animal had been browsing shortly
before it died.
Tracks in the snow provided a clear record of how
the lynx encountered and stalked the doe. The lynx
approached this deer from a slightly higher elevation
than where both kills were found, partially circling the
site for about 100 m. It briefly stopped at the edge of
a small opening about 50 m from the kill site, and then
again 25 m uphill on a knoll. Moving downhill in a
normal gait, the lynx used several fallen logs for cover,
but was clearly stalking for the last 10 m. It then made
three bounds before its attack, as the doe stood next
to a thicket of mixed-age trees. The deer appeared to
succumb <4 m from the attack site. The lynx then
dragged the carcass about 7 m to its final location.
LOM
192
THE CANADIAN FIELD-NATURALIST
Vol. 118
FiGure 1. Neck wound (arrows indicate puncture locations) resulting in the death of an adult female Mule Deer by a
Canada Lynx in the southern Canadian Rocky Mountains, January 1999.
Six site visits conducted over the three weeks fol-
lowing the initial find indicated that the lynx first fed
on the doe’s neck, continued to feed on the shoulders
and rib cage, and finally ate the rear and internal organs.
Deer hair had been removed and was positioned around
and on top of the kill. There were several well-used
lynx beds that appeared to be strategically located
upslope, <120 m from the kill site, with clear down-
hill views. The hindquarters of the fawn were moved
to 4 different locations between our site visits, and
each time were cached under snow and branches. It is
possible that this was prompted by our inspections.
On 29 January we installed an infrared monitor
(Trailmaster™ 1500, Goodson and Associates Inc.,
Kansas, with attached Olympus camera) at the doe’s
kill site to document the 24-hour activity of the lynx
at the site. The monitor was programmed to register
all beam interferences, while the remote camera was
set to take a photo upon beam interference, with <1
photo/15 min and between 0900 h and 1630 h to avoid
flash disturbance. Because the lynx no longer appeared
to be feeding on the fawn, we expected that all subse-
quent feeding events would be registered.
Twenty photos of the lynx were obtained and
showed that only this animal fed on the carcass (e.g.,
Figure 2). In addition, no other predator was detected
at the site during inspections that occurred about every
four days. lynx activity at the kill peaked around mid-
night and in the late morning (Figure 3).
The lynx abandoned the kill site after 28 days, at
which time the head and lower side of the doe’s car-
cass were frozen into the ground. Scratch marks sug-
gested that the lynx had unsuccessfully tried to remove
some snow to access parts of the deer. Upon incidental
recapture 16 days later, the lynx weighed 15.9 kg,
18.6% more than at his previous and original capture
in November 1996, while skeletal measurements had
not changed (C. D. Apps, unpublished data).
Our account is consistent with the observations by
Stephenson et al. (1991) of lynx ambushing ungulate
prey at close range. They reported a lynx remaining
on a Caribou (Rangifer tarandus) kill for 42 days. In
our study, the Lynx apparently abandoned the site be-
cause it could not make use of the carcass remains, and
it might have stayed longer had conditions permitted.
Previous reports of lynx predation on ungulates
have been associated with the low phase of the approx-
imate 10-year population cycle of Snowshoe Hares,
the lynx’s primary prey. The reliance of lynx on alter-
nate prey is greatest at this time (Mowat et al. 2000).
Although the deer kills we report occurred during an
assumed Snowshoe Hare population peak, hare densi-
ties in the study area were comparable to boreal regions
during the cyclic low (Apps 2000; C.D. Apps, unpub-
lished data).
2004 Poszic, APPS, AND DIBB: PREDATION ON MULE DEER By A LYNX 193
=
itl
FIGURE 2. Remote camera photo of a Canada Lynx at the carcass of a Mule Deer it killed in the southern Canadian Rocky
Mountains, January 1999.
80 10
a Frequency of Monitor interference
~9
70 .
=—@—Frequency of Days with > 0
Monitor Interferences 8
60
Uf
50
6
3 g
S 40+ 5 s
S a
we 4
30
3
20
2
10
00:00- 02:00- 04:00- 06:00- 08:00- 10:00- 12:00- 14:00- 16:00- 18:00- 20:00- 22:00-
01:59 03:59 05:59 07:59 09:59 11:59 13:59 15:59 17:59 19:59 21:59 23:59
Time of day (h)
Ficure 3. Lynx activity while feeding on a Mule Deer kill over 11 days in the southern Canadian Rocky Mountains,
January 1999. Total frequency (1 min. intervals; n = 344) and number of days that the Canada Lynx triggered an infrared
monitor (monitor interference) per 2-h period are shown.
194
We further note that the relatively high elevation
and deep snow of the kill site made it an atypical loca-
tion for Mule Deer during mid-winter. We speculate
that the deer may have been avoiding other predators,
most notably Gray Wolves (Canis lupus) that travel
primarily through the valley bottom. Thus, we expect
that this predation was opportunistic, perhaps influ-
enced by relatively low densities of Snowshoe Hares,
the age class and sex of the lynx (adult male), and the
vulnerability of the deer.
Acknowledgments
The Southern Canadian Rockies Lynx Project was
jointly funded by the Habitat Conservation Trust Fund
through the British Columbia Ministry of Water, Land
and Air Protection (formerly Environment, Lands
and Parks), Parks Canada, and the Columbia Basin
Fish and Wildlife Compensation Program. Additional
financial contributions were provided by the Friends
of Kootenay National Park, Husky Oil, World Wild-
life Fund Canada, Fairmont Hotels and Resorts (for-
merly Canadian Pacific Hotels & Resorts), and the
Bow Valley Naturalists. Contract supervision, input,
and direction were provided by A. Dibb of Parks Can-
ada, J. Krebs of the Columbia Basin Fish and Wildlife
Compensation Program, and A. Fontana, R. Neil, G.
Tipper, R. Forbes, and I. Teske of BC Environment.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Literature Cited
Apps, C. D. 2000. Space use, diet, demographics, and topo-
graphic associations of Lynx in the southern Canadian
Rocky Mountains. Pages 351-371 in Ecology and conser-
vation of Lynx in the United States. Edited by L. F. Rug-
giero, K. B. Aubry, S. W. Buskirk, G. M. Koehler, C. J.
Krebs, K. S. McKelvey, and J. R. Squires. University Press
of Colorado, Boulder, Colorado.
Mowat, G., K. G. Poole, and M. O’Donoghue. 2000.
Ecology of Lynx in northern Canada and Alaska. Pages
365-306 in Ecology and conservation of Lynx in the
United States. Edited by L. F. Ruggiero, K. B. Aubry, S.
W. Buskirk, G. M. Koehler, C. J. Krebs, K. S. McKelvey,
and J. R. Squires. University Press of Colorado, Boulder,
Colorado.
Parker, G. R., J. W. Maxwell, L. D. Morton, and G. E. J.
Smith. 1983. The ecology of the Lynx (Lynx canadensis)
on Cape Breton Island. Canadian Journal of Zoology 61:
770-786.
Saunders, J. K. Jr. 1963. Food habits of the Lynx in New-
foundland. Journal of Wildlife Management 27: 384-390.
Stephenson, R. O., D. V. Grangaard, and J. Burch. 1991.
Lynx, Felis lynx, predation on Red Foxes, Vulpes vulpes,
Caribou, Rangifer tarandus, and Dall Sheep, Ovis dalli,
in Alaska. Canadian Field-Naturalist 105: 255-262.
van Zyll de Jong, C. G. 1966. Food habits of the Lynx in
Alberta and the Mackenzie District, N.W.T. Canadian
Field-Naturalist 80: 18-23.
Received 8 September 2002
Accepted 25 October 2004
Effect of Fire Intensity and Depth of Burn on Lowbush Blueberry,
Vaccinium angustifolium, and Velvet Leaf Blueberry, Vaccinium
myrtilloides, Production in Eastern Ontario
Luc C. DUCHESNE! and SUZANNE WETZEL2?
'Rorest BioProducts Inc., 945 Queen Street East, Sault Ste Marie, Ontario P6A 2E5 Canada
>Natural Resources Canada, Canadian Forestry Service, 1219 Queen Street East, Sault Ste Marie, Ontario P6A 3A5 Canada
3Corresponding author at swetzel@NRCan.gc.ca
Duchesne, Luc C., and Suzanne Wetzel. 2004. Effect of fire intensity and depth of burn on Lowbush Blueberry, Vaccinium angusti-
folium, and Velvet Leaf Blueberry, Vaccinium myrtilloides, production in eastern Ontario. Canadian Field-Naturalist
118(2): 195-200.
The effects of prescribed fire intensity and depth of burn were investigated on Lowbush Blueberry (Vaccinium angustifolium)
and Velvet Leaf Blueberry (Vaccinium myrtilloides) stem density, blueberry production and the number of blueberries/stem in a
clear-cut Jack Pine, Pinus banksiana, ecosystem of eastern Ontario. Blueberry production and stem density were significantly
(P < 0.001) increased by low intensity prescribed fires of 597 and 1268 kW/m. In contrast, prescribed fires of medium and high
intensities did not affect blueberry production and stem density. The number of blueberries/stem was not affected (P = 0.056)
by prescribed burning, two years after treatment. Pearson’s multiple correlation analysis showed that blueberry production
(R: -0.683, P < 0.01), stem density (R: 0.733, P < 0.01) and the number of blueberries/stem (R: 0.803, P < 0.01) correlated with
depth of burn. As well, blueberry production (R: 0.507, P < 0.05) and stem density (R: -0.504, P < 0.05) correlated with fire
intensity. Depth of burn was a better predictor of berry production and stem density than fire intensity. These results suggest
that only low intensity fires with little penetrating effect in the ground should be used to manage blueberry crops.
Key Words: Lowbush blueberry, Vaccinium augustifolium, Vaccinium myrtilloides, wildfire, nontimber forest products (NTFP).
Nontimber forest products (NTFP) are all botanical
commodities harvested from the forest excluding in-
dustrial timber use (Duchesne et al. 2000). NTFP are
critical to the economy of forest and rural communi-
ties by providing food as well as supplemental income,
which often improves the standard of living of rural
and First Nation communities (Brubaker 1997; Du-
chesne et al. 2001; Mohammed 1999). Despite the
socio-economic importance of this industry there has
been little scientific research conducted for its support,
presumably because of its novelty. However, the long-
term success of the NTFP industry depends on acquir-
ing precise knowledge regarding the availability, and
sustainability of wild harvests as well as strategies to
domesticate and manage many of the most sought after
NTFP species. Species such as Lowbush Blueberry
(Vaccinium angustifolium) and Velvet Leaf Blueberry
(Vaccinium myrtilloides) need to be further domesti-
cated and/or managed in natural ecosystems to meet
the growing demand from the food and nutraceutical
industries (Duchesne et al. 2001). This paper describes
research conducted to improve blueberry management.
Canada is the world’s largest producer of wild blue-
berries (Lowbush and Velvet Leaf blueberries) with
an annual output of $42 425 million in farm gate value
resulting in production of 43 511 tonnes of frozen
blueberries (Agriculture and Agri-Food Canada 2002).
The demand for Lowbush and Velvet Leaf blueberries
is such that management of natural or established sites
is conducted to promote optimal yields ranging from
3360 to 8967 kg/ha (Mohammed 1999). Given that
blueberries are worth approximately $1.00/kg to farm-
ers, the annual output of managed fields ranges from
$3360 to $8967/ha, which is far superior to the aver-
age timber growth of Canada’s forests of 1.59 m°/ha/
year (Lowe et al. 1996) with an approximate value of
$100/ha/year.
Pruning of blueberry fields, either by mowing or
burning, is used routinely to maximize blueberry pro-
duction (Badcock 1958; Eaton 1958; Eaton and White
1960) as it stimulates the development of new shoots
from shallow rhizomes (Van Hoefs and Shay 1981). In
turn, new shoots are preferred over old shoots as the
ratio of flower buds to leaf buds is greater on new
shoots than on older shoots (Hall et al. 1972). Fire
pruning of blueberry fields is generally accomplished
by using straw as a fire carrier or tractor mounted oil or
propane gas burners that emit a constant flame (Blatt
et al. 1989). Burning also has the added advantage of
reducing problems with insects and disease (Blatt et
al. 1989; Smith and Hilton 1971). Although fire is
frequently used for the management of Lowbush and
Velvet Leaf blueberries (Blatt et al. 1989), which form
one commercial crop, there is a lack of information
about the relationship between fire behaviour and its
impact on berry production. Indeed, current prescrip-
tions aim at using fires that kill all stems (Blatt et al.
1989). However, fire behaviour varies a great deal even
during prescribed burns, which in turn affects the eco-
logical outcome of post-fire ecosystems (McRae et al.
2001).
195
196
Frontal fire intensity (or Byram’s fireline intensity)
is a measurement of the quantity of energy liberated as
a fireline moves through an ecosystem, and is the most
encompassing physical measurement of fire behavior
related to ecological impacts (reviewed by Alexander
1982 and McRae et al. 2001). Fire intensity is some-
times used together with depth of burn (Miller 1977),
which is a measurement of heat penetration into the
soil. However, both frontal fire intensity and depth of
burn are relatively new concepts in fire ecology and
have never been applied to blueberry management.
Hence, the objective of this study was to investigate
the effect of fires of different intensities and depth of
burn on Lowbush and Velvet Leaf blueberry pro-
duction and vegetative growth.
Materials and Methods
Study site
The study area is located at Frontier Lake (46°00’N,
77°33’ W) in a Jack Pine, Pinus banksiana, stand in
eastern Ontario within the middle Ottawa section (L.4c)
of the Great Lakes — St. Lawrence Forest region
(Rowe 1972). As reported by Herr et al. (1994), the
site is near the Petawawa Research Forest, and is rela-
tively flat, with a difference in elevation of approx-
imately 4 m over 1.0 km. The surface deposit is a
fine-grained and deep sand (10-30 m deep) (Gadd
1962) and the soil is a humo-ferric podzol. The study
site was selected because of its uniformity in tree com-
position and topography. It was harvested in 1942
and 1943 leaving residual standing timber with a stump
diameter of 17.5 cm or less. Dendrochronological
analysis of dominant trees and snags with multiple
fire scars suggests that the study site sustained sev-
eral fires, with the most recent in 1943, presumably
from broadcast slash burning following harvesting
(E. Stechishen, personal communication).
THE CANADIAN FIELD-NATURALIST
Vol. 118
Presently, the stand comprises a mix of Jack Pine
(Pinus banksiana), Red Pine (Pinus resinosa) and
White Pine (Pinus strobus) with the Red and White
pine forming an emergent layer (Herr et al. 1994).
Although the Jack and Red pine are of similar ages,
the Jack Pine has higher relative density and is the
dominant tree species on the site. Other plant species
found at the site include serviceberry (Amelanchier
sp.), Sweet Fern (Comptonia peregrina), Wintergreen
(Gaultheria procumbens), Sheep Laurel (Kalmia an-
gustifolia), Ground Pine (Lycopodium complanatum),
Cow Parsnip (Maianthemum canadense), Hairy Solo-
mon’s Seal (Polygonatum pubescens), Bracken Fern
(Pteridium aquilinum ) and Sand Cherry (Prunus
pumila).
Treatments
In the summer of 1990, an area of 150 m x 1000 m
was clear-cut with the slash left in place. The site was
divided into 40 plots of 35 m x 70 m with 8 m fire-
guards established around each plot. In 1991, ten plots
were burned under different indices of the Canadian
Forest Fire Weather Index (FWI) system (Table 1)
resulting in frontal fire intensities that varied from
597 to 21 305 kW/m and depth of burn that varied
from 0.37 to 2.78 cm (McAlpine 1995). This range
of fire intensity and depth of burn far exceeds the
range of fire behaviour currently used in blueberry
management (unpublished observations).
Pre- and post-burn fuel loads were measured for
both slash and duff fuels (McRae et al. 1979). Fire rate
of spread was measured with a pin grid network on
each plot; fire arrival times at each pin were recorded
to provide distance and time information. Fuel con-
sumption was determined as the difference between
these two values. Fire intensity was calculated using
Byram’s (Byram 1959: cited in McAlpine 1995)
TABLE |. Fire weather', fire behaviour parameters! and blueberry production from thirteen 35 m x 75 m plots in a clear cut
Jack Pine after prescribed burning of different fire intensities at Frontier Lake Experimental site in Eastern Ontario.
Plot Date Depth! of Intensity! Blueberries” Stem density* Blueberries/stem*
Number of burn! FWI! — Burn (cm) (kW/m) (g/m?) (stems/m?) (N/plant)
2 08/08/91 3.1 0.37 597 492.86 a (167.4) 73.2 a (8.5) 7.53 a (3.4)
7 08/08/91 3.6 0.38 1 268 242.18 a (79.44) 44.2 b (9.8) 5.52 a (1.6)
44 06/24/91 15.8 1.79 2 305 10.81 b (7.6) 5.9 c (0.7) 2.26 a (1.8)
40 07/10/91 4.3 2.78 4 844 114 b, (©@:9) 9.4 c¢ (2.9) 0.90 a (0.69)
32 07/12/91 9.6 1.85 7 600 8.78 b (8.7) 6.7 c (5.6) 0.53 a (0.46)
26 06/14/91 11.0 3.50 10 941 4.96b (4.8) 9.9 ¢ (7.1) 3.40 a (2.9)
46 06/24/91 17.4 1.95 12 065 ZO Mb Gels) 4.0 c (1.9) 3.10 a (2.7)
36 07/12/91 3.9 Dail 13 202 27.20b (8.9) 12.1 c (4.6) 2.59 a (1.13)
43 07/10/91 8.8 2.64 20 334 0.53b (0.24) 5.7 c (4.1) 0.50 a (0.42)
24 06/14/91 21.0 1.79 21 305 5.33b (0.48) 13.8 c¢ (2.4) 0.04 a (0.06)
Controls? — = — 9.01b (2.6) 5.9 c (1.48) 0.78 a (0.25)
' from McAlpine (1995).
* within column means followed by a different letter are significantly different at P < 0.05 determined by ANOVA. Observed
significance level was adjusted with the Bonferroni procedure.
> controls consisted of three unburned plots adjacent to the burned over plots.
2004
intensity equation I=HwR, where I is the intensity of
the fire (kW/m), H is the fuel low heat of combustion
(assumed to be 18 000 kJ/kg), w is the weight of fuel
consumed in the active front (kg/m?) (all fuel con-
sumed was assumed to have been burned by the active
fire front), and R is the rate of spread (m/sec).
To determine depth of burn, ten 50 cm steel pins
mounted with horizontal markers were used in each
plot to mark the top of the soil litter layer prior to each
burn. Immediately after the burn, the distance between
the horizontal marker and the top of the litter layer
was measured with a ruler and called depth of burn.
Two years following prescribed burning, there were
45 plant species in our research plots. The most impor-
tant species in terms the biomass and frequency (in
decreasing order of importance) were P. aquilinum,
V. angustifolium, V. myrtilloides, Amelanchier sp., P.
pumila, Comptonia peregrina, Kalmia angustifolia,
Yellow Panic-grass (Panicum xanthophysum), and
Houton’s Sedge (Carex houghtonii) (Tellier et al. 1995,
1996).
Blueberry collection
To compare the effect of fire intensity and depth of
burn, blueberries were collected two years after pre-
scribed fire from the ten burned over plots and from
three control plots. Controls consisted of three clear-
cut 35 m X 70 m plots adjacent to the burned-over
plots. Blueberries were not collected in subsequent
years because of logistical reasons limiting access to
the research plots.
For this study, three 3 m x 3 m quadrats were ran-
domly established in each of the 35 m x 70 m plots.
The perimeter of each of the 3 m x 3 m quadrats was
delineated with a string tied 40 cm above ground and
all berries within the 3 m x 3 m quadrats were picked,
advancing from the edge of the plot inwards. Ripe,
over-ripe, green, and deformed blueberries were in-
cluded in the harvest. All plots were harvested on 13
July and 14 July 1993. The harvested berries were kept
in plastic coolers in the shade until the end of the col-
lection day and their fresh weight determined in the
laboratory the same evening. The bags were then placed
in drying ovens at 50°C for 5 days before weighing.
Because the moisture content of blueberries (83.1 +
0.8 %) was comparable among all plots (P = 0.22)
and consistent with published data (Usui et al. 1994),
the results were expressed in terms of fresh weight only.
As well, no attempt was made to distinguish between
V. myrtilloides and V. angustifolium as the frequency
of these species (1:15- 1:30, myrtilloides: angustifoli-
um) was not significantly different among treatments
(S051):
To compare the effect of fire intensity and depth of
burn on the vegetative abundance of V. myrtilloides and
V. angustifolium, the number of stems of both species
was determined two years after prescribed fire from
the ten burned over plots and three control plots. Once
the berries had been removed from the 3 m x 3 m
DUCHESNE and WETZEL: EFFECT OF FIRE INTENSITY AND DEPTH OF BURN ON BLUEBERRY
197
quadrats, the number of stems was recorded for the
entire quadrat and expressed as stems/m/?.
As well, the number of blueberries/stem was com-
pared among the prescribed burns and the control.
For this, 100 stems were selected randomly outside
the 3 m x 3 m quadrats and the number of blueberries
determined for each stem. This protocol was repeated
in each of the ten prescribed burn plots as well as each
of the three control plots.
Statistical analyses
Analysis of variance (ANOVA) was conducted to
compare blueberry production, stem density and blue-
berry abundance/stem among the prescribed burns
and the controls (Systat 1997). For statistical analyses
the three control plots were pooled as one treatment
whereas each of the ten burned over plots was treated
as a separate treatment (McAlpine 1995). Means were
compared using the Bonferroni procedure (Systat
1997). Pearson’s multiple correlation analysis was con-
ducted to determine the relationship between frontal
fire intensity, depth of burn, berry production and the
number of blueberries/stem (Systat 1997).
Results
Blueberry production (g/m?) differed significantly
(P < 0.001) among treatments. The greatest blueberry
production was observed in prescribed fires of 597
and 1268 kW/m whereas there were no significant
differences among blueberry production of the other
treatments, including controls (Table 1). Likewise stem
density/ha differed among treatments (P < 0.001) and
was greatest in the fires of 597 and 1268 kW/m. There
was no difference in the number of blueberries/plant
among the other treatments including the controls
(P = 0.056).
Pearson’s multiple correlation analysis showed that
fire intensity correlated (P < 0.05) with blueberry pro-
duction, and stem density (Table 2). Depth of burn
correlated (P < 0.01) with blueberry production, stem
density and blueberries/plant. Depth of burn showed
better correlations with blueberry production, number
of blueberries/plant and stem density than fire inten-
sity (Table 2).
Discussion
Several studies have demonstrated that the response
of ecosystems varies greatly with frontal fire intensity
and depth of burn. Fire intensity has been shown to
correlate with P. banksiana regeneration (Weber et al.
1987) and post-fire abundance of P. aquilinum (Tellier
et al. 1995). Low fire intensities stimulated Corylus
cornuta sprouting and height growth of Rubus ideaus
(Johnston and Woodard 1985). Biomass nutrient reten-
tion (Duchesne and Tellier 1997) and soil seed bank and
competing vegetation dynamics along with P. resinosa
and P. strobus seedling performance are also affected
by prescribed burning intensity (Tellier et al. 1995,
1996; Whittle et al. 1997). Soil microbial activity and
198
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 2. Pearson’s multiple correlation analysis among fire intensity, depth of burn, blueberry biomass, number of blueberries/
stem, and stem density.
Intensity Blueberries/ha
Intensity 1.000
Blueberries/ha -0.507* 1.000
Depth of burn 0.517% -0.683**
Blueberries/stem -0.461 0.803**
Stem density -0.504* 0.766**
* significant at P < 0.05
** significant at P < 0.01
diversity were also affected by fire intensity (Duchesne
and Wetzel 2000; Staddon et al. 1998a, 1998b).
Fire has been used for hundreds of years in blue-
berry management by Indigenous people (Chapeskie
2001) and by farmers (Badcock 1958; Blatt et al.
1989), mostly using spring fires. This investigation
presents the first comprehensive data on the effect of
fire intensity and depth of burn on natural blueberry
production, which are indicated as critical factors to
consider in blueberry management. Indeed, the current
findings show that fire intensity must be kept low in
order to increase blueberry productivity using pre-
scribed fire. As well, care must also be given to reduce
depth of burn, which has a greater impact on blueberry
production than fire intensity (Table 2). Whereas fire
intensity is a measure of the caloric energy liberated by
the fire front (Alexander 1982), depth of burn integrates
the interaction between soil moisture conditions and
fire intensity (Miller 1977) and is more closely linked
to the response of blueberries to fire than fire intensity.
Since blueberry shoots arise from shallow rhizomes
and portions of the above ground stem not killed by
the fire (Flinn and Wein 1977; Martin 1955: Minore
1975), deep heat penetration in the humus layers is
likely to reduce stem production. Similar conclusions
have been reached in Ponderosa Pine (Pinus ponder-
osa) forests where depth of burn influenced greatly
understory species regeneration (Armour et al. 1984)
which is consistent with the concept that depth of
buried propagules, together with heat penetration, is
critical in post-fire survival (reviewed by Whittle et al.
1997). In turn, the differences observed in this inves-
tigation in post-fire blueberry stem densities, and the
negative correlation between stem density and depth
of burn may be ascribed to the deleterious effect of
fire on the underground rhizomes as was demonstrated
on Blue Huckleberry (Vaccinium globulare) (Miller
L977):
In practice, blueberry production can be maximized
by burning in the spring of every second year, presum-
ably to maintain a high ratio of flower buds to leaf buds
(Hall et al. 1972). In this investigation, the number of
blueberries/plant, which was hypothesized to be an
Depth of burn Blueberries/stem Stem density
1.000
=O ei 1.000
-0.724** 0.471 1.000
estimate of the flower bud to leaf bud ratio, was not
significantly different among treatments but inversely
correlated with fire intensity. These results cannot be
explained by conventional thinking regarding flower
bud formation (Hall et al. 1972), as the number of blue-
berries/plant correlated with depth of burn. However,
Smith and Hilton (1971) speculated that Lowbush
Blueberry performance after fire pruning might result
from the stimulative effects of the nutrients in ash
deposited on the surface soil during burning. Further
investigation is needed to assert the relevance of this
hypothesis in blueberry flower biology.
Although this investigation shows that low intensity
fires have a positive influence on blueberry production,
natural blueberry ecosystems support a variety of wild-
fire characteristics (Moola et al. 1998; Usui et al. 1995).
Hence the continuous effect of repeated fires should be
investigated on the long term productivity and biologi-
cal conservation of such ecosystems. In particular, it
will be important to assess the impact of burning every
second year, which is the recommended practice, on
soil nutrients (Smith and Hilton 1971). Future work
should also be conducted to investigate co-manage-
ment of blueberries with timber values (Duchesne et
al. 2001).
Documents Cited (marked * in text)
Agriculture and Agri-Food Canada. 2002. Canadian fruit
situation and trends. http://www.agr.gc.ca/misb/hort.
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Received 12 June 2002
Accepted 24 September 2004
Spring Dispersal Patterns of Red-winged Blackbirds, A gelaius
phoeniceus, Staging in Eastern South Dakota
H. J. Homan!, G. M. Linz!, R. M. ENGEMAN?, and L. B. PENRyY!
'U.S. Department of Agriculture, National Wildlife Research Center, 2110 Miriam Circle, Bismarck, North Dakota 58501-
2502 USA
2 U.S. Department of Agriculture, National Wildlife Research Center, 4101 LaPorte Avenue, Fort Collins, Colorado 80521 -
2154 USA
Homan, H. J., G. M. Linz, R. M. Engeman, and L. B. Penry. 2004. Spring dispersal patterns of Red-winged Blackbirds,
Agelaius phoeniceus, staging in eastern South Dakota. Canadian Field-Naturalist 118(2): 201-209.
Red-winged Blackbirds (Agelaius phoeniceus) are very abundant summer residents throughout the Prairie Pothole Region
of central North America. In late summer they assemble in post-breeding flocks that cause significant amounts of agricul-
tural damage, particularly in sunflower fields near natal sites. In April 2001, we aerially color-marked ~370 000 Red-winged
Blackbirds near Badger, South Dakota (44°48'N, 97°21'W), to determine if migrants staging here were summer residents in
sunflower production areas ~350 km to the northwest. We measured patterns of migratory dispersal by collecting birds in 54
randomly selected blocks in the northcentral U.S. and the Prairie Provinces of Canada. The marked specimens (n = 33) were
categorized into three polygons based on analyses of banding and re-sighting data and proximity to concentrated sunflower
production. We estimated that 82% of the migrants that had staged in eastern South Dakota resided. within or on the
periphery of the sunflower growing area. These birds probably stay near their breeding territories until at least late August
and cause early damage to sunflower, which comprises the majority of damage. Resident birds in Alberta and most of
Saskatchewan (18%) might arrive too late in the damage season to impact the sunflower crop significantly.
Key Words: Agelaius phoeniceus, Red-winged Blackbird, breeding range, color-marking, dispersal patterns, northern Great
Plains, spring migration, sunflower damage.
Several million hectares of wetlands have been
drained in the Prairie Pothole Region (Dahl 1990*), but
high densities of semipermanent wetlands remain in
North Dakota (0.88/km?, Reynolds et al. 1997*). These
are preferred nesting habitat of Red-winged Black-
birds (Agelaius phoeniceus) and make North Dakota
the center of abundance for this species. During the
mid-1990s, the breeding population in North Dakota
started gaining rapidly in size. Red-winged Blackbird
indices from the North American Breeding Bird Sur-
vey (BBS) are at historical highs for the state (Figure
1). From 1994-2002 North Dakota’s average BBS index
of all routes in the Prairie Pothole Region ranged
from 199 to 250 Red-winged Blackbirds per route.
North Dakota led all other U.S. states and Canadian
provinces during this period in annual indices of Red-
winged Blackbirds (Sauer et al. 2004*). Conflicts bet-
ween wildlife and agriculture often occur because of
local overabundance (Garrott et al. 1993; Conover
2002), and the growth in numbers of Red-winged
Blackbirds has exacerbated a long-term struggle bet-
ween sunflower producers and blackbirds (Linz and
Homan 1998). Oilseed sunflower is a preferred food
of Red-winged Blackbirds (Linz et al. 1984; Homan
et al. 1994). It is also an important economic crop in
North Dakota. In 2001, 75% of total oilseed sunflower
production in North America came from North Dakota
(National Agricultural Statistics Service 2004*). With
increased depredation pressure on the crop caused by
population expansion of Red-winged Blackbirds, many
growers probably dropped sunflowers from their field
rotations (Lamey and Luecke 1994). Since 1995, the
number of sunflower fields has steeply declined in cen-
tral and southeastern North Dakota, areas renowned for
their high levels of sunflower production (National
Agricultural Statistics Service 2004*).
Statewide field damage surveys have that blackbird
damage to sunflower ranges from $4 to 11 million
(U.S. dollars) in the Prairie Pothole Region (Hothem
et al. 1988). Based on current population estimates and
bioenergetic models, Red-winged Blackbirds cause
$3 million of the $5.5 million lost yearly to blackbirds
in the core area of sunflower production (Peer et al.
2003). Most of the damage occurs between mid-August
and early September, when the calorie content of im-
mature sunflower achenes is low and the birds must
eat more to reach satiation (Cummings et al. 1989; Con-
ner and Hall 1997). During this early damage period,
when >75% of total damage occurs, Red-winged
Blackbirds account for 80% of the blackbird species
observed in sunflower fields (Cummings et al. 1989).
This period is before en masse blackbird migration, and
the majority of these birds are of local origin. Most will
remain within 200 km of their natal sites until molt
completion (or near completion) in late August and
early September (Dolbeer 1978; Besser et al. 1983;
Linz et al. 1983). The damage can be quite serious in
central and southeast North Dakota and northeast South
Dakota, areas of concentrated production of sunflow-
ers (National Agricultural Statistics Service 2004*) and
201
202
plentiful wetlands to attract nesting Red-winged Black-
birds (~22 breeding pairs/km7, Linz et al. 2002). By
late summer, the Red-winged Blackbird population
responsible for most of the sunflower damage in the
Prairie Pothole Region is about 39 (+8.8) million (Peer
et al. 2003).
Reducing excessive field damage (e.g., >10% per
field) has proven an enormous challenge. The U.S.
Department of Agriculture (USDA) uses an integrated
management approach of lethal and nonlethal methods.
Most of the available methods are used infrequently
because of unmanageable logistics, little or no efficacy,
or low cost:benefit ratios (Linz and Hanzel 1997).
Mechanical frightening agents (e.g., scarecrows, pyro-
technics, and propane cannons) help alleviate light
predation pressure, but only work effectively if the dur-
ation of the damage period is less than the habituation
period (Cummings et al. 1986). Unfortunately, black-
birds habituate quickly to frightening agents, particu-
larly if the crop is a preferred food in an area of limited
alternate foods (Ward 1979). The taste repellent, methyl
anthranilate, is also used by producers, but the con-
centration in the commercial product (BirdShield™)
is below the known repellency threshold, despite the
formulation’s high cost (Werner et al. 2005). Experi-
ments with avicide were tried in sunflower fields with
ongoing damage. Avicide-treated rice (DRC-1339)
was placed in small plots opened in the fields. This
approach failed because (1) blackbirds foraged almost
exclusively on the standing heads of sunflower and
would not go to the ground to forage in the plots, (2)
precipitation necessitated numerous rebaitings, and
(3) nontarget avian risks increased substantially over
the baiting period because of migration (Schaaf 2003;
Linz et al. 2000). Two nonlethal methods showing
some promise are reduction of dense stands of cattail
(Typha spp) in wetlands near sunflower (Linz et al.
2004a) and strategic placement of lure crops to attract
foraging blackbirds away from sunflower fields (Linz
et al. 2004). Cattail management has been a USDA
program for over 10 years. The program is small com-
pared to existing coverage of cattail (Ralston et al.
2004); and it also faces year-to-year logistical chal-
lenges because of instability in roost locations across
years combined with cattail’s ability to rapidly invade,
colonize, or re-colonize wetlands (Homan et al. 2003).
Research on efficacy of lure crops is just beginning
and time will be needed to assess this method.
Sometimes population management may be the most
realistic and effective method for reducing persistent
damage caused by overabundant wildlife populations
(Garrott et al. 1993). The definition of overabundance
is subjective and based upon one’s interests, likes, and
dislikes; and therefore is controversial. It has been
defined generally as that point of abundance where all
positive values of the species have been overwhelmed
by negative values created by the sheer numbers of indi-
viduals (Conover 2002). The definition implies both a
THE CANADIAN FIELD-NATURALIST
Vol. 118
spatial and temporal component, as populations are
seldom ubiquitous or always aggregated. The defini-
tion is fitting, at least from an agricultural perspective,
in the sunflower growing areas of North Dakota and
northeastern South Dakota. The USDA has drafted an
Environmental Impact Statement (EIS) that addresses
the conflict between sunflower producers and black-
birds in North Dakota, South Dakota, and Minnesota
(Federal Register 2001*). Several management options
were included in the draft EIS. The research described
herein addresses one of the options being considered:
population management of spring migrating Red-
winged Blackbirds in northeastern South Dakota. This
part of South Dakota is one of the most northward sites
where the population is still grouped together enough
to make population management a feasible alternative.
Because blackbird damage to sunflower is a local-
ized phenomenon occurring within the broader region
of the northern Great Plains (Peer et al. 2003), it is nec-
essary to identify specific origins of local populations
before implementing any strategy of population man-
agement. Although leg-banding has provided valu-
able insights into migratory timing and dispersal of
Red-winged Blackbirds (Dolbeer 1978), this method
draws its samples randomly from regional populations.
Moreover, it is labor intensive in both its capturing
and ringing methods; these drawbacks combined with
natural annual mortality of Red-winged Blackbirds
cause data to be parsed over several years because of
extremely low rates of band returns (<0.5%, Besser et
al. 1983; Gammell et al. 1986; Stehn 1989). An alterna-
tive method of tracking movements, aerial mass color-
marking, provides a means for rapid accumulation of
data on movements of local populations within a single
season framework. Recovery rates from mass color-
marking projects depend on the number marked com-
pared to the size of the study population (Johns et al.
1989): however, thousands of birds can be marked in
a single application often yielding a rate of return 10
to 20 times that of leg-banding. Aerial mass color-
marking has been used to track spring movements of
Red-winged Blackbirds from northeastern Missouri
and eastern South Dakota (Knittle et al. 1987; Knittle
et al. 1996), short late-summer movements of Red-
winged Blackbirds in central North Dakota (Linz et
al. 1991), and movements of Red-winged Blackbirds
between winter roosts in the southcentral U.S. (Harsch
1995*). The marking formulation is environmentally
safe at the concentrations used (Bills and Knittle 1986;
Knittle and Johns 1986).
In April 2001, we used aerial mass-marking to iden-
tify migrating Red-winged Blackbirds staging in large
cattail-dominated wetlands in northeastern South Da-
kota. Millions of spring migrating blackbirds annu-
ally stage at this traditional stopover site between late
March and April (Sawin 1999). Our objective was to
assess migratory dispersal to breeding territories north
of the marking site. Previous research has shown that
2004 HoMaAn, LINZ, ENGEMAN, and PENRY: DISPERSAL PATTERNS OF BLACKBIRDS 203
250
200
North Dakota
L
5 “,
a 150 ree %
= Fi
g NL * Saskatchewan
7) oe ‘
— « Le
= 5 a _Manitoba
8 100 rid PO eee ee a ims
” i
a Fd
a ”
© Alberta
= 50
0
< 2 2 2 ND 2 £
Year
Ficure 1. Three-year rolling averages of indices from the North American Breeding Bird Survey from 1967 to 2003. The in-
dices are from routes in the Drift Prairie, Glaciated Missouri Plateau, and Aspen Parklands, which are the three major
physiographic regions in the Prairie Pothole Region used most frequently by Red-winged Blackbirds.
color-marked male Red-winged Blackbirds staging
in eastern South Dakota during spring were in part
destined for breeding grounds in or near concentrated
sunflower production; however, these data were col-
lected over 15 years ago (Knittle et al. 1987; Knittle
et al. 1996). Population management programs, when
used at sites far from the locality where actual damage
occurs, must be based on a thorough and contempo-
rary knowledge of movements of individual popula-
tions (Dolbeer 1978). We believed it necessary to repli-
cate the marking studies because changes may have
occurred in migratory patterns. Additionally, no data
exist on dispersal movements of females, and these
data would increase our understanding of the popula-
tion’s migration patterns.
Methods
Marking
During March 2001, we monitored cattail-dominat-
ed wetlands in six counties in eastern South Dakota
for arrival of migratory flocks of blackbirds. Three wet-
lands held migratory roosts large enough (>10 000
birds) to warrant aerial mass-marking. All three roosts
were within a 32-km radius of Badger, South Dakota
(44°48'N, 97°21'W). Roost size was estimated by
counting blackbirds as they entered the roost on the
evening of the spray (Meanley 1965; Arbib 1972). Spe-
cies compositions and sex compositions were estimat-
ed by randomly selecting and identifying groups of
individual birds as they entered (Dolbeer et al. 1978).
A fixed-wing agricultural spray plane applied the
marker near dark at an altitude of 20—30 m (Knittle et
al. 1987). The following morning we collected birds
as they departed the sprayed roost and later examined
them for fluorescent marks using a long-wave (360 nm)
ultraviolet light. We calculated the number of marked
male and female Red-winged Blackbirds in the roost
by multiplying the proportion of marked birds in the
sample by the estimated number of males and females
using the roost on the night of the spray.
The marker formulation was a 416-L solution con-
sisting of 208 L Carboset® (an acrylic adhesive; Nov-
eon™ Incorporated, Cleveland, Ohio), 102 L food-
grade propylene glycol, 7.7 kg fluorescent organic pig-
ment (DayGlo® Color Corporation, Cleveland, Ohio),
1 L each of a defoamer and surfactant, and 106 L
water (Knittle et al. 1996). We used CP® nozzles set at
5 (400 micron droplets). Spray volume was 28L/ha
delivered at 1.8 kg/cm’. In spray form the solution
dries in 2-3 minutes adhering to the feather surface.
204
Knittle and Johns (1986) found that 5% of marked birds
lost their marks within six weeks; however, particles
lodged in the barbules can remain until molt (Knittle
et al. 1996; Otis et al. 1986).
Sampling and Collections
We grouped the study area into 140 blocks, each
consisting of four 1°-latitude x 1°-longitude units. Two
units were randomly selected from each block. To en-
sure adequate sample sizes per effort, only those units
within regions that averaged 230 Red-winged Black-
birds per BBS route were selected (Sauer et al. 2004);
37 units in Canada and 19 units in the U.S. were chos-
en in this manner. No units south of the 1° x 1° unit
containing the marking sites were sampled. The sam-
ple units covered an extensive area (>1.0 x 10° km?)
bounded by 44—57° N latitude and 95—119° W longi-
tude (Figure 2). Southwestern North Dakota, central
Minnesota, central and western South Dakota, and
southeastern Montana were excluded because BBS
counts were <30 (Sauer et al. 2004).
We assigned the 1° x 1° units to one of three disper-
sal polygons: core, peripheral, and outside-peripheral
(Figure 2). The shape and area of the polygons were
based on an analysis of banding and re-sighting data,
physiography, and proximity to the area of concen-
trated sunflower production (Stehn 1989). The core
polygon encompassed the breeding range of birds hav-
ing a high probability of causing early damage to sun-
flowers. The peripheral polygon contained the sur-
rounding breeding range of birds that were capable
(with only short pre-migratory movements) of entering
the core area during the early damage period (mid-
August — early September) (Dolbeer 1978; Gammell
et al. 1986). The outside-peripheral polygon contained
the birds farthest removed from the core area and en-
compassed the rest of the study area not covered by
the core and peripheral polygons. The 1° x 1° units
were placed in core and peripheral polygon categories
if any of the unit’s area intercepted the polygon’s bound-
ary. We used a GIS to place the polygons on a geo-
referenced grid of the 1° x 1° units.
We used shotguns (12-gauge with either #6 or #7/
steel shot) to collect male and female Red-winged
Blackbirds on breeding territories during June in the
U.S. and June and early July in Canada. The wings
were removed from the specimens and placed in an
envelope with the GPS coordinates of the collection
site. The wings were later viewed for fluorescent pig-
ments using a 360-nm ultraviolet lamp under 1.75 mag-
nification. The markings on tagged birds are usually
subtle and invisible to the naked eye under natural
light. To eliminate false positives, only splash marks
and individual particles firmly attached to the feathers
were considered conclusive evidence of a valid mark
(Knittle et al. 1987). Blood samples were removed on-
site from randomly selected specimens and used for
microsatellite genetic analysis in a separate study
(Williams et al. 2004). The wings were frozen and shall
THE CANADIAN FIELD-NATURALIST
Vol. 118
be kept for future research on primary feather chem-
istry and its relationship to geographic origins (Ed-
wards and Smith 1984).
The data were analyzed using descriptive statistics,
likelihood ratio chi-square analyses (G-tests), and non-
parametric tests. We used G-tests to assess differences
between (1) the proportion of marked birds (sexes com-
bined) in the sample with the expected proportion of
marked birds in the study area; (2) the proportions of
marked males and females in the sample with the ex-
pected proportions of marked males and females in the
study area; and (3) the proportions of marked birds
within core, peripheral, and outside-peripheral poly-
gons. The first two tests used extrinsic expected fre-
quencies based on estimates of marking efficiency at
the staging site and population size in the study area
during the breeding season. The third comparison used
intrinsic frequencies generated exclusively from the
collections (Sokal and Rohlf 1981). Population size
in the study area was estimated using a combination
of stable age structure analysis from banding data and
linear regression analysis of BBS indices and inde-
pendently determined density estimates (Stehn 1989).
The resultant regression equation was Y = 0.3X, where
X was the average BBS count within each ecological
stratum in the study area and Y was the population den-
sity per km? (see Aldrich 1963; Robbins et al. 1986).
We used the Wilcoxon Rank Sum test to compare
ranked differences between males and females in dis-
tances traveled from the marking site to the collecting
sites. Distance measurements were made using a GIS.
Results
We applied fluorescent marker seven times, tagging
an estimated 235 500 male and 131 100 female Red-
winged Blackbirds over the period 1-23 April. This
period covered the Red-winged Blackbird migration
through eastern South Dakota in 2001. We collected
2398 males and 2060 females on breeding territories,
of which 33 (0.74%) were marked (Table 1). The
overall recovery rate of 0.74% was similar to the
expected recovery rate of 0.96% (G = 1.1, P = 0.30),
based on total number of birds marked in April and the
estimated population size of breeding Red-winged
Blackbirds in the sampled collection area (38.1 x 10°,
from Stehn 1989) which included the population in
the outside-peripheral polygon. The ratio of marked
males : females in the sample (f = 23 : 10) was near
the expected ratio of 22 : 11 (G = 0.07, P = 0.80).
Proportions of marked birds collected in the three
polygons differed (G = 6.44, P = 0.04), with the per-
centages of marked birds in the core polygon (1.03%)
and peripheral polygon (0.93%) nearly three times
greater than the percentage collected in the outside-
peripheral polygon (0.35%) (Table 1). The outside-
peripheral polygon contributed 69% of the total G-
value. Of the 33 marked recoveries, 15 (46%) were
collected in the core polygon and 12 (36%) were
collected in the peripheral polygon.
2004 Homan, LINZ, ENGEMAN, and PENRY: DISPERSAL PATTERNS OF BLACKBIRDS 205
Outside-peripheral
polygon
Peripheral polygon
Core polygon
Axel
study block
© Female N
A Male A
3x Marking site 300 0 300 Kilometers
a okt
FiGurRE 2. Locations of 33 marked Red-winged Blackbirds (in relation to core, peripheral- and outside-peripheral polygons)
after dispersing from a spring staging site in eastern South Dakota in April 2001.
TABLE 1. Color-marked male (©’) and female (Q) Red-winged Blackbirds collected during June and July 2001 in core,
peripheral, and outside-peripheral polygons after migratory dispersal from a staging site in eastern South Dakota during
April 2001.
Number Number Number Percent
units? Collected Marked Marked
Polygon ‘os O Total ‘oi fe) Total ol Q All
Core 14 793 668 1 461 9 6 15 eit} 0.90 1.03
Peripheral 15 681 605 1 286 10 2 12 1.47 0.33 0.93
Outside 27 924 787 Lala 4 D 6 0.43 0.25 0.35
Total 56 2 398 2 060 4 458 2B 10 33 0.96 0.48 0.74
4No
birds were collected in two units
206
No marked birds were collected north of 53° N.
Recovery distances were similar between sexes (T =
0.18, P = 0.86), with the median location 519 km
(range: 20-1353) from the marking sites (48°23'N,
100°27'W). The median azimuth from the marking
sites was 325°. The median distance and direction of
marked females placed them on the northwestern side
of the core polygon (48°23'N, 100°27'W; whereas,
males were 70 km due west (48°30'N, 101°23'W), in
the peripheral polygon. For all recoveries combined,
the median location was 50 km northeast of Minot,
North Dakota (48°14'N, 101°18'W).
Discussion
The seven sprays were evenly distributed through-
out the migratory period and probably yielded an
accurate depiction of the migratory distribution pat-
terns of Red-winged Blackbirds. Similar to the results
of previous banding and color-marking experiments
in eastern South Dakota, our data showed that most
birds followed the Prairie Pothole Region as they
traveled northwest to their breeding territories (Besser
et al. 1983; Knittle et al. 1987; Knittle et al. 1996).
Although Red-winged Blackbirds are not confined to
breeding in this region, they are found here in their
highest densities. A statewide population census of
breeding birds in North Dakota showed that the Prairie
Pothole Region (comprised of several physiographic
regions, but mainly the Drift Prairie and Glaciated
Missouri Plateau) contained 70% of the state’s Red-
winged Blackbird population (Stewart and Kantrud
1972).
Unlike parameters such as median distance and
direction, both of which can be influenced by differ-
ences in breeding densities over the study area, the pro-
portions of marked birds within the three polygons were
distribution measures mathematically independent of
density. It was thus possible to consider our results as
reflections of behavioral phenomena, such as fidelity
to migratory pathways and philopatry. The marked
population was apparently not distributing itself ran-
domly in the study area. The low proportion of marked
birds in the outside-peripheral polygon suggested that
eastern South Dakota may be used mainly by migrants
already near their final destination, and as a result,
traveling relatively short distances after departure from
the staging site. We speculate that other staging sites
might exist (perhaps much farther to the west), and
these should have birds destined for breeding territories
in Montana, southern Alberta, and Saskatchewan.
Marking of large roosts farther west (for example, a
large blackbird roost exists near Great Bend, Kansas
[38° 22'N, 98° 49'W]) may demonstrate that western
migratory pathways exist distinct from the one used by
blackbirds in eastern South Dakota. Certainly, the very
low proportion of marked birds in the outside-periph-
eral polygon, compared to the other two dispersal
polygons, suggests a different population of birds.
THE CANADIAN FIELD-NATURALIST
Vol. 118
There were two other marking studies done in the
general vicinity of our marking site. These were done
at Lake Thompson, South Dakota (44°23'N, 97°33'W),
approximately 30 km to the southwest. Both were
similar in design, scope, and sampling effort to our
study, except that only males were collected. One study
was conducted in 1983 (Knittle et al. 1987), the other
in 1985 (Knittle et al. 1996). Even though geopolitical
boundaries were used to analyze returns instead of dis-
persal polygons, comparisons of results among and
between studies can still be made. Results were similar
between our study and the 1983 study in two impor-
tant facets: (1) the recovery rate of marked birds in
Canada was substantially lower than the U.S. recov-
ery rate (4.4 vs. 7.0%, Knittle et al. 1987), and (2)
proportions of marked birds collected in western North
Dakota, central North Dakota, and northeastern South
Dakota were greater than other regions. By contrast,
results diverged in the 1985 study, both from our results
and from those from the 1983 study. The expected
rate of recovery in the 1985 study was much less than
the observed recovery rate (5.2 vs. 14.6%, Knittle et
al. 1996). To obtain a 14.6% recovery rate, the male
population would have had to have been 6.7 x 10°, a
number 65% lower than what was estimated in the
study area during that time (19.0 x 10°, Stehn 1989).
Saskatchewan’s Red-winged Blackbird population
had indeed been in steep decline for nearly a decade,
as evidenced by BBS indices (Figure 1); however,
trends for Alberta, Manitoba, and North Dakota were
either stable or increasing. It is unlikely for such a
conspicuous species that a 65% decline would be
missed in the BBS surveys. Of course, the number of
birds marked in 1985 could have been underestimated
by this magnitude, but an even more anomalous result
in the 1985 study argues against this; the percentage
of marked birds in Canada was greater than the per-
centage marked in the Prairie Pothole Region below
49° N (17 vs. 16%). Usually, recovery rates are inverse-
ly related to the distance traveled from a marking site
because unmarked populations arriving by other routes
from other areas dilute the proportion of marked birds.
Although it is conceivable that the Red-winged Black-
bird population marked at Lake Thompson in 1985
migrated beyond traditional nesting areas and immi-
grated into Canada, perhaps seeking better wetland
conditions, band recoveries collected over several dec-
ades have shown that Red-winged Blackbirds usually
return to within 100 km of their natal sites (Nero
1956; Dolbeer 1978). If Red-winged Blackbirds were
not philopatric, but nomadic or irruptive, we contend
that large fluctuations in BBS counts would occur
among physiographic regions comprising the Prairie
Pothole Region. No significant correlations existed in
yearly changes in BBS indices between North Dakota
and the three Prairie Provinces within our study area,
and perusal of average BBS indices over a 36-year
period does not seem to indicate irregular migratory
aegnnce
behavior (Figure 1). The extraordinarily high overall
recovery rate of marked birds in the 1985 study may
have resulted from improper identification of marks
(i.e., false positives) caused by environmental contam-
ination with fluorescence pigments used for identifying
insecticide formulations and fertilizers (Knittle et al.
1987). We believe that our data from 2001 and the data
from the 1983 study have provided the most accurate
analyses of dispersal patterns of migrating Red-winged
Blackbirds in eastern South Dakota.
Summary and Conclusions
In landscapes with numerous wetlands, blackbird
damage to sunflowers averages 25% per field. One-
quarter of the fields receive >10% damage (Linz et al.
2000). At the 10% damage level, agricultural producers
start dropping sunflower from their crop rotations and
replacing it with other oil crops, such as soybean and
canola (North Dakota Agricultural Statistics 1990*;
Lamey and Luecke 1994). There is no evidence that
the rapid population growth of Red-winged Blackbirds
has directly affected other bird species; however, the
potential for indirect effects exists. Sunflower fields
were used by 49 nonblackbird species, representing all
the major feeding guilds, during the late-summer and
early fall migrations (Schaaf 2003). Sunflower fields
have several characteristics that could make them excel-
lent migratory stopover sites for rest, cover, and pro-
curement of energy reserves (Hutto 1998; Petit 2000).
First, they provide large blocks of sturdy herbaceous
cover with a dense canopy and rank understory in a
landscape that by mid-August is mostly barren north of
46°N because of the harvest of small grains (Schaaf
2003). Second, sunflower fields provide a diverse sel-
ection of foods, including seeds of weedy plants in the
furrows and numerous invertebrates in and around
the fields (Schulz 1978; Charlet et al. 1997; Schaaf
2003). This attracts avian granivores and insectivores
(and of course, the carnivores). Soybean and canola
fields, which often replace sunflower, have neither the
beneficial vegetative structure nor the energy and are
a less productive habitat for birds (Linz et al. 2004d).
Moreover, these crops are “clean cropped,” unlike sun-
flower, which is often not plowed until May of the fol-
lowing year. Sunflower stubble was used by 33 species
of migrating birds during early spring in North Dakota
(Galle et al. 2004). It was used more frequently
during spring migration than fields of soybean, small
grain, corn, and sorghum. Thus, loss of sunflower fields
in the Prairie Pothole Region could have unforeseen
ecological impacts on migrating nonblackbird species.
We estimate that 82% of the Red-winged Blackbirds
that stage in eastern South Dakota during spring migra-
tion reside either within or on the periphery of the sun-
flower growing area. If population management of
the spring breeding population in the northern Great
Plains is deemed the best of the EIS alternatives, we
suggest that the most efficacious strategy would be to
HoMAN, LINZ, ENGEMAN, and PENRY: DISPERSAL PATTERNS OF BLACKBIRDS
207
manage the population in eastern South Dakota. Lastly,
it may be possible to avoid impacting the Canadian
migrants, which comprised 18% of the birds staging in
eastern South Dakota, by not applying management
over the entire migration. Canadian Red-winged Black-
birds should be among the last of the regional popula-
tions of Red-winged Blackbirds to arrive at the stag-
ing site (Weatherhead and Bider 1979). The arrival of
Yellow-headed Blackbirds (Xanthocephalus xantho-
cephalus), a nontarget blackbird species, usually signi-
fies that the Red-winged Blackbird migration is nearing
its end and may be a good indicator to cease manage-
ment operations.
We recommend future research on (1) genetic
markers to identify local populations of Red-winged
Blackbirds residing in Canada and the U.S.; (2)
color-marking spring migrants in flyways farther west;
(3) the relationship between timing of arrival at stag-
ing sites and distance traveled to breeding territories;
and (4) color-marking pre-migratory roosts [or other
means of identification, such as genetics or mineral
analyses of primary feathers] northwest of the core
sunflower growing area prior to fall migration.
Acknowledgments
Personnel from North Dakota/South Dakota Wildlife
Services and North Dakota State University helped
collect the birds. We thank the following for their sup-
port and cooperation on this project: the Departments
of Agriculture of North Dakota and South Dakota; the
U.S. Fish and Wildlife Service; Minnesota Department
of Natural Resources; North Dakota Game and Fish
Department; South Dakota Department of Game, Fish
and Parks; South Dakota Department of Environment
and Natural Resources; Montana Department of Fish,
Wildlife and Parks; Canada Customs and Revenue
Agency; Canada Department of Foreign Affairs and
International Trade; the Environmental Protection
Branch of Environment Canada; the Wildlife Branch
of Manitoba Conservation; the Environment Branch
of the Alberta Natural Resource Service; the Fish and
Wildlife Branch of Saskatchewan Environment and
Resource Management; the Manitoba Wildlife Animal
Care Committee and Animal Care Committees within
other provincial, federal, and state governments; the
National Sunflower Association; and private landown-
ers in the U.S. and Canada. Our research was conduct-
ed under the auspices of Quality Assurance Study Pro-
tocol QA-776, as amended; as such, safety guidelines,
animal care, and scientific validity were reviewed,
approved, and permitted by the National Wildlife
Research Center, the U.S. Fish and Wildlife Service,
the Environmental Protection Branch of Environment
Canada, and the natural resource agencies in the states
and provinces within the study area. Use of commercial
products by the U.S. Government does not constitute
an endorsement of these products.
208
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Changes in Loon (Gavia spp.) and Red-necked Grebe (Podiceps
grisegena) Populations in the Lower Matanuska-Susitna Valley, Alaska
TAMARA K. Mitis!* and BRAD A. ANDRES2*
' Department of Biological Sciences, University of Alaska Anchorage, 3211 Providence Drive, Anchorage, Alaska 99508
USA
2 U. S. Fish and Wildlife Service, Nongame Migratory Bird Management, 1011 East Tudor Road, Anchorage, Alaska 99503
USA
> current address: U. S. Fish and Wildlife Service, Nongame Migratory Bird Management, 1011 East Tudor Road, Anchorage,
Alaska 99503 USA
* current address: Division of Migratory Bird Management, U. S. Fish and Wildlife Service, P.O. Box 25486, DFC-Parfet,
Denver, Colorado 80225-0486 USA; corresponding author
Mills, Tamara K., and Brad A. Andres. 2004. Changes in loon (Gavia spp.) and Red-necked Grebe (Podiceps grisegena)
populations in the lower Matanuska-Susitna Valley, Alaska. Canadian Field-Naturalist 118(2): 210-214.
More than two-thirds of the human population of Alaska resides in the south-central portion of the state, where its continued
growth is likely to affect some wildlife populations negatively. To assess changes in waterbird populations in this region, we
compared counts of Common Loons (Gavia immer), Pacific Loons (G. pacifica), and Red-necked Grebes (Podiceps
grisegena) made on Matanuska-Susitina Valley lakes. In general, the number of lakes occupied by loon or grebe pairs
decreased between 1987 and 1999. Decreases in the number of lakes occupied by Common Loons were less drastic in the
northwest region of the study area than in the southeast region; human development is greater in the southeastern portion of
our study area. Contrary to lake occupancy, the percentage of lakes that fledged Common Loon chicks remained stable between
years. Because the human population is expected to continue to grow, proactive management of lake use and lakeshore
development, coupled with monitoring of loon and grebe occupancy and productivity, is needed to ensure the persistence of
these waterbird populations in the lower Matanuska-Susitna Valley.
Key Words: Common Loon, Gavia immer, Pacific Loon, Gavia pacifica, Red-necked Grebe, Podiceps grisegena, breeding
occupancy, productivity, south-central Alaska.
The stability of many bird populations mainly de-
pends on the stability of the environments they inhabit
(Newton 1998). Nesting loons (Gavia spp.) and grebes
(Aechmophorus spp., Podiceps spp.) are often nega-
tively affected by habitat degradation and increased
levels of human-related disturbances (Riske 1976;
McIntyre 1978; Evers 2003). Common Loons (Gavia
immer), Pacific Loons (G. pacifica), and Red-necked
Grebes (Podiceps grisegena) breeding on lakes in the
Matanuska-Susitna Valley (Mat-Su Valley), Alaska, are
encountering many changes to their local environment.
The area’s human population has tripled in the last two
decades, and the current annual growth rate is 3.3%
(McKibben and Nelson 1999*). Within the Mat-Su
Valley, population growth has been greatest in the
southeast, the area closest to Alaska’s largest city
(Anchorage; McKibben and Nelson 1998*, 1999*),.
The growing human population in the Mat-Su Valley
has begun to encroach upon the freshwater habitat
favored by breeding loons and grebes. Development of
lake shorelines for houses and increased recreational
use of lakes are suspected of having detrimental effects
on loon and grebe populations in the Mat-Su Valley
(Tankersley 1987*, Fair 1998*).
Concern over the susceptibility of local loon popu-
lations to anthropogenic pressures prompted the forma-
tion of a volunteer program, the Alaska Loon Watch,
in 1985. Under the direction of the Alaska Department
of Fish and Game (ADF&G), volunteers collected data
on loon and grebe presence and breeding activity on
lakes throughout the Mat-Su Valley (see Fair 1998*).
Using data collected through the Alaska Loon Watch
program and our own observations, we assessed changes
in lake occupancy, distribution, and productivity of loons
and grebes breeding in the Mat-Su Valley between
1987 and 1999. Based on the significant growth of the
human population in the region, we predicted that lake
occupancy and productivity by loons and grebes would
have decreased over time. Furthermore, we predicted
that the distribution of loons and grebes would shift
spatially from southeast to northwest in response to
corresponding changes in intensity of shoreline devel-
opment and lake recreation.
Study Area
The Mat-Su Valley of south-central Alaska lies be-
tween the Matanuska and Susitna rivers and borders
upper Cook Inlet. Over 1000 lakes, ponds, and wet-
lands of glacial origin occupy kettles in moraines and
ice-stagnation complexes in this 500 km? region
(Colazzi et al. 1986°). Lakes are classified as oligo-
trophic or mesotrophic with pH levels conducive to
support fish species preyed on by loons and grebes
(Ruggles 1991). The elevation of the valley floor ranges
from tide level to 400 m, but local relief of the area is
210
2004
Uplands are dominated by White Spruce (Picea glauca),
Paper Birch (Betula papyrifera), and Quaking Aspen
(Populus tremuloides), Black Cottonwood (Populus
trichocarpa) and willows (Salix spp.) are common
along waterways and on alluvial plains. Maritime in-
fluences moderate the climate in the Mat-Su Valley
with average mid-summer temperatures of 14°C, annu-
al snowfall of 150 cm, and annual precipitation of
about 48 cm. We concentrated our survey effort with-
in the lower Mat-Su Valley, an area bounded by the
MILLS AND ANDRES: CHANGES IN LOON AND GREBE POPULATIONS IN ALASKA
211
communities of Palmer to the southeast, Willow to
the northwest, Sutton to the east, and the Susitna
River to the west (Figure 1).
Methods
We surveyed lakes in late May and late August of
1999 to determine occupancy by loons and grebes
and productivity of loons. Because of their smaller size
and tendency to linger in aquatic vegetation, produc-
tivity of Red-necked Grebes was not recorded. Of
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FiGurE 1. Location of the lower Matanuska-Susitna Valley, Alaska, where lake occupancy and productivity of loons and
grebes were assessed, in the delineated area, in 1987 and 1999.
D2
219 lakes surveyed in 1987 by biologist Nancy
Tankersley (ADF&G) and volunteers of the Alaska
Loon Watch program, we determined that 139 lakes
had adequate coverage in both years to allow a mean-
ingful comparison. In 1999, observers scanned each
lake with binoculars from several vantage points along
the lakeshore to ensure complete lake coverage. Lakes
were scored for the presence or absence of single loons
or loon pairs during late May and for the presence or
absence of loon chicks during late August. Field meth-
ods were similar in 1987. A lake was considered oc-
cupied if a loon pair was found on a lake surveyed on
or before 5 July, or if chicks were discovered on the
lake. Only lakes surveyed after 25 June were used to
determine productivity.
To detect changes in the spatial distribution of loons
over the 12-year period. We divided the study area
was divided into two regions of differing human pop-
ulation densities. The Little Susitna River runs east to
west and divides the study area into southeastern (Was-
illa, high human population) and northwestern portions
(Willow, low human population). Lake physiographic
features are comparable between regions, and lakes
vary similarly in size, food availability, and shoreline
topography (Ruggles 1991).
We used McNemar’s symmetry test for matched
pairs to compare temporal and geographic differences
in lake occupancy and productivity (Agresti 1996 pages
226-229). Alternative hypotheses were constructed to
indicate a decline in parameter estimates between 1987
and 1999; no statistical analysis was conducted when
n <3 lakes. We used P-values to examine strength of
differences between years and regions. Standardized
normal standard errors of differences were also cal-
culated (Agresti 1996 page 228).
Results
The number of lakes occupied by any loon or grebe
species decreased significantly between 1987 and 1999
across the entire study area (Table 1). Decreases in
lake occupancy between years were consistent among
Common Loons, Pacific Loons, and Red-necked
Grebes (Table 1). Differences in occupancy of lakes by
loon or grebe pairs, however, were not uniform among
regions of the Mat-Su Valley. Decreases in the num-
ber of lakes occupied by any loon or grebe pair and
by Common Loons were less drastic in the northwest
region of the study area (Willow) than in the southeast
region (Wasilla; Table 1), where development is greater.
Decreases in lake occupancy by Pacific Loons tended
to be greater in the northwest section (P = 0.1094),
but conclusiveness of results was hampered by small
sample sizes (Table 1). Point estimates of decreases in
occupancy by Red-necked Grebe pairs were similar
between regions, but variability was much higher in
the northwest region (Table 1).
Contrary to lake occupancy, the percentage of lakes
that fledged Common Loon chicks remained stable
between 1987 and 1999. Information on productivity
THE CANADIAN FIELD-NATURALIST
Vol. 118
of Red-necked Grebes was not collected in 1987, and
sample sizes were too small to permit analysis of
changes in productivity for Pacific Loons. Productivity
of Common Loons was similar on lakes in both regions
of the study area.
Discussion
Temporal and spatial changes in the population dis-
tribution of loons and grebes in the Mat-Su Valley from
1987 to 1999 are likely attributable to the concurrent
rise and spatial settlement of the human population.
Significant declines in lake occupancy by Common
and Pacific loons and Red-necked Grebes indicated
that fewer birds are establishing breeding territories
at area lakes. Most of the lakes that are no longer used
by breeding loons and grebes (65%) were located in
the southeastern portion of the study area — an area that
has also experienced the greatest human population
growth. Common Loons have been extirpated from
lakes within the nearby Municipality of Anchorage,
and Pacific Loon populations are decreasing there
(Fair 1998*). Such changes in lake occupancy may
be indicative of declining loon and grebe populations
or may reflect large-scale emigration due to the loss
of suitable nesting habitat. Common Loons inhabiting
boreal regions of Alaska, however, appear to be stable
(Groves et al. 1996).
Population declines of Common Loons and Red-
necked Grebes throughout North America have oc-
curred most frequently at the southern boundaries of
their breeding ranges where habitat quality has become
marginal owing to development (De Smet 1987; Mc-
Intyre 1988). In the Mat-Su Valley, a spatial shift in
lake occupancy from southeast to northwest may be
linked to habitat quality decreases in the same spatial
direction. Habitat in the southeastern portion of the
study area is likely poorer in quality compared to the
northwest, where fewer people live and more lakes
remain undeveloped. The stability of lake occupancy to
the northwest implies that habitat quality is optimal,
a fact supported by the rapid reoccupation of vacant
territories (sensu Newton 1998).
The negative trends in lake occupancy may also
reflect changes in the demographics of the Mat-Su
Valley loon and grebe populations. Loons and grebes
are long-lived species known to return to breed on the
same lake territories year after year (McIntyre 1988;
Stout and Neuchterlein 1999). The combination of a
long lifespan and strong site-fidelity may have caused
individuals to occupy lakes that had deteriorated in
quality over several years. When existing occupants
died or left, the vacancies were not filled, and lake
occupancy declined over time. Thus, lakes may have
lost loons and grebes not suddenly through abandon-
ment by resident breeders, but by failure of new birds
to replace them after the death of residents.
Although habitat in the southeastern region may be
less suitable during selection of a territory, loons may
remain productive if they choose to nest there. Greater
2004 MILLS AND ANDRES: CHANGES IN LOON AND GREBE POPULATIONS IN ALASKA ZAS
TABLE |. Occupancy and productivity of breeding pairs of loons and grebes on lakes in high (Wasilla) and low (Willow)
human population regions of the lower Matanuska-Susitna Valley, Alaska, in 1987 and 1999.
Species — stage Percentages of lakes occupied Difference (SE)
area both years 1987 only 1999 only 1999 — 1987 P-value’
Any loon or grebe - occupancy
entire area (n = 86) 67 Di, 6 -21 (6) 0.0005
Wasilla (n = 52) 71 29 0 -29 (6) <0.0001
Willow (n = 34) 62 23 15 -8 (10) 0.2905
Common Loon - occupancy
entire area (n = 63) 59 33 8 =25) | + (7) 0.0012
Wasilla (n = 36) 58 42 0 -42 (8) <0.0001
Willow (n = 27) 59 22 19 -4 (12) 0.5000
Pacific Loon - occupancy
entire area (n = 17) 41 47 12 -35 (17) 0.0547
Wasilla (n = 10) 40 50 10 -40 (21) 0.1094
Willow (n = 7) 43 43 14 -29 (26) 0.3125
Red-necked Grebe - occupancy
entire area (n = 33) 76 24 0 -24 (7) 0.0039
Wasilla (n = 25) 76 24 0 -24 (9) 0.0156
Willow (n = 8) 75 25 0 -25. (15) 0.2500
Common Loon - productivity
entire area (n = 34) 24 38 38 OP Fas) 0.5775
Wasilla (n = 21) 29 33 38 5 (18) 0.5000
Willow (n = 13) 15 46 38 -8 (25) 0.5000
Pacific Loon - productivity
entire area (n = 10) 80 0 20 ~ -
Wasilla (n = 7) 86 0 14 - -
Willow (n = 3) 67 0 33 - -
' one-sided test, 1987 > 1999.
* small sample sizes precluded reasonable statistical testing.
breeding success for Common Loons in the south-
eastern region may reflect differences in the age struc-
ture of the population. Across numerous species, non-
breeders and non-territory holders consist mainly of
sub-adult birds (Smith 1976; Birkhead et al. 1986).
Because replacements for vacant territories in the north-
west are likely drawn from the non-territorial cohorts
(Ruggles 1991), these loons would be expected to have
lower productivity than experienced territorial loons
on southeast region lakes.
Tolerance of human activity by experienced territory
holders may also explain the differences in Common
Loon breeding success between the regions. Common
Loons are known to be relatively flexible in behavior
and may acclimate themselves to low-level human dis-
turbance (Titus and VanDruff 1981; Heimberger et al.
1983; McIntyre 1988). Years of breeding experience
and gradual habituation to the subtle progression of
human disturbance would likely result in higher breed-
ing success for loons that established territories years
ago.
Loons may also benefit by nesting in areas where
humans are moderately active. Recreational activities
and residents who watch over loons may deter preda-
tors from taking young or eggs. Reports from Alaska
Loon Watch volunteers often include stories of resi-
dents protecting adults and chicks by discouraging
Bald Eagles and other predators (Tankersley 1987*,
Mills, personal observation). This interference, com-
bined with the defensive behavior of an adult loon,
may be intense enough to dissuade additional preda-
tion attempts.
Changes in the distribution of loons and grebes
warrant concern about the future of these populations
within the region. The human population is expected
to continue to increase in the Mat-Su Valley (Alaska
Department of Natural Resources 1998), which could
result in further changes to the lake habitat used by
loons and grebes. Although degradation of lake habi-
tats are likely widespread across south-central Alaska,
only a small portion of North America’s populations of
Common Loon, Pacific Loons, or Red-necked Grebes
occur in south-central Alaska. People residing in south-
central Alaska, however, value living with wildlife and
believe it makes their community “interesting and
special” (Alaska Department of Fish and Game 2000).
Therefore, proactive management of lake use and lake-
shore development, coupled with continued monitoring
of loon and grebe populations, is needed to improve
the stability of the freshwater habitats and ensure the
continued persistence of loons and grebes in the Mat-
Su Valley of Alaska.
214
Acknowledgments
We sincerely thank Nancy Tankersley and all the
Alaska Loon Watch volunteers for their devoted inter-
est and effort. This project was funded by the U. S.
Fish and Wildlife Service, Region 7 Nongame Migra-
tory Bird Program, the North American Loon Fund,
and the Alaska State Parks. Special thanks to Rick
Mills for assisting in field work. Helpful manuscript
comments were provided by A. J. Erskine.
Documents Cited (marked * in text)
Colazzi, E. J.. M. A. Maurer, and S. J. Carrick. 1986.
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area, Alaska. Alaska Division of Geological and Geo-
physical Surveys, Public-Data File 86-62. 19 pages.
Evers, D. C. 2003. Status assessment and conservation plan
for the Common Loon (Gavia immer) in North America.
Unpublished report, U. S. Fish and Wildlife Service,
Hadley, Massachusetts. 80 pages.
Fair, J. 1998. The status of loons in Anchorage and the lower
Matanuska-Susitna Valley of Alaska: a summary report
of Alaska Loon Watch 1985-1997. Unpublished report,
Anchorage Audubon Society, Anchorage, Alaska. 36 pages.
McKibben, B., and R. Nelson. 1998. Matanuska-Susitna
Borough planning department — 1998 facts. Palmer, Alaska.
15 pages.
McKibben, B., and R. Nelson. 1999. Matanuska-Susitna
Borough planning department — 1999 facts. Palmer, Alaska.
35 pages.
Tankersley, N. 1987. Alaska Loon Watch 1987. Unpublished
report, Alaska Department of Fish and Game, Anchorage,
Alaska. 27 pages.
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Anchorage, Alaska. 138 pages.
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Birkhead, T. R., S. F. Eden, K. Clarkson, S. F. Goodburn,
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D. C. 26 pages.
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ductive success of the Red-necked Grebe in southern
Manitoba. Condor 89: 460-467.
Groves, D. J., B. Conant, R. J. King, J. I. Hodges, and J.
G. King. 1996. Status and trends of loon populations sum-
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grebes breeding in central Alberta. Ph. D. thesis, University
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Received 30 December 2002
Accepted 2 November 2004
The Barred Owl, Strix varia in Alberta: Distribution and Status
LISA TAKATS PRIESTLEY
Beaverhill Bird Observatory, Box 1418, Edmonton, Alberta T6B 2X3; e-mail: lisa@beaverhillbirds.com
Priestley, Lisa Takats. 2004 The Barred Owl, Strix varia, in Alberta: Distribution and Status. Canadian Field-Naturalist 118(2):
215-224.
Barred Owl distribution and status in Alberta were investigated using over 300 individual records (1912 through 1999) that
were collected from literature, museum/zoo specimens, nest cards, bird surveys, volunteer raptor banders, and naturalists. Barred
Owls were distributed throughout much of the boreal forest, aspen parkland, foothill, and mountain ecoregions of Alberta.
Fifty-four breeding records (46 nests) were found. Barred Owls were associated with older forests and had a clumped distri-
bution, predominantly along water where larger Balsam Poplar trees provide nesting sites. According to Alberta’s “Status of
Alberta Wildlife 2000” criteria, the Barred Owl should be assessed as Sensitive. There is no evidence that Barred Owls have
expanded their range in Alberta in the last 100 years; rather, they have maintained their distribution.
Key Words: Barred Owl, Strix varia, distribution, status, Alberta, volunteer surveys, nests.
The Barred Owl, Strix varia, is widely distributed
throughout North America, ranging from the east
coast to the western Canadian provinces (American
Ornithologists’ Union 1998; Johnsgard 1988; Mazur
and James 2000). It is found from the southern tip of
Florida to southeastern Alaska. In Canada, the Barred
Owl is a permanent resident in woodlands of British
Columbia, through central and western Alberta, central
Saskatchewan, south-central and southeastern Mani-
toba, central and southern Ontario, southern Quebec,
New Brunswick, Prince Edward Island, and the Mari-
time provinces (Godfrey 1986). There is little pub-
lished historical information available on the Barred
Owl in western Canada, except for British Columbia
(Boxall and Stepney 1982). However, recent studies
have found this owl to be more common in western
Canada than originally believed (Campbell et al. 1990;
Mazur and James 2000; Mazur et al. 1997; Takats
1998).
The Barred Owl is still considered rare in northern
regions of Alberta (McGillivray 1996). It was found
in the boreal forest region north of Edmonton, in the
foothills/montane forests of western Alberta, and in
Jasper National Park. The detailed status and distri-
bution of the Barred Owl, however, is poorly -docu-
mented in the province (Boxall and Stepney 1982;
Kirk and Hyslop 1998). There has been considerable
debate over the theory that the Barred Owl has only
recently extended its range into the western states,
Canada, and Alaska, although their relative rarity in
the west has been assumed from the paucity of histor-
ical records (Shea 1973; Taylor and Forsman 1976;
Leder and Walters 1980; Boxall and Stepney 1982;
Sharp 1989; Houston and McGowan 1999). It has also
been suggested that their numbers are increasing in the
boreal forest due to their increasing tolerance of pre-
dominantly coniferous forests (Boxall 1986).
In many parts of its range, the Barred Owl is depend-
ent on large areas of remote forest with mature and
old growth trees for nesting, roosting, and foraging
(Paris 1947; Elody 1983; Devereux and Mosher 1984;
McGarigal and Fraser 1984; Elody and Sloan 1985;
Allen 1987; Bosakowski et al. 1987; Johnson 1987;
Dunbar et al. 1991; James 1993; James et al. 1995;
Mazur et al. 1997; Mazur et al.1998). In the United
States it has been reported to nest in interior portions
of expansive, mature woodland (Allen 1987). The
typical Barred Owl nest is in a cavity in a large living
or dead tree or in the top of a broken snag. There are
records of Barred Owls using more conspicuous plat-
form nests (i.e., stick nests) built by squirrels or other
large birds (Mazur et al. 1997), as well as ground nests
(Robertson 1959; Postupalsky et al. 1997), but these
are potentially less productive than cavity nests (Pos-
tupalsky et al. 1997) and are generally quite rare.
Alberta Environmental Protection (1996) placed
the Barred Owl on the Yellow B list in the Status of
Alberta Wildlife report. The Yellow B list includes
species that are: (1) naturally rare but not in decline,
(2) naturally rare and have clumped breeding distribu-
tions, or (3) associated with habitats or habitat elements
that are, or may be, in decline. The status of Canada’s
remaining old growth forests is of growing concern
because of the high rate of harvest (Ellis 1993). In the
year 2000, the Barred Ow] was placed on the Sensitive
species list (Alberta Sustainable Resource Develop-
ment 2000).
The first step in managing wildlife populations is
having knowledge of distribution and abundance
(Mosher and Fuller 1996). The first objective of this
paper was to compile all historic Barred Owl records
(published and unpublished) for Alberta, in order to
determine the past and present distribution in the prov-
ince. The second, based on recent studies, was to evalu-
ate this species’ status and general habitat use (as it
relates to status) in Alberta. The third was to establish
whether evidence exists to support the suggestion of
range expansion into the west.
Pas)
216
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 1: Barred Owls banded in Alberta: date, location, age, sex, and name of bander (1966-1999).
Date Location Age-Sex*
May 1966 Edmonton L-U
April 1987 Water Valley SY-U
November 1988 SSA Ste U-U
April 1988 Deerland AHY-F
June 1989 Deerland L-U
May 1990 Deerland L-U
May 1991 Niton L-U
May 1991 Deerland L-U
May 1992 Deerland L-U
May 1994 Millarville AHY-F
June 1994 Tawatina L-U
June 1994 Uncas L-U
June 1994 Calling Lake AHY-F
June 1995 Solomon Creek AHY-F
August 1996 Gregg Lake AHY-U
May 1995 Water Valley AHY-F
May 1995 Water Valley AHY-M
May 1995 Uncas AHY-F
May 1995 Uncas L-U
May 1995 Tawatina L-U
November 1995 Redwater AHY-M
November 1995 Se lae2° U-U
April 1995 Calling Lake AHY-M
June 1995 Calling Lake AHY-F
June 1996 Tawatina AHY-F
June 1996 Tawatina L-U
May 1996 Calling Lake AHY-M
May 1996 Calling Lake AHY-M
May 1996 Calling Lake AHY-F
June 1996 Calling Lake AHY-M
July 1996 Calling Lake AHY-M
August 1996 Calling Lake AHY-M
May 1997 Tawatina L-U
May 1998 Calling River L-U
May 1998 Calling Lake L-U
June 1998 Uncas L-U
June 1999 Uncas L-U
June 1999 Vinca L-U
* Age — L=nestling/fledgling, AH Y=after hatch year, SY=second year, Sex — U=unknown, M=male,
Methods
Information on Barred Owls in Alberta was col-
lected from a variety of sources, which included: pub-
lished literature, museum collections (National Museum
of Canada, National Museum of Natural Sciences (now
Canadian Museum of Nature), American Museum of
Natural History, Cornell University Museum of Verte-
brates, Royal Ontario Museum, University of Calgary
Museum of Zoology, University of Alberta Museum
of Zoology, Provincial Museum of Alberta, Alberta
Breeding Bird Atlas (Federation of Alberta Natural-
ists), Avian Raptor Nest Cards (Alberta Sustainable
Resource Development/Beaverhill Bird Observatory
1999*), banding records (Canadian Wildlife Service
Bird Banding Office), and personal communications
with Provincial and National Parks personnel. Records
Number Bander
3 E. Jones
D. Collister
Pletz/B. Gehlert
Cromie
Cromie
Collister
Cromie
Cromie
Stepnisky/G. Court
Takats
Takats
Collister
Collister
Cromie
Cromie
Cromie
Roper
Halmazna
Court
Sissons/G. Court
Cromie
Cromie
Olsen/R. Sissons
Olsen/R. Sissons
Olsen/R. Sissons
Olsen/R. Sissons
Olsen/R. Sissons
Olsen/R. Sissons
Cromie
Cromie
Cromie
Cromie
Cromie
Pletz
BWW PD FB DR OD EOD DBD i OD OD OD OD i i
Fae Ragen re Ce ee ee eG eee OSs GS eee ee eae
F=female
from the following volunteer programs were also col-
lected: Alberta Bird Records 1983-1988 (Alberta Or-
nithological Records Committee), Breeding Bird Sur-
veys, Christmas Bird Counts and May Species Counts,
volunteer owl survey programs (Edmonton Ow! Prowl,
Alberta Owl Prowl, Alberta Nocturnal Owl Survey),
dead raptors turned in to Alberta Sustainable Resource
Development, and unpublished data including field
notes.
All georeferenced Barred Owl sightings and nest
locations were entered into the Biodiversity Species
Observation Database (BSOD) (Alberta Sustainable
Resource Development/Alberta Conservation Associ-
ation 1998*). Maps comparing distributions from 1912
to 1975 and 1976 to 1999 were created in ArcView
(ESRI GIS Mapping and Software).
2004
PRIESTLEY: BARRED OWL IN ALBERTA
Ficure 1. Photo of a Barred Owl pausing before entering a typical nesting cavity (photo by Gordon Court).
Results
Of 320 reports of Barred Owls, 297 of these were
entered into the BSOD database (23 records lacked
information on date, location, and/or observer). The
first record of a Barred Owl in Alberta was from a
specimen collected in 1912, from the Calgary area,
though this has been considered a mislabeled speci-
men (Houston and McGowan 1999). The first live
Barred Owl recorded in Alberta was one heard calling
along the Athabasca River near Fort McMurray in
1934 (Preble 1941).
Dead Owls
Museum specimens, private collections, and dead
owls turned in to Fish and Wildlife constituted 53
Barred Owl locations distributed throughout the prov-
ince. The most southeasterly report was a dead owl
turned in to Fish and Wildlife in February 1984 from
Coronation (Boxall 1986). Morphological information
collected on 26 owls shows that the majority were
adults (24 of 26), 12 females, 10 males, 4 unknown
sex. Boxall and Stepney (1982) reported an unusually
high number of dead Barred Owls turned in to Fish
and Wildlife during a short period of time (15 indi-
viduals from 1982 to 1985).
Banding, Literature and Personal Communications
Barred Owls have been banded on 38 occasions in
Alberta from 1966 to 1999 (CWS Banding Office) by
thirteen banders (Table 1). There were 15 clutches of
owls banded at nest sites, as well as nine adult females,
eight adult males, and three adults of unknown sex.
Only one Barred Owl was banded before 1987 (2.6
percent). :
There were 42 reports of Barred Owls collected from
publications (Preble 1941; Jones 1956; Jones 1966;
Salt and Wilk 1958; Salt and Salt 1976; Francis and
Lumbis 1959; Jones 1987; Sadler and Myers 1976;
Boxall and Stepney 1982; Rintout and Myers 1983;
Pintel et al. 1991; Takats 1995) and 63 records collect-
ed from personal communications. Only 35 of these
records were pre-1975 (33 percent). Jones (1987) sum-
marized observations of Barred Owls as being “fairly
evenly distributed in Alberta, particularly in Alberta’s
northern forests and heavily forested foothill regions
of Alberta”.
Holroyd and VanTighem (1983) report the Barred
Owl as a rare, year-round resident in Banff and Jasper
National Parks. They state:
“Tt occurs regularly near Jasper townsite especially along
the lower Miette River, where it has nested, and near Cot-
tonwood Slough (Roy Richards, pers. comm.) and Pyramid
Lake (R. Salt, pers. comm.). It has been recorded twice
near North Saskatchewan River Crossing (M. Dyer, pers.
comm.), twice near Vermilion Lakes Banff, once at Lake
Annette (K. VanTighem, pers. comm.) and once near Ma-
ligne Canyon (J. Salt, pers. comm.).”
Volunteer Surveys
Breeding Bird Atlas volunteers reported 65 Barred
Owl locations during a five-year survey from 1987
through 1991 (data were collected between February
and July of each year). Atlas data showed that Barred
Owls were concentrated in the Boreal Forest region,
218
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 2. Barred Owl locations recorded on volunteer owl survey programs (EOP — Edmonton Owl Prowl, AOP — Alberta
Owl Prowl, ANOS — Alberta Nocturnal Owl Survey).
Date Location Observation Observer
24 February 1988 Big Lake 1 individual EOP-—_ Beck and Beck (1988)
5 March 1988 Cooking Lake 1 individual EOP— _ Beck and Beck (1988)
6 March 1988 Wabamun Creek 1 individual EOP— _ Beck and Beck (1988)
24 February 1989 Big Lake 1 individual AOP-—_ E. Bamford
05 March 1989 Cooking Lake 1 individual AOP—_ R. and M. Berg
06 March 1989 Wabamun Lake 1 individual AOP -—_ S. Jungkind, Belmonte, Gomez, Diener
21 May 1989 Water Valley 1 individual AOP— _ D. Hutchinson, D. Collister
10 April 1998 Lac La Biche pair duetting © ANOS — J. Gammon and P. Okrainec
15 May 1998 Shaw Lake 1 individual ANOS — J. Gammon
18 April 1998 Hillcrest Road 2 individuals ANOS — M. Heckbert and J. Doll
26 April 1998 Sibbald 1 individual ANOS — D. Woodsworth, Kanagawa, Mitchell
27 March 1999 Nojack South 1 individual ANOS — R. Gutsell, R. Wiacek, B. McCulloch
and primarily coniferous foothills and montane forests
west of Calgary and in Jasper National Park (Semen-
chuk 1992). Few records indicated breeding evidence
and only one possible breeding record was discovered,
north of Lesser Slave Lake at La Crete along the Peace
River. During Alberta Christmas Bird Counts from
1965 to 1998, volunteers in 44 count circles recorded
53 Barred Owls. Only 17 (32 percent) of these owls
were recorded before 1990. Only four and two owls
were recorded during Breeding Bird Surveys and May
Species Counts, respectively.
There have been three volunteer surveys conducted
specifically for owls (Table 2): Edmonton Owl Prowl
(1988), Alberta Owl Prowl (1989), and the volunteer
Alberta Nocturnal Owl Survey (1998 and ongoing).
Seven Barred Owls were found during the first two
owl surveys (Beck and Beck 1988, personal commu-
nication). Volunteer Alberta Nocturnal Owl surveyors
found 13 individual Barred Owls (11 records) on elev-
en 10 km transects along roads (16 routes were sur-
veyed throughout the province). The Alberta Bird
Record contributed 35 more locations of Barred Owls
in 1988 (Alberta Ornithological Records Committee).
Two intensive studies have been conducted on the
Barred Owl in Alberta (Takats 1998; Olsen 1999).
Takats (1998) conducted a study on distribution and
abundance of the Barred Owl in the Foothills Model
Forest (located in the foothills and mountains around
Hinton and Jasper). Forty-two different territorial
Barred Owls (10 females, 17 males, and 15 unknown
sex) were recorded in 1995 and 1996. Of these, seven
were paired and the other 28 were single but may have
had mates that did not respond to broadcasts (Takats
1998). Surveys were continued in 1997 and 1998 and
four additional Barred Owls were located. The density
of Barred Owls was determined to be 0.05 and 0.04
owls/km?, in 1995 and 1996, respectively.
The habitat used by Barred Owls at 45 calling loca-
tions in the Foothills Model Forest was predominant-
ly older mixedwood forest containing Trembling Aspen
(Populus temuloides), White Spruce (Picea glauca)
and Balsam Poplar (Populus balsamifera). Roosting
and foraging occurred in a variety of stand types, but
were also predominantly older mixedwood Populus
sp. and spruce (Takats 1998).
A study to evaluate the effects of forest fragmenta-
tion on bird communities was initiated in north-central
Alberta (Schmiegelow and Hannon 1993). Preliminary
work located six Barred Owl territories, and evidence
of three breeding pairs was discovered in the Calling
Lake area (G. Court, personal communication). Two
additional territories and four additional breeding
sites were found in a study from 1996 through 1998
(Olsen 1999). During the breeding season, the density
of Barred Owls was 0.04 pairs/km?. Owls were found
to use old growth mixed forest stands (Olsen 1996).
Breeding Records
There were 54 breeding records (only three found
before 1975). The first evidence of breeding was re-
corded in 1949 (Grant 1966), but the first nest was
not discovered until 1966, in Edmonton (Jones 1966)
(Table 3). Boxall and Stepney (1982) reported eight
breeding records, and Semenchuk (1992) reported six
confirmed breeding records during the Provincial
Breeding Bird Atlas Project (1987-1991). The north-
ern-most breeding record was a nest found at 58° 19'
latitude and 116° 17' longitude near La Crete (Takats
1995). Some local residents have reported Barred Owls
to be present for over 20 years.
Breeding records for Barred Owls were not com-
mon (n = 54) and only 46 nests have been found (1966
through 1999): 38 (82.6 percent) were in natural cavi-
ties (or bowls on top of dead trees that had broken off),
two (4.3 percent) were in stick nests, one (2.2 percent)
was in a man-made stick nest, and five (10.9 percent)
were in nest boxes. In most cases owls nested in older
mixedwood stands and used large diameter Populus
sp. trees (> 40 cm) (primarily Balsam Poplar) for
2004
TABLE 3: Confirmed breeding records of Barred Owls for Alberta.
Man-Made Platform
Date Location Nest Type
1949 Lesser Slave Lake Unknown
1966 Edmonton Cavity Nest
1968* Edmonton Cavity Nest
1976* Blue Lake Cavity Nest
LOTA* Jasper Cavity Nest
1977* Blue Lake Cavity Nest
1978 Chilver Lake Unknown
IO Miette River Cavity Nest
1980* Miette River Cavity Nest
1984** Spruce Grove Cavity Nest
1988 Deerland Cavity Nest
1989 Deerland Cavity Nest
1990 Deerland Cavity Nest
199] Deerland Cavity Nest
199] Niton Cavity Nest
1992 Deerland Cavity Nest
1993 La Crete Cavity Nest
1994 La Crete Cavity Nest
1994 Millarville Unknown
1994 Uncas
1994 Tawatinaw Cavity Nest
1994 Elk Island Stick Nest
1994 Calling Lake Unknown
1994 Miette River Cavity Nest
1995 Lynx Creek Cavity Nest
1995 Miette River Cavity Nest
1995 La Crete Cavity Nest
1995 Tawatinaw Cavity Nest
1995 Cross Lake Cavity Nest
1995 Uncas Nest Box
1995 Calling Lake Cavity Nest
1995 Calling Lake 2 Cavity Nest
1996 Bragg Creek Cavity Nest
1996 Solomon Creek Cavity Nest
1996 Blackcat Ranch Cavity Nest
1996 Miette River Cavity Nest
1996 Tawatinaw Nest Box
1996 Calling Lake Unknown
1997 Cross Lake Cavity Nest
1997 Miette River Cavity Nest
1997 Tawatinaw Cavity Nest
1997 Lac La Biche Stick Nest
1997 Calling Lake Cavity Nest
1998 Uncas Cavity Nest
1998 Solomon Creek Cavity Nest
1998 Calling River Cavity Nest
1998 Calling Lake Cavity Nest
1999 Uncas Nest Box
1999 Tawatinaw Nest Box
999 Fe Vinca Cavity Nest
1999 Cross Lake Nest Box
PRIESTLEY: BARRED OWL IN ALBERTA 219
Observer/Reference
Grant (1966)
Jones (1966)
E. Jones (personal communication)
Boxall and Stepney (1982)
Boxall and Stepney (1982)
Boxall and Stepney (1982)
Wiseley (personal communication)
Richards (personal communication)
Richards (personal communication)
R. Copeland (personal communication)
R. Cromie (Nest Card)
R. Cromie (Nest Card)
R. Cromie (Nest Card)
R. Cromie (personal communication)
H. Pletz/B. Gehlert
R. Cromie (Nest Card)
Takats (1995)
Takats (1995)
D. Collister (personal communication)
R. Cromie (Nest Card)
R. Cromie (Nest Card)
H. Pletz (personal communication)
G. Court (personal communication)
Takats (1998)
Takats (1998)
Takats (1998)
A. Miller (personal communication)
R. Cromie (Nest Card)
R. Cromie (Nest Card)
R. Cromie (Nest Card)
G. Court (personal communication)
G. Court (personal communication)
H. Pletz (personal communication)
Takats (1998)
Takats (1998)
Takats (1998)
R. Cromie (Nest Card)
Olsen (1999)
A. Karvonen (personal communication)
L. Takats (personal communication)
R. Cromie (Nest Card)
Olsen (1999)
Olsen (1999)
R. Cromie (personal communication)
L. Takats (personal communication)
T. Roper (Nest Card)
Olsen/Cromie (Nest Card)
R. Cromie (Nest Card)
R. Cromie (Nest Card)
H. Pletz (Nest Card)
R. Cromie (Nest Card)
* Boxall and Stepney (1982) ** Nest cut down, two eggs cracked, one survived, owl held at Valley Zoo, Edmonton
*** One young Barred Owl was fostered in to this nest.
nesting (Takats 1998; Avian Raptor Nest Cards; Olsen
1999). Nest boxes built specifically for Barred Owls
were readily taken over in areas where natural cavities
were not abundant (G. Court, personal communica-
tion; R. Cromie, personal communication).
Distribution
Most occurrences of Barred Owls were in the boreal
forest, foothill, and mountain ecoregions from 1912
through 1974 (Figure 2) and from 1975 to the present
(Figure 3). Few owls were recorded in the parkland,
220 THE CANADIAN FIELD-NATURALIST Vol. 118
Barred Owl Occurrences
1912-1974
Medicine Hat
FIGURE 2. Barred Owl distribution from 1912 through 1974 (map courtesy of Alberta Conservation Association/Alberta Sus-
tainable Resource Development).
NR
i)
2004. PRIESTLEY: BARRED OWL IN ALBERTA
Barred Owl Occurrences
1975-1999
FiGuRE 3. Barred Owl distribution from 1975 through 1999 (map courtesy of Alberta Conservation Association/ Alberta
Sustainable Resource Development).
222
and only one individual was recorded in the northern
limit of the grassland ecoregion. Detection of Barred
Owls appears to have increased after 1975, but there
have been only two records outside the range of the
early distribution map.
Discussion
The Barred Owl is distributed over much of Alberta’s
forested area. Evidence suggests that Barred Owl dis-
tribution in the province has changed little over the
last 100 years. As more detailed studies are conducted,
as there is an increase in the number of interested
naturalists exploring isolated woodlands, and as there
is increased access to remote areas, more reports of
Barred Owls will accumulate, Oeming (1957) and
Jones (1966) concur. Mazur et al. (2000) suggested that
Barred Owls are shy of humans, which may account
for their secretive nature.
In British Columbia the first records of Barred Owls
were from Liard Crossing in 1943 and Nechako Low-
lands in 1946 (Campbell et al. 1990). Scotter et al.
(1985) reported a Barred Owl record from 1977 in
the South Nahanni River, Northwest Territories, which
shows that Barred Owls have existed northwest of
Alberta for over 20 years. As well, the idea that the
Barred Owl is adapting to the coniferous boreal forest
does not hold true. Barred Owls have shown a clumped
distribution in areas that contain large deciduous trees
(predominantly riparian areas). They use Balsam Pop-
lars for nesting and rely on a more open subcanopy
for flight, although the roost cover provided by White
Spruce trees is important, particularly in the winter
(Takats 1998). Some of the first records of Barred
Owls occurred along riparian areas.
The Sensitive designation assigned by Alberta Sus-
tainable Resource Development (2000) is well founded.
Based on recent studies and personal communications
with raptor banders and naturalists, the Barred Owl
should not be considered rare in Alberta; however,
this species does have a clumped breeding distribu-
tion. As well, these owls rely on cavities in old, large
diameter Populus sp. trees for nesting, and select old
and/or mature mixedwood forests (a habitat that is in
decline) to fulfill their life requisites (Takats 1998;
Olsen et al. 1996*; Olsen 1999; Mazur and James 2000).
As older forests are usually targeted first for har-
vest, the amount of old growth forest remaining de-
creases and stands become increasingly fragmented.
Loss of nesting, roosting, and foraging habitat occurs
when a forest is clearcut; moreover, Great Horned
Owls, Bubo virginianus, are known to favour frag-
mented landscapes. There is direct conflict between
these two owl species, with the Barred Owl losing out
to the larger Great Horned Owl (Bent 1961; Bosa-
kowski 1994; Laidig and Dobkin 1995; Takats 1998
and field notes; Olsen 1999; G. Court, personal com-
munication). Barred Owl numbers and range are lim-
ited by the amount of adequate nesting habitat avail-
able where they can reproduce successfully and fledge
THE CANADIAN FIELD-NATURALIST
Vol. 118
their young without interference from competitors
and predators.
Acknowledgments
Funding for parts of this work was provided by
Foothills Model Forest, Alberta Sport, Recreation,
Parks and Wildlife Foundation, Alberta Sustainable
Resource Development (Fish and Wildlife), Environ-
ment Canada (Canadian Wildlife Service), Beaverhill
Bird Observatory, and Weldwood of Canada, Hinton.
The Bird Banding Office (Canadian Wildlife Service)
provided Barred Owl banding information for Alberta.
The Federation of Alberta Naturalists provided loca-
tions from the Breeding Bird Atlas. The Alberta Con-
servation Association/Alberta Sustainable Resource
Development provided use of the Biodiversity Species
Observation Database (BSOD) to create maps of the
distributions.
I thank Tony Erskine, Jim Duncan, and Bob Nero
for reviewing the submitted manuscript. Gordon Court,
Jim Beck, and Geoff Holroyd initially reviewed the
manuscript, provided owl location information, and
continue to encourage me with my work in raptor
ecology. Lance Engley (Alberta Conservation Asso-
ciation) provided the maps. Chuck Priestley, Dawn
Birn, Kris Kendell, and Jeff Adamyk also provided
some editorial comments. Jim Duncan and Kurt Mazur
provided the idea to write the paper in the first place.
I acknowledge Jim and Barb Beck (the ‘Owl Nuts’)
for providing the Edmonton and Alberta Owl Prowl
data as well as many other locations. Edgar Jones,
Doug Collister, Ray Cromie, Wayne Smith, Hardy
Pletz, Bob Gehlert, Ben Olsen, Trevor Roper, and
Rick Lauzon (AXYS) provided many owl locations.
Thanks also to Wayne Roberts (University of Alberta
Museum of Zoology), Michel Gosselin (National
Museum of Canada [now Canadian Museum of Na-
ture), Mark Steinhilber (Provincial Museum of Alber-
ta), and Rusty Copeland (Valley Zoo, Edmonton) for
providing information on museum and zoo specimens.
Thanks to Howard Troughton for providing the Christ-
mas Bird Count information in a ready-to-use file.
Special thanks to Stephen Glendinning and Jeff
Adamyk, who spent many hours conducting broad-
cast surveys for owls in the foothills. Finally, thank you
to all the volunteer raptor banders, owl surveyors, and
raptor enthusiasts who have contributed most of the
information we know about Barred Owls in Alberta.
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Received 30 July 2002
Accepted 22 June 2004
Use of Eelgrass, Zostera marina, Wrack by Three Species of Ladybird
Beetles (Coleoptera: Coccinellidae) in Prince Edward Island
DaviD J. GARBARY, SARAH FRASER, CARRIE FERGUSON, and RANDOLPH F. LAUFF
Department of Biology, St. Francis Xavier University, Antigonish, Nova Scotia B2G 2WS5 Canada
Garbary, David J., Sarah Fraser, Carrie Ferguson, Randolph F. Lauff. 2004. Use of Eelgrass, Zostera marina, wrack by three
species of ladybird beetles (Coleoptera: Coccinellidae) in Prince Edward Island. Canadian Field-Naturalist 118(2):
225-228.
Large numbers of the introduced ladybird beetle, Coccinella septempunctata L., were present at Wood Islands and Green
Point, Prince Edward Island, in wrack consisting primarily of Zostera marina L. (Eelgrass). The wrack occurred in a 0.5 to
1.0 m band parallel to the shore, and was from five to 25 cm thick. The other ladybirds, Propylea quatuordecimpunctata
(L.), an introduced coccinellid also found in high numbers, and an individual of the native Hippodamia tredecimpunctata
(Say) were found only at Wood Islands. At both sites the ladybird beetles occurred in the mid-intertidal zone along at least
100 m of shoreline, and were absent to rare on the terrestrial vegetation above the high tide mark. At four of the other eight
sites surveyed, occasional individuals were present in the wrack, but they were no more abundant than could be observed on
landward vegetation. Mean densities of C. septempunctata at the two primary sites were 52 m? (Green Point) and 410 m7?
(Wood Islands).
Key Words: Coccinella septempunctata, Propylea quatuordecimpunctata, Hippodamia tredecimpunctata, ladybird beetles,
Coccinellidae, Zostera marina, Eelgrass, intertidal zone, Prince Edward Island.
With over 150 species and subspecies, the Coc-
cinellidae of Canada and Alaska are a conspicuous
and ecologically important element of the terrestrial
biota (McNamara 1991). In addition to the native
fauna, there is great interest in the distribution of
invasive ladybirds and the subsequent loss of native
biodiversity (Gordon and Vandenberg 1991). This is
also true in eastern Canada where Hoebeke and Wheel-
er (1996) and McCorquodale (1998) and Majka and
McCorquodale (in press) reported the spread of intro-
duced species in the Maritimes.
Despite being a terrestrial family, there are several
reports of Coccinellidae from beaches and salt marshes
in both freshwater and marine environments (Davis
and Gray 1966; Schaefer et al. 1987; Turnock 1996;
Pupedis 1997; review by Nalepa et al. 1998). Here we
report on the mass occurrence of living ladybird beetles
in the marine intertidal of Prince Edward Island and
their association with Eelgrass (Zostera marina) wrack.
Materials and Methods
Ten intertidal locations on Prince Edward Island
(Table 1) were visited on 30-31 August 2002 for the
examination of Eelgrass wrack as part of a study on
Eelgrass decline. An abundant population of ladybird
beetles was at site one (Wood Islands), and several hours
were spent photographing and quantifying the assem-
blage. At subsequent sites three individuals inspected
the wrack for a minimum of 15 min along at least 100 m
of shoreline. If only a few beetles were observed, their
presence was noted. If many were present, densities
were calculated using a 20 x 20 cm quadrat. The quad-
rat was placed haphazardly on the eelgrass wrack (n =
25) at irregular intervals on the shore.
Characteristics of the primary study sites were: The
Wood Islands site was a sandy beach with sandstone
outcrops. The primary species of seaweeds associated
with the wrack were recorded. Green Point was a salt
marsh adjacent to an abandoned wharf, and common
plants in the marsh were recorded. At Green Point the
wrack was almost exclusively Eelgrass. Characteris-
tics of other sites are mentioned, where necessary, in
the body of the text. The weather on both days was
mostly bright and sunny; however, a mild rain fell at
Marchwater (1800 h, 30 August) and Belmont Prov-
incial Park was extremely windy (0800 h, 31 August).
Coordinates of primary sites were determined using a
global positioning system (Garmin GPS 12, Olanthe,
Kansas; Table 1).
Beetles were identified using the keys in Gordon
(1985) and by comparison with specimens in the in-
sect collection at St. Francis Xavier University. Voucher
specimens have been deposited in the Herbarium of
St. Francis Xavier University (STFX) and in the insect
collection.
Results
Three species of ladybird beetles, Coccinella sep-
tempunctata, Hippodamia tredecimpunctata, and Prop-
ylea quatuordecimpunctata, were present in intertidal
Eelgrass wrack (Zostera marina) in Prince Edward
Island during late August. All species were present at
Wood Island; however, only C. septempunctata was
collected from the other sites.
PIT)
226
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 1. Relative abundance of P. quatuordecimpunctata, H. tredecimpunctata and C. septempunctata in sites across Prince
Edward Island, and their corresponding GPS coordinates. “Low” corresponds with an observation of < 5 individuals.
Site Coordinates
Wood Islands 45°56'N
62°45'W
St. Peters Bay 46°26'N
62°28'W
March Water 46°29'N
63°44'W
Belmont Provincial Park 46°31'N
63°49'W
Green Point 46°35'N
63°52'W
Cascumpec Bay 46°45'N
64°04'W
Linkletter Provincial Park 46°24'N
63°51'W
Victoria Provincial Park 46°12'N
63°30'W
West River Bridge 46°11'N
63°14'W
Pinnette Provincial Park 46°04'N
62°54'W
At Wood Islands, C. septempunctata occurred pri-
marily in a loose to dense band of Eelgrass wrack,
0.2-1.0 m wide, that formed in the mid-intertidal zone
on a sandy beach (Figure 1). No coccinellid beetles
were found in the dry wrack in the splash zone nor
in the mixed herbaceous vegetation above the high
tide mark. A few beetles were also found in small
clumps of wrack lower in the intertidal zone that had
recently been inundated by the incoming tide and
very gentle wave action. The wrack consisted mostly
of leaves of Eelgrass and was mixed with several com-
mon seaweeds including the brown algae, Fucus ser-
ratus, Chorda filum, Chordaria flagelliformis, and the
red algae, Chondrus crispus (Irish moss), Palmaria
palmata (Dulse) and Furcellaria lumbricalis. The
Eelgrass was relatively fresh and had numerous green
leaves.
The beetles were present on the exposed wrack to
about two cm into the wrack mass in loosely packed
leaves (Figure 2). Beetle density was 410 + 340 m?
(mean + SD). Beetles were absent deep within the
20-30 cm thick wrack bundles. The beetles walked
along the surface of the leaves and were single or in
clumps of two-five individuals. Occasional beetles
were present on the bare sand adjacent to the wrack
or on clumps of seaweed (mostly Chorda filum and
Fucus serratus) that separated from the main body of
wrack. No flying beetles were observed; however,
walking beetles occasionally spread their elytra.
At Green Point, the Eelgrass wrack accumulated
in a 0.5 —2 m band in the mid-intertidal zone of a salt
marsh. This was a typical marsh dominated by Spar-
tina alterniflora in the lower marsh and a mixture of
Abundance
Very high
Absent
Absent
Absent
High
Absent
Low
Low
Low
Low
S. patens, Scirpus americanus, S. maritimus, Glaux
maritimus, Triglochin maritima and Limonium nashii
in the mid-intertidal zone. At various sites along the
shore there was extensive accumulation of old Eelgrass
in the upper intertidal zone. The Eelgrass wrack tend-
ed to form a blanket that matted down the surround-
ing vegetation or occasionally was suspended up to
30 cm above the ground.
The beetles (all C. septempunctata) were found on
the Eelgrass in the mid-intertidal zone, with rare indi-
viduals on the surrounding grasses and sedges. The
insects were common (52 + 8.5 m7) over more than
100 m of shoreline, and were typically single. Beetles
were absent on the upper intertidal wrack, and none
were observed in the lower intertidal zone. The insects
walked on the Eelgrass and did not fly. In addition to
the ladybird beetles, one Leptinotarsa decemlineata
(Colorado Potato Beetle) was observed on the wrack.
At Linkletter and Pinnette Provincial Parks and West
River Bridge, 3-5 beetles (all C. septempunctata)
were found on Eelgrass in the upper intertidal zone.
These sites were primarily sand beaches with either
scattered clumps or continuous carpets of Eelgrass up
to 2 m wide in the high intertidal zone. At St. Peters
Bay, Belmont and Victoria Provincial Parks and Cas-
umpec Bay, beetles were absent, despite the presence
of extensive Eelgrass wrack.
Upon our return to Wood Islands, 28 h after the
initial observations, we found that the previous day’s
wrack had largely disappeared. A few hundred dead
ladybird beetles were present in the remaining wrack
and on sandstone outcrops along with a few live
individuals.
2004
GARBARY, FRASER, FERGUSON, and LAUFF: USE OF EELGRASS BY LADYBIRD BEETLES
Ficure |. Ladybird beetle site at Wood Islands, Prince Edward Island, showing band of intertidal wrack on beach with investi-
gator (C.F.) examining Eelgrass.
Discussion
Although the records for both introduced species
(C. septempunctata, P. quatuordecimpunctata) do not
represent range extensions, it is disturbing that they
did make up essentially all of the coccinellid fauna at
the sampled sites. P. quatuordecimpunctata has been
recorded in PEI since at least 1994 (Hoebeke and
Wheeler 1996). The first records for C. septempunc-
tata on PEI (Charlottetown) are from 1982; it is now
abundant in the province (Majka and McCorquodale;
in press). The two sites where C. septempunctata was
abundant shared the feature of having abundant Eel-
grass wrack in the mid-intertidal zone. The beetles
were generally not found in the older, dry wrack at the
upper part of the shore nor in the vegetation above
the high tide mark (Wood Islands and Green Point),
and the surrounding salt marsh vegetation (Green
Point). Examination of the Eelgrass substratum showed
no conspicuous populations of invertebrates that might
be a suitable food source. In addition, the beetles were
sluggish, suggesting exhaustion due to struggling or
partial suffocation. The location of the beetles and their
behaviour suggest that the they were only recently
washed up to the eelgrass wrack, a substrate which
allowed them firm footing. Sites with few or no beetles
had less fresh Eelgrass wrack. The intertidal substra-
tum at these sites tended to be rockier, with better
developed populations of seaweed.
Although terrestrial, both C. septempunctata and
Propylea quatuordecimpunctata have previously been
found in coastal habitats including salt marshes in
Connecticut, North Carolina and Delaware (Schaefer
et al. 1987; Pupedis 1997; Nalepa et al. 1998). Davis
and Gray (1966) also reported another ladybird beetle,
Naemia serriata, from a salt marsh in North Caro-
lina. The mass occurrences of C. septempunctata that
we found are different from that in Delaware in which
numerous dead and some living individuals were
washed ashore following deposition in the ocean and
association with seaweed wrack (Schaefer et al.
a
2.
Coccinella septempunctata on mid-intertidal
Eelgrass wrack. Note: The white spots on the leaves are a
calcified red alga.
FIGURE
228
1987). The North Carolina mass occurrence is similar
to that reported by Schaefer et al., and involved mass
mortality and shore deposition (Nalepa et al. 1998).
Turnock (1996) suggested that accumulations of lady
beetles on the shores of Lake Manitoba resulted from
wave deposition and subsequent migration up the
shore to structures protruding from the sand. Given
the localization of C. septempunctata in this study,
particularly at Green Point, the Eelgrass seems to have
been a fortunate substratum on which the beetles could
take hold, and rest prior to dispersal.
Although there were conspicuous corpses of lady-
bugs in the wrack at Wood Islands on the day after the
survey, the vast majority of the population had dis-
appeared from the shore. There was no evidence that
the beetles had moved onto the grassy field adjacent
to the beach. Invasions of Coccinellidae into North
America show that these species can cover a large dis-
tance (Schaefer et al. 1987). McCorquodale (1998)
gives range expansion rates of 31-440 km y"! across
North America for four introduced coccinellids in
Nova Scotia, although he concedes that not all of this
is likely to be long distance flights. Schaefer et al.
(1987) comment on the occurrence of C. septempunc-
tata on Sable Island, 300 km from mainland Nova
Scotia. Thus the 20 km flight across the Northumber-
land Strait to or from Nova Scotia is reasonable, espe-
cially if a suitable wind is available.
Our records of C. septempunctata on the north and
south shores of PEI are consistent with eelgrass pro-
viding a staging substratum during migration. Migra-
tions of Hippodamia convergens cover hundreds of
kilometres in single flights in California from San
Francisco and the Imperial Valley to the Sierra Nevadas
(Hodek 1973). However, the aggregations we observed
in Prince Edward Island are more likely reflective of
accidental downing of migrating populations as a result
of weather conditions, followed by subsequent wash-
up. The Eelgrass provided a better refugium than other
substrata in the mid-intertidal zone. We suggest that
the beetles are only saved by the Eelgrass wrack, and
that there is no particular attraction to it as previously
described for similar vegetation with C. septempunc-
tata (Schaller and Nentwig 2000; Frantsevich and
Zolotov 2001).
Acknowledgments
We thank Christine Nalepa and Chris Majka who
provided helpful discussion and literature; the com-
ments of two anonymous reviewers were also an asset
to this paper. Barry Taylor kindly assisted with plant
identification and David McCorquodale verified iden-
tifications of beetles in our insect collection. This
THE CANADIAN FIELD-NATURALIST
Vol. 118
work was supported by a grant from the Natural Sci-
ences and Engineering Research Council (NSERC)
to D. J. G., funding from the Nova Scotia Museum to
R. FE. L., and by NSERC undergraduate awards to S.
F and C. F.
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Williams. 1998. Mass appearance of lady beetles (Coleop-
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salt marshes of Connecticut. Bulletin Series, Yale School
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Schaefer, P. W., R. J. Dysart, and H. B. Specht. 1987. North
American distribution of Coccinella septempunctata
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Received 17 September 2002
Accepted 15 November 2004
Predicting the Effects of Cerulean Warbler, Dendroica cerulea
Management on Eastern Ontario Bird Species
JASON JoNES!, WILLIAM J. MCLEISH, and RALEIGH J. ROBERTSON
Department of Biology, Queen’s University, Kingston, Ontario K7L 3N6 Canada
| Present address, Department of Biology, Vassar College, Poughkeepsie, New York 12604 USA; e-mail: jajones @
vassar.edu
Jones, Jason, William J. McLeish, and Raleigh J. Robertson. 2004. Predicting the effects of Cerulean Warbler,
Dendroica cerulea, management on eastern Ontario bird species. Canadian Field-Naturalist 1 18(2): 229-234.
Single-species habitat management strategies are often undertaken without explicit consideration of their effects
on the larger community. Here we explore the potential effects of managing eastern Ontario deciduous forests
for the Cerulean Warbler (Dendroica cerulea) by examining its potential as a biodiversity indicator species and
as an umbrella species. Our results indicate that the Cerulean Warbler would not be an effective biodiversity
indicator, as its distribution across the studied landscape did not coincide with areas of high avian species rich-
ness. However, the Cerulean Warbler may be effective as an umbrella species for the maintenance of populations
of other canopy-nesting species that require mature deciduous forest habitats. It is hoped that the conclusions
reached in Ontario, while perhaps not directly transferable to all parts of the breeding range, encourage other
Cerulean Warbler researchers to ask similar questions in their study areas.
Key Words: Cerulean Warbler, Dendroica cerulea, conservation utility, biodiversity indicator species, umbrella
species, eastern Ontario.
Few North American songbirds are receiving the
scientific and conservation attention that is currently
focused on the Cerulean Warbler (Dendroica cerulea;
Robbins et al. 1992; Rosenberg et al. 2002*; Hamel et
al. 2004). The Cerulean Warbler has suffered signifi-
cant long-term breeding population declines (annual
declines of 3.04% over 1966-2000; Link and Sauer
2002) which are largely attributed to habitat destruction
on both the breeding and wintering grounds (Robbins
et al. 1992). Concern over the long-term health of this
species has led to its designation as threatened, rare, or
of special concern in the United States and as a Species
of Special Concern in Canada (Robbins et al. 1992;
Hamel 2000; COSEWIC 2003*).
In two separate meeting in 2001 and 2002, a group
of academic and governmental scientists, land mana-
gers, industry biologists and non-governmental organi-
zations formed the Cerulean Warbler Technical Group
(CWTG): an effort to develop a proactive, broad-based,
multiple stakeholder approach to Cerulean Warbler
conservation in both North and Latin America (Hamel
et al. 2004). One of the outcomes of these meetings
was a breeding grounds research plan that is designed
to identify key population limitation factors and ex-
plore forest management options for the maintenance
and creation of Cerulean Warbler habitat on a range-
wide basis.
Ironically, the very thing that limits our ability to
currently diagnose specific reasons for breeding ground
population declines — a general lack of natural and life-
history information — may also limit the efficacy of
the CWTG research plan. Here, we take advantage of
data collected during one of the longest running Ceru-
lean Warbler research programs in North America
(dating to 1994; Oliarnyk and Robertson 1996; Jones
et al. 2000, 2001, 2004; Jones and Robertson 2001:
Barg et al. 2005) to make predictions regarding the
potential effects of managing deciduous forests for
Cerulean Warblers on sympatric bird species in eastern
Ontario. Specifically, we ask two questions. One, will
the promotion of Cerulean Warblers and Cerulean
Warbler habitat promote the preservation of avian
diversity? In other words, is the Cerulean Warbler a
biodiversity indicator (sensu Landres et al. 1988)?
Two, can the Cerulean Warbler act as an umbrella
species for other bird species with similar life — and
natural histories? The protection of the habitat of the
umbrella species ideally results in the protection of
the habitat of those species whose requirements are
subsumed by those of the umbrella (Launer and Mur-
phy 1994; Berger 1997; Simberloff 1998).
Study Area and Methods
This investigation was conducted at the Queen’s
University Biological Station (QUBS), Ontario
(44°34'N, 76°20'W), within the Great Lakes-St. Law-
rence mixed forest region. Our study area was restricted
to approximately 2 600 ha of research tracts managed
by QUBS. The landscape in the area is dominated by
mature, secondary-growth, lowland mixed deciduous
forest, interspersed with rocky outcrops, marshes, lakes
and abandoned agricultural fields.
229
230
Bird surveys. In 1997 and 1998, we surveyed birds
on QUBS property using variable-circular-plot point
counts (Reynolds et al. 1980; Jones et al. 2000). We
surveyed 80 stations in 1997 (17 May — 20 June) and
67 stations in 1998 (21 May — 21 June); the 1998 sta-
tions were a subset of those sampled in 1997. The
point-count stations were located to maximize spatial
coverage of the study area. Each point count was
10 min long. Each station was separated by at least
200 m to minimize the potential for double-counting
individuals. Point counts were conducted between
0.5 hr before sunrise and 3 hr after sunrise EST in
order to sample during peak song activity, and were
only conducted under calm weather conditions. For our
analyses we included birds detected within 100 m of
the plot center. Probability of detection was similar for
all species analysed, as the detection thresholds for all
but one species (Black-and-white Warbler, Mniotilta
varia, 92 m) were beyond 100 m (Jones unpublished
data). Data from the first two visits per station each
year were used in the analyses to facilitate comparison
between years and because two visits are sufficient to
confirm the presence or absence of Cerulean Warblers
(Jones et al. 2000).
Vegetation Surveys. We collected vegetation data
at 59 point-count stations in 1997 at five circular sub-
plots, each with a radius of 5 m. The first subplot was
centered on the point count station center and the other
four were located 50 m away in each of the cardinal
directions. Within each of the subplots we counted the
number of saplings [stems < 3.0 cm diameter at breast
height (dbh)], measured the dbh of all stems 2 3.0 cm
and grouped them into two size classes (3.0 — 15.0 cm
dbh, 15.0 — 30.0 cm dbh). Using an imaginary | m radius
cylinder projected upward from the forest floor, we
estimated cover within 3 m height intervals from the
ground to the top of the canopy. Total cover and per-
cent cover of each woody plant species was estimated
by eye in each height interval on a scale of 0 to 10
(0 = 0% cover, 10 = 100% cover). Two observers made
all cover estimates; the two observers spent several
days prior to data collection assuring that their cover
estimates were within 10% of one another. For analysis
we reduced these cover estimates to two variables:
maximum cover below 6 m (understory cover) and
maximum cover above 12 m (canopy cover). Each
vegetation variable was averaged across subplots to
describe the habitat of the point-count station. We
measured only those vegetation variables thought to
be important to Cerulean Warblers; the importance of
these variables has been supported by subsequent re-
search (Jones and Robertson 2001; Jones et al. 2001).
We also restricted the number of vegetation variables
for analytical reasons (see below).
Data Analysis. In our analyses, we included only
those species known to breed in our study area. We also
excluded species that are not adequately sampled by
diurnal point counts, such as colonial nesters (e.g.,
THE CANADIAN FIELD-NATURALIST
Vol. 118
Barn Swallow, Hirundo rustica), nocturnal species (e.g.,
Whip-poor-will, Caprimulgus vociferus), waterfowl
(e.g., Wood Duck, Aix sponsa), and waders (e.g., Great
Blue Heron, Ardea herodias).
(1) Biodiversity indicator evaluation
We tested whether the presence of Cerulean War-
blers was a predictor of overall bird species richness.
For the purposes of these analyses, we defined spe-
cies richness as the number of species detected in the
first two visits to a point-count station, excluding the
Cerulean Warbler if present. We used randomization
tests to compare the mean species richness at stations
where Cerulean Warblers were present to the expect-
ed species richness at a randomly generated sample
of points (Chase et al. 2000). In these tests, the mean
species richness was calculated for a random sample
of point-count stations, with the number of random
stations equaling the number of stations where Ceru-
lean Warblers were detected in a given year. We iter-
ated this procedure 1000 times to generate an expected
distribution of mean species-richness values. We then
compared the observed species richness associated
with Cerulean Warblers and determined its statistical
significance. These randomization tests were performed
using S-PLUS 4.0 (Mathsoft 1997*). Values reported
in the results are means + SE.
(2) Umbrella species evaluation
The initial step in evaluating the potential of the
Cerulean Warbler as an umbrella species was to estab-
lish an ecological context. We categorized the bird
species detected during our surveys into species groups
based on habitat preferences, diet and foraging sub-
strate, and nesting substrate. These classifications were
based on observations reported in the literature (Ehr-
lich et al. 1988; Robbins et al. 1989a; Freemark and
Collins 1992; Canterbury et al. 2000); we did not in-
clude our survey data in these classifications. In addi-
tion, we created a conservation concern grouping that
included species which were experiencing statistically
significant population declines as indexed by North
American Breeding Bird Survey data for 1966-2000
(Sauer et al. 2001*). For the purposes of these analyses
we focused on the groups to which Cerulean Warblers
belonged: mature forest habitat (n = 13 species), insect-
foliage foragers (n = 15), canopy_nesters (n = 12),
and species of concern (n = 14).
We used two methods to test if the distribution of
Cerulean Warblers was representative of the distribu-
tions of other species in the same functional group.
First, we used the checkerboard score (C-score) devel-
oped by Stone and Roberts (1990) to test for non-
randomness in presence-absence matrices. One of the
reasons we selected this metric of co-occurrence is that
is not particularly prone to Type 1 error (Gotelli and
Entsminger 2000*) and, unlike other co-occurrence
metrics, it allows for overlap in species distributions
(Gotelli and McCabe 2002; Feeley 2003). We calcu-
lated C-scores (hereafter, observed C-score) for each
2004
JONES, MCLEISH, and ROBERTSON: CERULEAN WARBLER MANAGEMENT
TABLE |. Interpretation of the principal components axes from analysis of 5 vegetation variables for 59 point-count stations.
Bold-face eigenvalues significant following bootstrap analyses.
Axis cvi Ce Wes SPD‘ SSD* LSD! Interpretation of positive axis values
PCl 29.2 0.6249 -(.6281 -0.2509 0.0187 0.3195 mature forest with dense canopy
REZ 54.1 0.2676 0.2143 0.7024 0.5205 0.3438 mid-succession forest
PC3 74.2 0.0036 0.3208 0.1185 -0.7046 0.6218 mid- to late-succession forest
PC4 88.5 -0.4737 0.0870 -0.4715 0.4648 0.5742 mature forest with patchy canopy
PES 100.0 0.5599 0.6702 -0.4553 0.1280 = -0.1171 early succession forest
‘Cumulative variance explained; "Canopy cover (% cover > 12.0 m); ‘Understory cover (% cover < 6.0 m); ‘Sapling density
(stems/m7); ‘Stem density (stems/m7) 3.0-15.0 cm dbh; ‘Stem density 15.0-30.0 cm dbh.
functional group to examine if species within each
functional group were distributed randomly across the
landscape with respect to one another. For each survey
year, we used re-sampling techniques to calculate
10 000 C-scores based on the original presence-absence
matrix. The observed C-score was then compared with
the generated distribution of expected C-scores. A C-
score significantly greater than expected indicates that
the assemblage is competitively structured; that is,
individual species have distinct, and often exclusive,
distributions (Stone and Roberts 1990). Conversely, a
C-score significantly smaller that expected indicates
that there is a degree of cohesion in the distribution
patterns of the species included in the matrix. All C-
score calculations were carried out using EcoSim 5.0
(Gotelli and Entsminger 2000). For all iterations, the
number of species detected at each point-count station
was kept consistent with the original matrix and each
station was equally likely to be inhabited by a given
species. Survey results from 1997 and 1998 were ana-
lyzed separately.
In our second test, we used logistic regression ana-
lyses to predict the probability of occurrence along a
habitat gradient for all species within each species
group to which Cerulean Warblers belonged. The
Red-eyed Vireo (Vireo olivaceus) was not included in
these analyses due to its near-ubiquitous distribution.
For these analyses we included only the 1997 surveys
of the 59 point-count stations for which we collected
vegetation data. We generated the habitat gradient by
entering all five vegetation variables into a principal
components analysis, giving us an approximate 10:1
ratio of sites to variables. We tested the significance
of the eigenvalues for each variable within each com-
ponent using a bootstrap approach, following the
recommendations of Peres-Neto et al. (2003). We
drew 1000 bootstrap samples by resampling entire rows
with replacement, thereby ensuring that the bootstrap
matrices had the same dimensions as the original veg-
etation matrix; we conducted a PCA on each of these
1000 matrices. P-values were estimated by the number
of bootstrap loadings equal to or less than zero for
original loadings that were positive (greater than or
equal to zero for negative loadings), divided by 1000.
For the purposes of this paper, we considered P = 0.10
as our significance cut-off. The first PC axis (PC1)
explained 29% of the variance of the vegetation data
(Table 1); positive values along PC1 represented sites
of mature deciduous forest and negative values repre-
sented early successional forest. We included PC1 as
the independent variable in our logistic regression ana-
lyses. All these analyses were performed with JMP
IN 4.0.2 (SAS Institute Inc. 2000*) and MS-EXCEL
using the PopTools add-in module (Hood 2002). We
calculated 95% confidence intervals around the logis-
tic regression coefficient to facilitate comparison of
occurrence probabilities across species.
Results
(1) Biodiversity indicator — The presence of Ceru-
lean Warblers was not a significant predictor of avian
species richness in either 1997 or 1998. In other words,
observed species richness at Cerulean Warbler point-
count stations was not significantly different from spe-
cies richness expected by chance, based on bootstrap
analyses (1997, observed richness 12.69 + 0.75 spe-
cies, expected 13.95 + 0.03, P = 0.12; 1998, observed
9.75 + 0.63, expected 9.82 + 0.03, P = 0.83).
(2) Umbrella species — All three of the species
groups to which Cerulean Warblers belong exhibited
cohesive distributions in both 1997 and 1998, as in-
dexed by their C-scores (Table 2). C-scores that are
significantly lower then expected are indicative of co-
occurrence in the distribution patterns of the species in-
cluded in the analyses. Species of conservation concern
also exhibited cohesive distributions in both 1997 and
1998 (Table 2).
The results of the logistic regression analyses using
PC1 indicate that species within each of the species
groups to which Cerulean Warblers belonged were
distributed differentially along the generated habitat
gradient, some more so than others (Table 3). Within
the mature forest group, only one of the 12 group spe-
cies (Black-and-white Warbler) did not overlap with
the Cerulean Warbler confidence intervals. Similarly,
only one of the 12 canopy nesting species (Blue Jay,
Cyanocitta cristata) did not overlap with the Cerulean
Warbler confidence intervals. Conversely, the insect-
232
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 2. Tests for cohesive distributions of functional groups, as indexed by the C-score of Stone and Roberts (1990). Esti-
mated values are mean + SE for a generated random distribution based on the actual presence-absence matrix for each group
for each year. C-scores that are significantly lower then expected are indicative of co-occurrence in the distribution patterns
of the species included in the analyses.
1997
Functional Group Observed Expected
Mature forest 80.76 91.94 + 0.03
Insect-foliage 86.02 92.29 + 0.02
Canopy nesters 67.03 71.92 + 0.02
Species of concern 136.11 147.68 + 0.12
1998
P Observed Expected ie
0.0003 41.42 48.13 + 0.02 0.0017
0.0050 52.96 65.15 + 0.02 <0.0001
0.0078 36.63 40.90 + 0.02 0.0068
0.0049 73.32 85.04 + 0.03 0.0001
TABLE 3. Logistic regression coefficients and upper and lower 95 % confidence intervals (C. I.) predicting occurrence across
a habitat gradient for members of the mature forest (MF), insect-foliage (IF), canopy nesting (CN) and conservation
concern (CC) species groups detected in 1997. The confidence intervals of the species in bold face do not overlap with the
confidence interval of the Cerulean Warbler.
Species Functional Regression Lower Upper
group coefficient Spy Vo Osill, 951701 11:
Cerulean Warbler (Dendroica cerulea) all 0.519 0.121 0.917
American Redstart (Setophaga ruticilla) all 0.144 -0.299 0.587
Ovenbird (Seiurus aurocapilla) MF, CC 0.475 0.024 0.926
Black-and-white Warbler (Mniotilta varia) MEF -0.290 -0.645 0.065
Scarlet Tanager (Piranga olivacea) all 0.106 -0.239 0.451
Least Flycatcher (Empidonax minimus) MF, CN, CC 0.116 -0.290 0.522
Yellow-throated Vireo (Vireo flavifrons) MF, IF, CN 0.066 -0.381 0.513
Wood Thrush (Hylocichla mustelina) MF, CC -0.287 -0.791 0.217
Black-throated Green Warbler (Dendroica virens) MF, CN, CC 0.134 -0.272 0.540
Northern Waterthrush (Seiurus noveboracensis) MF -0.195 -0.777 0.387
Warbling Vireo (Vireo gilvus) IF -0.995 -1.936 -0.054
Ruffed Grouse (Bonasa umbellus) MF -0.140 -0.620 0.340
Veery (Catharus fuscescens) MF, CC -0.622 -1.786 0.542
Yellow-rumped Warbler (Dendroica coronata) MF, IF, CN 0.009 -0.483 0.501
Common Yellowthroat (Geothlypis trichas) IEXEE -0.192 -0.555 0.171
Golden-winged Warbler (Vermivora chrysoptera) IEVEGE -0.534 -0.955 -0.113
Indigo Bunting (Passerina cyanea) TENCE -0.535 -0.974 -0.096
Chestnut-sided Warbler (Dendroica pensylvanica) IEF; Ee -0.705 -1.438 0.028
Yellow Warbler (Dendroica petechia) IF -0.232 -0.585 0.121
Black-capped Chickadee (Poecile atricapillus) IF 0.058 -0.279 0.395
Rose-breasted Grosbeak (Pheucticus ludovicianus) Wee -0.725 -1.270 -0.180
Baltimore Oriole (Icterus galbula) LE ENEC 0.281 -0.217 0.779
Blue-grey Gnatcatcher (Polioptila caerulea) IF, CN -0.279 -0.781 0.223
Cedar Waxwing (Bombycilla cedrorum) CN -0.066 -0.440 0.308
Blue Jay (Cyanocitta cristata) CN -0.873 -1.528 -0.218
Eastern Wood-Pewee (Contopus virens) CN, CC -0.202 -0.670 0.266
American Crow (Corvus brachyrhynchos) CN -0.304 -0.835 0.227
foliage and conservation concern groups exhibited less
concordance with the Cerulean Warbler distribution
relative to the habitat gradient — 43% (6 of 14) and
29% (4 of 14), respectively.
Discussion
Effective biodiversity indicators tend to be habitat
specialists with wide geographic ranges; they also tend
to have well-known natural histories (Caro and O’ Do-
herty 1999). Despite fitting this profile (Hamel 2000;
Oliarnyk 1996; Jones 2000; Barg 2002), our results
indicate that the Cerulean Warbler would not be par-
ticularly effective as an avian biodiversity indicator in
eastern Ontario, as its distribution across the studied
landscape did not coincide with areas of high avian
species richness.
Our co-occurrence and logistic regression results do
suggest that the Cerulean Warbler is suited to a role as
an umbrella species. Perhaps not surprisingly, the dis-
tribution of the Cerulean Warbler was well matched
to the distributions of other canopy nesters in mature
deciduous forest (e.g., Scarlet Tanager, Piranga oli-
vacea). Given the hierarchical nature of habitat selec-
tion, broad habitat requirements are likely more impor-
2004
tant in determining species distributions than are spe-
cies’ food and nesting requirements (Hutto 1985; Block
and Brennan 1993); indeed, we found that the species
grouped by diet were more variable in their distri-
butions along our succession gradient than were the
species grouped by habitat type or nest location. Small
body size — and, as a consequence, small home range
size (Barg et al. in press) — could limit the Cerulean
Warbler’s umbrella suitability, as effective umbrella
species tend to have large home ranges (Caro and
O’Doherty 1999); however, the Cerulean Warbler’s
apparent tendency to live in conspecific aggregations
(Hamel 2000) potentially offsets any limitation im-
posed by small body size and individual home range
size. We do not mean to suggest that the Cerulean
Warbler would be a better umbrella than other, more
widespread, species such as the Scarlet Tanager. Rath-
er, our conclusions suggest that, if habitat manage-
ment is directed at Cerulean Warblers, other species
will likely benefit.
Our co-occurrence and logistic regression results
highlight a potential management conflict between
mature forest and shrubland species. Although our C-
scores indicate significant patterns of co-occurrence
within the conservation concern group, there was no
overlap between the logistic regression confidence in-
tervals of the Cerulean Warbler and shrubland species
that are considered to be at risk, such as the Golden-
winged Warbler (Vermivora chrysoptera). Given their
disparate habitat requirements (i.e., forest edge vs.
forest interior), management for Golden-winged War-
blers will necessarily conflict with management aimed
at maximizing Cerulean Warbler population health.
One additional conservation role the Cerulean War-
bler may fill, and may be already filling, is that of a
flagship species: a species that attracts attention sup-
port by virtue of its ‘charismatic’ nature (Simberloff
1998). The Cerulean Warbler is a Neotropical migrant
songbird, a group of birds that has been in the conser-
vation spotlight over the last 30 years (e.g., Robbins
et al. 1989b). The Cerulean Warbler is a beautiful
bird with an elusive nature that has a high profile due
to extensive public education and activism (Rosenberg
et al. 2002) and is highly valued by birders and orni-
thologists alike. More recently, the Cerulean Warbler
has achieved notoriety as the focus of a legal battle
surrounding its candidacy for listing on the U.S. En-
dangered Species Act (Ruley 2000). This attention
has led to the development of the CWTG and has
spurred a great deal of basic research and forest man-
agement interest (Hamel et al. 2004). The apparent
dependence of this species on large tracts of forest
creates a possibility for the Cerulean Warbler to serve
as a valuable symbol of the overall health of deciduous
forests in eastern North America.
Acknowledgments
We thank J. Pither and R. Montgomerie for sta-
tistical advice. J. Barg, A. Erskine and an anonymous
JONES, MCLEISH, and ROBERTSON: CERULEAN WARBLER MANAGEMENT
reviewer provided helpful comments on earlier drafts.
F. Phelan, M. Phelan, F. Connor and the staff at the
Queen’s University Biological Station provided logis-
tical support. Funding was provided by B. and K.
Jones, Wildlife Habitat Canada, the Eastern Ontario
Model Forest Program and an NSERC operating
grant to RJR. We also had the support of the World
Wildlife Fund of Canada in the form of a MacNaughton
Conservation Scholarship to JJ and grants from the
Endangered Species Recovery Fund to RJR. This
project is part of Natural Legacy 2000, a nationwide
initiative in Canada to conserve wildlife and habitats
in private and public. We gratefully acknowledge the
support of the Government of Canada’s Millennium
Partnership Fund. JJ was also supported by an NSERC
scholarship, Queen’s Graduate Awards and the Queen’s
Bracken Fellowship.
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Received 22 October 2002
Accepted 21 July 2004
Parasite Prevalence in Dark-eyed Juncos, Junco hyemalis, Breeding at
Different Elevations
HEATHER BEARS
Department of Zoology, University of British Columbia, 6270 University Boulevard, Vancouver, British Columbia V6T 174
Canada; e-mail: bears @zoology.ubc.ca
Present address: Centre for Applied Conservation Research, 2424 Main Mall, Forest Sciences Building, University of
British Columbia, Vancouver, British Columbia V6T 1Z4 Canada
Bears, Heather. 2004. Parasite prevalence in Dark-eyed Juncos, Junco hyemalis, breeding at different elevations. Canadian
Field-Naturalist 118(2): 235-238.
During the summer of 2001, Dark-eyed Juncos (Junco hyemalis) were captured within the lowest (1000 m above sea level)
and highest (2000 m asl) elevation extremes of their breeding range in Jasper National Park, Alberta. Blood samples were
taken to identify parasite genera, and to test for differences in parasite prevalence among elevations. The most common
parasites at either elevation were Haemoproteus spp., Leucocytozoon spp., and Trypanosoma spp. A significantly higher
proportion of low- compared to high-elevation birds was infected by at least one of these, supporting the prediction that
high-elevation habitats may be refuges from parasites.
Key Words: Dark-eyed Juncos, Junco hyemalis, blood parasites, mountains, elevation, Alberta.
Birds breeding at high elevations often experience
a delayed date of reproductive onset, exposure to ex-
treme weather, and scarce or sparsely distributed re-
sources (Hamman et al. 1989; Landmann and Winding
1993; Kollinsky and Landmann 1996; Widmer 1999;
Bears et al. 2003). Dark-eyed Juncos (Junco hyemalis)
show a significant reduction in seasonal reproductive
output with increasing breeding elevation from the
montane valley (1000 m asl) to the subalpine-alpine
treeline (2000 m asl) in Jasper National Park, Alberta
(Bears 2002, Bears et al. 2003). Yet, high elevation
habitats are not occupied by less competitive age or
size classes of juncos, or by later arriving individuals
(Bears 2002), all of which are traits that render juncos
less successful competitors for territory (Cristol et al.
1990; Grasso et al. 1996). Further, inter-annual return
of birds to their site of capture is high, and roughly
equivalent among elevations (Bears 2002). Hence, it
does not appear that juncos are “forced” to breed at
high elevations due to intraspecific competitive exclu-
sion from lower-elevation habitat. This led me to ex-
plore the idea that high-elevation juncos are compen-
sated for decreased seasonal reproductive output over
their lifetimes by some unrecognized benefits of breed-
ing at high elevations. In other mountain ranges,
studies have shown that the blood parasites of birds,
and the insect vectors that carry them, tend to be low
at upper breeding elevations (Stabler et al. 1974; Braun
et al. 1993). Thus, as part of a series of investigations
into the benefits of high-elevation breeding, I tested
whether the juncos have fewer parasites within higher-
versus lower-elevation segments of their breeding
range in Jasper.
Methods
Juncos were captured and monitored at eight 50 —
70 ha study sites in Jasper National Park (52°53'N,
118°3'W), Alberta, from 1 May to 20 August in 2000,
and from 15 April to 20 August in 2001. Four sites
were located near the lowest elevation within the Park
(1000 — 1020 m asl), separated by 5-10 km. Four sites
were at the highest elevation at which juncos breed
within the park (1950-2100 m asl), and were separat-
ed by > 18 km. All high-elevation sites had south or
southest aspects. Morphological measurements taken
from juncos in these sites (H. Bears, unpublished data)
most closely match the Oregon subspecies, Junco
hyemalis oregonus (Miller 1941), but some appear to
be intergrades between Junco hyemalis oregonus and
Junco hyemalis hyemalis, which produces Junco hye-
malis cismontanus (Miller 1941). Subspecies desig-
nations of Dark-eyed Juncos are a capricious topic
based on phenetic rather than genetic data, and they
are a taxonomic nightmare in the Canadian Rockies
where multiple subspecies meet and hybridize. There-
fore, we refer to the birds analyzed here simply as
Junco hyemalis.
Birds were captured using Japanese mist nets with
painted model male juncos as decoys. Juncos were
lured towards the net by playing the taped song of a
conspecific. Birds were given a numbered Canadian
Wildlife Service leg band and colour bands that
conveyed sex, age, and site information when caught.
Blood samples were taken from each bird caught
between | May and 20 August in 2001 only by punc-
turing the alar vein with a needle and collecting ca.
40 ul of blood in a heparinized microhematocrit tube.
235
Blood was blown out of microhematocrit tubes into
centrifuge tubes and kept on wet ice. Because blood
parasites may follow a diurnal periodicity (Gore et
al. 1982), the birds selected for parasite identification
were caught at approximately the same time each day
(7:00-12:00 hrs). Within 10 hours of collection, 5 ul
of blood were used to produce three microscope slides
per bird, using the methods of Harrison and Harrison
(1986) and Bennett (1970). The slides were fixed in
100% methanol immediately. In the laboratory, blood
smears were stained with Geimsa stain for 30 min-
utes, and rinsed with distilled water followed by acetone
under a fumehood (Deviche et al. 2001). Smears were
examined under 400 x 10 magnification, and 50 fields
of view per slide were classified as negative or posi-
tive for various parasites. Parasites were identified to
the genus level by examination under high power
(1000 x magnification) with oil immersion, using
various keys (Pierce 1981; Bennett and Pierce 1988;
Burrey-Caines and Bennett 1992; Bennett et al. 1994),
~and by comparing with photos of blood parasites taken
from juncos captured in Alaska (supplied by Pierre
Deviche, Arizona State University, personal commu-
nication). Parasite species were difficult to ascertain
with absolute certainty, but the genus level could be
resolved without ambiguity. Therefore, we used the
genus level when comparing parasite prevalence among
elevations.
At each site, one bird was caught between the 1* and
5" of each month (May-August), and another between
the 11 and 15" of each month, in order to represent
sites and time periods within the breeding season equiv-
alently. No females were captured using playback
and mist-netting methods, and so analyses here deal
solely with males. The statistical significance level
for all tests conducted was set at a = 0.05. All tests
were performed using SPSS 10. All techniques used
were approved by the animal care committee of the
University of British Columbia (A0-0046), Parks Can-
ada (2000-008), and Environment Canada (Banding:
10429 AJ; Collection: BC SCI 2000/067).
THE CANADIAN FIELD-NATURALIST
Vol. 118
Results
Thirty-two high- and 32 low-elevation adult male
birds caught across all eight sites were used in these
analyses. In addition, 12 fledglings were caught at high
elevations (in August) and 12 were caught at low ele-
vations (in August). Three parasite genera were found
in the blood of juncos: Haemoproteus (Family Plas-
modiidae), Leucocytozoon (Family Plasmodiidae) and-
Trypanosoma (Family Trypanosomatidae). All data are
summarized in Table 1. The most prevalent blood para-
site at both elevations was Haemoproteus, followed
by Leucocytozoon, and Trypanosoma. A significantly
higher proportion of low-elevation birds (66%, 21/32)
compared to high-elevation birds (28%, 9/32) were
infected by at least one of these parasites (P = 0.002,
Fisher’s Exact Test). A higher percentage of low-ele-
vation birds (34%, 11/32) compared to high-elevation
birds (19%, 6/32) were infected with Haemoproteus
spp., but the difference was not significant (P = 0.08,
Fisher’s Exact Test). Similarly, more low-elevation
birds (25%, 8/32) versus high-elevation birds (9%,
3/32) were infected with Leucocytozoon spp., with a
near significant difference (P = 0.07, Fisher’s Exact
Test). Of these individuals, 42% (8/19) of low-eleva-
tion and 44% (4/9) of high-elevation birds had both
Haemoproteus spp. and Leucocytozoon spp. present
in their blood. Two cases of infection with Trypano-
soma spp. were found in low-elevation birds, and none
at high elevations. Thirty-four percent (11/32) of low-
elevation and 72% (23/32) of high-elevation birds
were not infected with any parasites. There was no
relationship between date of capture and infection at
low elevations (P = 0.23, r = 0.33; Pearson’s r). How-
ever, at high elevations, a low proportion of individ-
uals (12.5%, 2/16) caught between 1 May and 15 June
were infected with Leucocytozoon spp. and Haemo-
proteus spp., but between 15 June and 30 August, a
significantly higher proportion were infected (7/16,
44%; P = 0.05, Fisher’s Exact Test). In samples from
low elevations not used in this analysis (taken from
birds nearby, but not within our study areas) two cases
TABLE |. Summary of data on presence and absence of blood parasites in Dark-eyed Juncos from low (~1000 m asl) and
high (~2000 m asl) elevations.
Adults (ASY) Infection/Parasite
Infected
Trypanosoma present
Leucocytozoon present
Haemoproteus present
Both Haemoproteus and
Leucocytozoon present
no parasites
Fledglings Parasite
Leucocytozoon present
Low (N = 32) High (N = 32)
21 9
2 0
8 3
11 6
8 of 19 individuals 4 of 9 individuals
11 23
Low (N = 12) High (N = 12)
2 1
2004
of Plasmodium spp. (family Plasmodiae) were noted.
More fledglings were infected with Leucocytozoon spp.
at low elevations as compared to at high elevations
(17%, 2/12, vs 8.3%, 1/12), but the difference was not
significant (P = 0.39, Fisher’s Exact Test). No other
blood parasites were observed in fledglings.
Discussion
High-elevation adult males and fledglings had lower
incidences of blood parasites as compared to low-ele-
vation adult males and fledglings. If relief from para-
sites enables adults to survive longer and breed for
more years, then this could aid in equalizing the life-
time reproductive success of high- and low-elevation
birds. Blood parasites can decrease survivorship by
directly increasing susceptibility to predation (Vaughn
and Coble 1975). In addition, there may be a trade-
off between reproductive effort and the efficiency of
the immune response. For instance, parasite loads may
increase during the reproductive period, as they did
here at high elevations, when breeding adults spend
considerable time provisioning their young and in
nest and territorial defence, or when breeding effort
is increased experimentally (Ots and Horak 1996;
Norris et al. 1994; Weatherhead and Bennett 1991,
1992; Rintmaki et al. 1999). A simpler reason for the
differential susceptibility observed here might also be
due to a difference in the timing of emergence of the
insect vectors carrying the parasites.
The two most common parasite genera in this study,
Haemoproteus and Leucocytozoon, are protozoon para-
sites of birds. Haemoproteus spp. are primarily trans-
mitted by insects in the dipteran family Ceratopogoni-
dae (no-see-ums, sandflies) or Hippoboscidae (louse
flies), whereas Leucocytozoon spp. are primarily trans-
mitted by simuliids (e.g., black flies) (Greiner and
Ritchie et al. 1994; Rosskopf and Woerpel 1996; Rint-
maki et al. 1999). Trypanosoma (likely avium), which
was rare in our study, is also transmitted by members
of the family Simuliidae. The principal effects of
Leucocytozoon infections are intravascular haemolytic
anemia, weight loss, and sometimes death, whereas
Haemoproteus and Trypanosoma in birds are generally
less pathogenic (Greiner and Ritchie 1994). Finally,
two low-elevation samples (not analyzed as part of the
sub-samples selected) contained Plasmodium spp.,
which is transmitted by mosquitos (family Culicidae).
Almost all of these insect vectors were noted to have
emerged later at high elevations, perhaps preventing
exposure of birds to the parasites for much of the sea-
son. High-elevation birds were also at lower densities
(Bears 2002), and therefore transmission between
birds may have been lower.
Results suggest that high-elevation habitats may be
of conservation importance in limiting the spread of
blood parasites in birds. The Canadian Rockies may
play a particularly important role in limiting the rate
at which avian diseases travel east and west across
BEARS: PARASITE PREVALENCE IN DARK-EYED JUNCOS
the Rocky Mountains. Further work, including com-
parisons of parasite levels in females, and in other
species that breed over wide elevation ranges, is re-
quired in order to assess the generality of this parasite
refugium hypothesis in the Rocky Mountains of Can-
ada. Mechanisms by which high-elevation birds are
protected from parasites should also be explored.
Acknowledgments
Project funding was provided by NSERC, and
personal funding by NSERC PGS-A, Environment
Canada, Agriculture and Agri-foods Canada, Health
Canada, Fisheries and Oceans Canada, and Natural
Resources Canada. J. N. M. Smith provided helpful
advice in the preparation of this manuscript. S. Stearns
encouraged me with the pursuit of parasite quantifi-
cation across elevations. I benefited in the field from
the help of G. Brown, M. Bandura, and A. Bendzsak.
M. Adamson provided microscopy facilities. Thanks
to A. J. Erskine and two anonymous referees for
reviewing the manuscript.
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Received 24 October 2002
Accepted 4 November 2004
Movements of Subadult Male Grizzly Bears, Ursus arctos, in the
Central Canadian Arctic
RosBert J. GAu!, Puitip D. MCLOUGHLIN, RAY Case!, H. DEAN CLUFF?, ROBERT MULDERS!, and
FRANCOIS MESSIER?
'Wildlife and Fisheries Division, Department of Resources, Wildlife and Economic Development, Government of the Northwest
Territories, #600 5102-50th Avenue, Yellowknife, Northwest Territories X1A 3S8 Canada; e-mail: rob_gau@ gov.nt.ca
*Department of Biology, University of Saskatchewan, 112 Science Place, Saskatoon, Saskatchewan S7N 5E2 Canada
3Department of Resources, Wildlife, and Economic Development, Government of the Northwest Territories, North Slave
Region, P.O. Box 2668, Yellowknife, Northwest Territories X1A 2P9 Canada
Gau, Robert J., Philip D. McLoughlin, Ray Case, H. Dean Cluff, Robert Mulders, and Francois Messier. 2004. Movements of
subadult male Grizzly Bears, Ursus arctos, in the central Canadian Arctic. Canadian Field-Naturalist 118(2): 239-242.
Between May 1995 and June 1999, we equipped eight subadult male (3-5 yrs old) Grizzly Bears (Ursus arctos) with satellite
radio-collars within a study area of 235 000 km?, centred 400 km northeast of Yellowknife, Northwest Territories, Canada.
Subadult male annual home ranges were extraordinarily large (average = 11 407 km’, SE = 3849) due, in part, to their
movement’s occasional linear directionality. We believe their long-range linear movements may reflect some individuals
tracking the migration of Caribou (Rangifer tarandus). Seasonal daily movement patterns were similar to adult males that
were previously reported. The areas used by these bears are the largest ranges reported for any Grizzly Bears and the scale
of their movements may put individual bears in contact with humans even when developments are hundreds of kilometres
from the central home range of an animal.
Key Words: Grizzly Bear, Ursus arctos, home range, movements, subadult, central Arctic, Northwest Territories.
The population of Barren-ground Grizzly Bears
(Ursus arctos) in the Northwest Territories (NWT)
exists at a low density in the tundra and is considered
“sensitive” after a recent species-at-risk assessment
(Government of the NWT, 2000). As such, there is
concern for any increase in human presence that might
impact on their numbers.
Economic activity in the central Arctic of the NWT
and Nunavut increased dramatically in the early 1990s
with the discovery of diamonds. At present there are
three mines (two diamond, one gold) and numerous
base-metal, gold, and other diamond developments in
the region. To address the effects of these develop-
ments, in 1995 the Government of the NWT and the
University of Saskatchewan initiated the first multi-
faceted research program into the ecology of Barren-
ground Grizzly Bears inhabiting the central Arctic.
One aspect of our research program was to detail
the spatial requirements of the Barren-ground Grizzly
Bears in this region (McLoughlin 2000). However,
incidental to our primary objectives, we obtained data
on large-scale movements of some subadult male bears
(3-5 yrs old) that were also captured and monitored.
Although many aspects of bear ecology have been well
documented, descriptions of dispersal and movement
patterns for subadult Grizzly Bears remain rare and
difficult to obtain (McLellan and Hovey 2001). While
progress with DNA analysis may shed insights on sub-
adult dispersal in the future (see Waits et al. 1999;
Woods et al. 1999; Woods and Strobeck 2000), current
methods to examine dispersal in bears generally re-
quire marking young animals to identify when captured
or killed at a later date, or radio tracking 2- and 3-year
olds captured prior to or immediately following sepa-
ration from their mother. Our findings parallel and
complement McLoughlin et al. (1999) and McLoughlin
et al. (2003).
Methods
The study area was centred in Canada’s central
Arctic (66°10'N, 111°25'W), encompassing approxi-
mately 235 000 km? of mainland Nunavut and the
NWT (Figure 1). The study area was delineated by the
community of Kugluktuk, the Kent Peninsula, Aylmer
Lake, Mackay Lake, and Great Bear Lake. We previ-
ously noted the biophysical characteristics of the region
in Gau et al. (2002).
Between May 1995 and June 1999, helicopters were
used to search for and capture bears. Bears weighing
>110 kg (males) and >90 kg (females) were fitted with
tracking devices. There were the minimum weights we
considered bears robust enough to wear a collar safely.
We considered most two- and three-year-old bears too
small and growing too rapidly to be fitted with satel-
lite collars. Some telemetry methods (e.g., inserts or
breakaways to collar belting, ear-tag transmitters, ex-
pandable radio-collars) show promise; however, im-
provements are still needed (Costello et al. 2001).
Satellite (Service Argos Inc., Landover, Maryland,
USA) and conventional VHF radio-telemetry (Telonics
Ltd., Mesa, Arizona, USA) were used to obtain spatial
information on Barren-ground Grizzly Bears. Most
239
240
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 1. Subadult male Grizzly Bears, and their periods of long-range (>200 km) linear directional movement, captured
and collared between 1995 and 1999 in the central Canadian Arctic.
Number 95% fixed Mean Daily Movement (km/day) Linear Directional Movements
of kernal Late Distance Number
Bear Age Year locations range (km?) Spring Summer summer Autumn covered (km) of days
G595 4 1995 103 15 899 eS) 10.4 6.2 9) 539 Sif)
G600 3 1995 129 22 007 16.6 8.8 10.5 es 7719 59
G612 4 1995 91 4448 24.8 9.7 4.0 Nile ge 471 23
446 33
G618 5 1995 66 4540 6.1 6.7 9.5 5.6
G656 5) 1996 45 32 188 n/a! n/a! n/a! n/a! 273 26
305 40
G657 5) 1996 42 6162 n/a! n/a! n/a! n/a!
G689 4 1998 58 3662 n/a! n/a! n/a! n/a!
G700 4 1998 64 2349 7.9 59 4.2 ay 201 32
' <8 locations/season in every season of the year were recorded thus omitted from analysis.
collars were designed to transmit approximately 2-5
latitude-longitude locations every two days (8-hour
duty cycle) from 1 May to | November.
Our calculations and techniques for study of ani-
mals, ranges from satellite telemetry locations and rates
of movement (km/day) were previously described in
McLoughlin et al. (1999) and McLoughlin et al. (2003).
Annual home ranges were determined using the 95%
isopleth for bears only with 238 locations, so as not
to overestimate range size with smaller sample sizes
(Seaman et al. 1999). Also, only those animals that
transmitted 28 locations/season in every season of the
year were included for analysis. We defined seasons
according to changes in the diet of Barren-ground
Grizzly Bears during the active period (adapted from
Gau et al. 2002), including spring (den emergence-
20 June), summer (21 June-31 July), late-summer (1
August-9 September), and autumn (10 September-
den entrance).
Results
Of the male bears that were not in a family group
with their mother, 6 of the 45 males handled were too
small for collaring. However, we did collar and mon-
itor 8 subadult males between 3 and 5 years of age
out of a sample of 39 collared males (Table 1). Male
subadult movements were extraordinarily large and
annual home range averaged 11 407 km? (SE = 3849,
range 2349 — 32 188).
A unique feature of the subadult movements we
observed consisted of periods of long-range (>200 km)
linear directional forays. Five of the eight subadults
we followed exhibited this linear movement pattern.
For example, 4-year-old bear G612 in 1995 moved
471 km from 31 May to 22 June along a northerly
trek from the treeline to the Arctic coast. While the
other movements may not be as dramatic as G612 in
terms of time a distance was covered, long-range linear
directional movement appeared common for subadult
males in this Barren-ground Grizzly population. Bears
G595, G600, G612, and G656 had linear directional
movements in the spring; additionally, bears G612,
G656, and G700 had autumn linear directional move-
ments.
The subadult males followed a seasonal daily move-
ment pattern similar to adult males (see McLoughlin
et al. 1999). Only five bears met our criteria to inves-
tigate seasonal movements. Means were 12.6 km/d
(SE='3.6), 8:3 km/d' (SE = 0:9), 6:9’ kin/d"\(SE'=' 1:3);
and 7.6 km/d (SE = 1.2) for spring, summer, late
summer, and autumn, respectively. There was a clear
general trend from a high rate of movement (spring) to
lower rates for the rest of their active period, although
an ANOVA determined no significant differences
between seasonal means (F3 ,,= 1.6, P = 0.2).
Discussion
The annual ranges of adult and subadult Barren-
ground Grizzly Bears in the central Canadian Arctic
are the largest ranges yet reported for grizzlies in North
America (see Table 1, McLoughlin et al. 1999). How-
ever, there are very few published data about subadult
Grizzly Bear movement patterns either to refute or sup-
port our claim (McLellan and Hovey 2001). Jonkel
(1987), along with Mace and Waller (1997), noted
that dispersing immature brown bears tended to have
smaller home ranges than adult male bears. However,
LeFranc et al. (1987), along with Nagy et al. (1983),
summarized examples where subadults, believed dis-
persing from maternal home ranges, had home ranges
as large or larger than those of adult males. Regardless,
the magnitude of the movement patterns we observed
eclipses other results that have been previously pub-
lished.
We have gleaned valuable insights into the move-
ment patterns of Canadian Barren-ground Grizzly
Bears. Mean annual ranges were 7245 km? for adult
males and 2100 km? for females, with no difference in
2004
GAU, MCLOUGHLIN, CASE, CLUFF, MULDERS, and MESSIER: MOVEMENTS OF BEARS 241
Kent Peninsula
‘CORONATION
GULF
Kugluktuk
hie de oa
i \ MacKay axe
a Aylmer
=z)
250 km
co Nunavut
Northwest 7
Erritories
Lake
FiGureE |. Location of the study area in Canada’s central Arctic. The treeline indicates the approximate northern limit of
coniferous forest in the region.
the ranges for females of differing family status (Mc-
Loughlin et al. 2003). The large disparity between
adult males and females (5145 km7?), and especially
between subadult males and females (9307 km2), is in-
teresting since females introduce younger male bears
only to a seemingly small portion of the land they will
eventually use in the central Arctic. Although we can
expect a high degree of movement and population over-
lap among males in the central Arctic (McLoughlin et
al. 2002), it is possible that some of the subadult male
ranges we recorded were somewhat inflated. We sus-
pect that some bears in this study tracked the spring
migration of Caribou (Rangifer tarandus), a behaviour
previously suspected in northern Alaska for Barren-
ground Grizzlies (Reynolds and Garner 1987).
At the daily and seasonal movement rates we ob-
served for subadult males, because of their similarity to
adult male daily movement rates, it would be possible
for subadult males to have home range sizes typical
of male adults in the region. However, the unique fea-
ture of the subadult movements we observed appeared
to be their occasional linear directionality. Other than
homing behaviours of transplanted bears (Miller and
Ballard 1982), extended directional movements are
rare (McLellan and Hovey 2001). Explanations for long-
range bear movements include seeking out quality hab-
itat, spacing behaviour resulting from social interac-
tions with other bears, the abundance and distribution
of food (e.g., following migrating caribou herds), in-
breeding avoidance, and maximizing reproductive fit-
ness, or dispersal immediately following separation
from their mother (Rogers 1987; Pasitschniak-Arts
and Messier 2000). All these factors likely contributed
to the movement patterns of subadult males in the
Canadian central Arctic. McLoughlin et al. (1999) also
pointed out that Barren-ground Grizzly Bears have
larger scale movements when compared to other griz-
zly populations principally due to low primary pro-
ductivity in the tundra environment.
The spatial behaviour of subadult male grizzlies
increases their probability of coming in contact with
humans even when sites of human activity (e.g., ex-
242
ploration and hunting camps, industrial developments,
and communities) are of considerable distance from
the central home range of an individual. Subadult bears
in particular do not have the life-experience of mature
bears, are often imbued with more curiosity, and thus
are highly susceptible to human activity. Management
of bears in the central Arctic should focus on main-
taining low levels of human-caused mortality of bears,
with the realization that communities, hunting camps,
and mining/exploration camps may impact bears from
more than just the general vicinity. Also, the wide-
spread movements of subadult bears are a compelling
argument for a comprehensive and consistent bear
conflict avoidance program throughout the central
Arctic. Developments that might not be considered in
optimum Grizzly Bear habitat should have the tools
or resources to effectively manage potential problem
bears.
Acknowledgments
Funding for our research was supplied by the
Government of the NWT Department of Resources,
Wildlife, and Economic Development, University of
Saskatchewan, West Kitikmeot/Slave Society, Indian
and Northern Affairs Canada, BHP Diamonds, Rescan
Environmental Services, Axys Environmental Consult-
ing Ltd., Diavik Diamond Project, Monopros Limited,
Echo Bay Mines Ltd., Nunavut Wildlife Management
Board, the Federal Department of Indian Affairs and
Northern Development, the Northern Scientific Train-
ing Program, the Natural Sciences and Engineering
Research Council of Canada, and the Polar Conti-
nental Shelf Project (number 01298).
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H. B. Quigley, and S. L. Simek. 2001. Comparison of an
expandable radiocollar and an eartag transmitter for moni-
toring juvenile black bears. Western Black Bear Work-
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Gau, R. J., R. Case, D. F. Penner, and P. D. McLoughlin.
2002. Feeding patterns of barren-ground grizzly bears in
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Lefranc, M. N., M. B. Moss, K. A. Patnode, and W. C.
Sugg. 1987. Grizzly bear compendium. Interagency Griz-
zly Bear Commitee, Bozeman, Montana. 540 pages.
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Mace, R. D., and J. S. Waller. 1997. Spatial and temporal
interaction of male and female grizzly bears in northwest-
ern Montana. Journal of Wildlife Management 61: 39-52.
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McLoughlin, P. D. 2000. The spatial organization and habi-
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Kingsley, and C. B. Larsen. 1983. A study of grizzly
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Received 3 February 2002
Accepted 11 November 2004
Severe Chronic Neck Injury Caused by a Snare in a Coyote, Canis latrans
PIERRE-YVES Daoust!:3 and PETER H. NICHOLSON! 2
‘Canadian Cooperative Wildlife Health Centre, Department of Pathology and Microbiology (Daoust), and Class of 2002
(Nicholson), Atlantic Veterinary College, University of Prince Edward Island, 550 University Avenue, Charlottetown,
Prince Edward Island CIA 4P3, Canada
Present address: College Village Animal Clinic, 2036 E. Northern Lights Boulevard, Anchorage, Alaska, 99508, USA
3Corresponding author: e-mail: daoust @upei.ca
Daoust, Pierre-Yves, and Peter H. Nicholson. 2004. Severe chronic neck injury caused by a snare in a Coyote, Canis latrans.
Canadian Field-Naturalist 118(2): 243-246.
A two-year-old male Coyote, Canis latrans, in poor body condition was found in a moribund state with a snare deeply embedded
in the ventral portion of its neck, more than a month after the official end of the trapping season on Prince Edward Island.
This snare had presumably malfunctioned, and the cable had cut through the soft tissues of the neck as well as the trachea
and had obstructed both jugular veins and both common carotid arteries but had largely spared both vagosympathetic trunks.
Cases like this illustrate the need to continue to work on improving the efficiency of trapping methods, through research and
trapper education.
Key Words: Coyote, Canis latrans, trapping, injury, snare, Prince Edward Island.
Animal welfare issues surrounding trapping meth-
ods used to capture furbearers have been an ongoing
topic of discussion between wildlife managers and
animal protection groups for many years (Proulx and
Barrett 1991). Because of this and of the economic
importance of the fur trade to Canada, this country
has taken a leading role in developing national and
international standards for the performance of restrain-
ing- and killing-type traps. In the section of the Agree-
ment on International Humane Trapping Standards
(AIHTS) (1997*) dealing with killing type traps such
as the commonly used rotating-jaw Conibear trap, the
designated time limit to irreversible loss of corneal
reflexes in at least 80% of the animals of the target
species caught in the trap varies from 45 seconds in
Ermine (Mustela erminea) to 120 seconds in Pine Mar-
ten (Martes americana) to 300 seconds in 17 other
species of North American and European furbearing
animals. This Agreement requires that the parties in-
volved continue research with a view to lowering the
threshold requirements. Nonetheless, it implicitly rec-
ognizes that no killing trapping method used to cap-
ture wild animals can as yet guarantee a humanely
acceptable process in each instance. Manual neck
snares (where the animal provides the energy neces-
sary to tighten the snare) are widely used by trappers
to capture various furbearing animals, and Guthery and
Beasom (1978) and Boddicker (1982) discussed the
advantages and disadvantages of snares as compared
to other trapping devices. Snares are allowed in most
Canadian jurisdictions, except the southern regions
of some provinces. Being considered devices that are
constructed by the trappers themselves, they are not
subject to the testing requirements under the AIHTS
(1997), but their design must be approved by relevant
competent authorities such as provincial Departments
of Wildlife. This article describes an unsuccessful cap-
ture by snare of a Coyote (Canis latrans), with severe
consequences.
Case Description
On 26 February, 2002, a male Coyote, subsequently
determined to be 2 years old (Matson’s Laboratory,
Milltown, Montana, USA), was found alive but mori-
bund in a field in Kings County (46°08'N, 62°36'W),
Prince Edward Island (PEI), and was euthanized by a
shot to the head. It was submitted for necropsy to the
Diagnostic Laboratory of the Atlantic Veterinary Col-
lege, University of PEI. Postmortem examination
revealed that the animal had been caught in a snare
and had managed to escape. The snare’s cable, made of
galvanized steel wire 2 mm in diameter, was equipped
with a standard U-shaped lock, similar to an Adams
lock. The snare surrounded the animal’s neck, with a
portion of cable approximately 20 cm long dangling
beyond the neck. The coyote was in poor body con-
dition; the stomach was completely empty, and the
intestines contained only a small amount of ingesta.
However, some fat was still present around the base
of the heart, and a sample of diaphyseal bone marrow
from one of the femurs contained approximately 54%
fat, as measured by comparison of the wet and dry
weights of the sample. A large area of the skin along
the ventral side of the neck, about 50 cm?, was miss-
ing and had been replaced by scar tissue that released
a foul odour indicative of suppuration. The portion of
the cable along the ventral side of the neck had tran-
sected the full diameter of the trachea and was
embedded in scar tissue between the trachea and the
esophagus (Figure 1). The wall of the severed portion
of the trachea was completely healed, although the
tissue of repair had extended as a thin circular band
243
244
into the tracheal lumen, reducing its surface area to
about one-seventh of its original size (Figure 2). The
esophageal lumen was patent. There was no gross evi-
dence of suppuration accompanying the scar tissue that
surrounded the trachea and the cable. At the time of
necropsy, the cable was freely movable within the
affected tissues. The architecture of both jugular veins
disappeared at the level of the scar tissue. A thin probe
inserted into the cranial portion of the common caro-
tid artery on both sides of the trachea was blocked
from further progression at this level. The outline of
the vagosympathetic trunk on both sides was also lost
among the scar tissue. No other significant lesion was
seen at necropsy. Samples of the affected portion of
trachea and surrounding soft tissues were fixed in for-
malin, processed routinely for microscopic examina-
tion, and stained with hematoxylin and eosin.
Microscopically, the scar tissue surrounding the
affected portion of trachea consisted of abundant dense
fibrous tissue, much of which was birefringent under
polarized light. This fibrous tissue enclosed several
pockets of necrotic material (including debris of in-
flammatory cells) and, in some areas, contained numer-
ous cross sections of hair shafts. Serial sections of this
tissue, parallel to the length of the trachea, revealed
on both sides an artery, about 3 mm in diameter, and
a nerve, about 1 mm in diameter. Taking into account
the shrinkage that normally occurs in tissues processed
for microscopic examination, the diameters of these
two structures were compatible with those of the com-
mon carotid artery and vagosympathetic trunk, respec-
tively, for an animal of this size. Depending on the
section examined, the lumen of the common carotid
artery on both sides of the trachea was either empty
or partly or completely filled with a well organized
thrombus. The vagosympathetic trunk on both sides
was morphologically normal, except for a few degen-
erative lesions suggesting some loss of axons and their
myelin sheaths (wallerian degeneration). The tissue
within the tracheal lumen also consisted of dense fi-
brous tissue that enclosed some necrotic material and
numerous cross sections of hair shafts.
Discussion
Ideally, a snare should cause rapid death by neck
strangulation and subsequent asphyxiation. A quick
death is more humane and also gives the animal less
time to find a way out of the snare. A variety of factors
can influence the performance of a snare. Some lock-
ing mechanisms tighten less quickly and firmly than
others (Phillips 1996), or small kinks in the cable may
weaken it and make it easier to break or may prevent
full function of the lock. Inclusion of a swivel attach-
ing the lock to the cable (not present in this case) can
prevent the cable from kinking as the lock slides
along it. If the cable is not anchored firmly enough,
the animal may be able to pull off the snare before
maximum closure has been achieved. If death is not
THE CANADIAN FIELD-NATURALIST
Vol. 118
rapid and the cable is anchored too low, it may be more
easily accessible to the animal’s jaws and be chewed
through. Seventeen of 131 (13%) Coyotes caught by
one of three types of snares studied by Phillips (1996)
managed to escape, one by breaking the lock and 16 by
chewing through the cable.
In this Coyote, the relative abundance and density
of the scar tissue in the neck and, microscopically, its
birefringence under polarized light suggested that the
failed capture had occurred at least a few weeks prior
to death. The trapping season for Coyote and Red Fox
(Vulpes vulpes) on PEI officially terminated on Janu-
ary 15, more than a month before this animal was
found. The reason why it managed to escape capture
was not determined, although the portion of cable dan-
gling from its neck was of the right length to suggest
that the animal had chewed through it rather than pull
the whole cable from where it was anchored. Unfortu-
nately, the animal’s gums and teeth were not examined
for the presence of recent damage that would have sup-
ported this suggestion. At the time of escape, sufficient
closure of the snare may have already been achieved
for the cable to exert a strong pressure on soft tissues
of the ventral side of the neck and be forced gradually
through these tissues over the following weeks. Grad-
ual transection and concurrent repair of the tracheal
wall would thus have allowed it to remain continuous.
Alternatively, transection of all soft tissues, including
the trachea, could have occurred at the time of the
animal’s initial struggle in the snare. Such rapid tran-
section of the trachea, however, would more likely
have resulted in the formation of a gap between its
cut ends, thus preventing them from healing together.
Moreover, if the trachea had been rapidly transected,
the jugular veins would probably also have been cut
and the animal would presumably have bled to death.
The thicker hair coat and skin on the dorsal side of the
neck as compared to the ventral side (Scott et al. 2001)
and the tough nuchal ligament on the dorsal side (Evans
1993) may have prevented the cable from moving into
the tissues from that side.
The common carotid arteries and the vagus nerves
are important structures running along both sides of
the trachea. In this animal, the lumen of both common
carotid arteries was occluded. However, this is not a
critical problem, at least in canids. In dogs, both com-
mon carotid arteries can be ligated experimentally
without causing any clinical signs, implying that col-
lateral circulation (e.g., via the vertebral arteries) is
able to quickly compensate and transport sufficient
blood to the brain (Whisnant et al. 1956). Such col-
lateral circulation would have even more time to devel-
op if the obstruction were gradual, as is suspected to
have occurred in this case. The same reasoning applies
to the jugular veins, located much more superficially
in the ventral region of the neck, since collateral cir-
culation within the venous system can develop even
more readily than in the arterial side. Proper function
2004
DAOUST AND NICHOLSON: NECK INJURY IN A COYOTE 245
FiGure |. Right lateral view of the neck of a Coyote. The carcass is lying on its back, with the head to the left. The cable
from a snare has cut through the trachea (T) and is now lodged between it and the esophagus (E). The distortion of
the wall of the trachea just above the cable as been caused by scar tissue of repair. A metal rod has been inserted in
the lumen of the esophagus. The common carotid artery (C) and vagosympathetic trunk (V) are clearly visible to the
left of the cable. The lock of the snare is at the bottom of the picture. (Bar = 2 cm.) :
of at least one of the vagosympathetic trunks is, how-
ever, essential to life. The vagal (parasympathetic)
portion of these nerves originates in the brain and
supplies efferent and afferent innervation to many
vital organs, including the cardiovascular system and
digestive tract (Andrews and Lawes 1992; Esler 1992;
Guyton and Hall 1996). In particular, vagal stimula-
tion protects against excessive stimulation of cardiac
function by the sympathetic nervous system during
physical activity and stress. In this Coyote, it was not
possible to dissect the vagosympathetic trunk on either
side of the affected portion of trachea, because both
trunks were well embedded in scar tissue at this level.
However, careful microscopic examination showed
that both trunks were in large part morphologically in-
tact. Although their structure had likely been stretched,
and their path distorded, by the cable, the gradual pro-
cess through which this happened would presumably
have provided sufficient time for anatomic and physio-
logical compensation.
The exact cause of the eventual demise of this coy-
ote was not clear. There are undocumented reports by
veterinary practitioners of collars being left permanent-
ly on growing dogs and eventually becoming buried
under the skin, with damage limited to chronic sup-
puration of the subcutis (J. B. Miller, Department of
Companion Animals, Atlantic Veterinary College, Uni-
versity of PEI, personal communication). Similarly, a
square of a monofilament gillnet mesh was found al-
most totally embedded in the snout of an otherwise
healthy Porbeagle (Lamna nasus) that had been caught
on the Scotian Shelf (Benz et al. 2001). However, the
marked reduction in size of the tracheal lumen in this
Coyote may have reduced its stamina and prevented it
from foraging efficiently. The esophageal lumen was
FiGurRE 2. Cranial view of the trachea of a Coyote at the level
where the cable of a snare has cut through this organ.
The ventral side of the trachea is at the top. The carti-
laginous ring (CR) outlines what should be the normal
size of the tracheal lumen. Scar tissue of repair has
greatly narrowed this lumen. (Bar = | cm.)
246
patent, but the presence of the cable against its ventral
surface may have interfered with the passage of large
food boluses. Albeit seemingly superficial, the suppu-
rative process and, therefore, probable bacterial in-
fection, associated with the soft tissue damage would
have further drained the animal’s energy reserves.
Although this animal had not yet reached a stage of
emaciation, its poor body condition, combined with
the energy demands imposed by the winter season,
may have been sufficient to bring it to a stage of
exhaustion, perhaps combined with hypothermia. The
clinical significance, if any, of the mild damage seen
microscopically in the vagosympathetic trunks could
have been assessed only in the live animal.
The efficacy of various trapping devices, including
snares, can now be properly tested under standardized
laboratory conditions (Proulx and Barrett 1990, 1991).
Ultimately, however, the proportion of animals that
fail to die rapidly and undergo prolonged suffering
depends much on the experience and expertise of the
trappers in the field. Regardless of the exact cause of
failure of the snare in this case, its outcome emphasizes
the need for continued attention to appropriate train-
ing of hunters and trappers, in order to ensure that the
best trapping devices and capture techniques are used
consistently and, as a result, as few animals as pos-
sible undergo undue suffering. It also illustrates the
extreme resilience of Coyotes.
Acknowledgments
This article benefited greatly from discussions with
Neal Jotham.
Documents Cited [marked * in text]
Agreement on International Humane Trapping Standards.
The European Community, the Government of Canada,
and the Government of the Russian Federation. 1997.
Department of Foreign Affairs and International Trade,
Ottawa, Ontario, Canada. 31 pages.
THE CANADIAN FIELD-NATURALIST
Vol. 118
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Received 7 February 2003
Accepted 26 October 2004
Interactions of Brown Bears, Ursus arctos, and Gray Wolves, Canis
lupus, at Katmai National Park and Preserve, Alaska
Tom S. SMITH*, STEVEN T. PARTRIDGE”, and JOHN W. SCHOEN?
4 United States Geological Survey Alaska Science Center, 1011 E. Tudor Road, Anchorage, Alaska 99503 USA
>Alaska Office — National Audubon Society, 308 G. Street, #217, Anchorage, Alaska 99501 USA
Smith, Tom S., Steven T. Partridge, and John W. Schoen. 2003. Interactions of Brown Bears, Ursus arctos, and Gray Wolves,
Canis lupus, at Katmai National Park and Preserve, Alaska. Canadian Field-Naturalist 118(2): 247-250.
We describe several encounters between Brown Bears (Ursus arctos) and Gray Wolves (Canis lupus) that were observed at
Katmai National Park and Preserve in southwest Alaska. Katmai Brown Bears and Gray Wolves were observed interacting
in a variety of behavioral modes that ranged from agonistic to tolerant. These observations provide additional insight regard-
ing the behavioral plasticity associated with bear-wolf interactions.
Key Words: Brown Bear, Ursus arctos, Gray Wolf, Canis lupus, interactions, Katmai National Park and Preserve, Alaska.
Flexibility in mammalian behavior parallels the evo-
lution of large brains (Gilbert 1989). Gittleman (1986)
presented data showing that bears and wolves have
the highest brain:body weight ratios within the order
Carnivora, and claimed that this accounts for their
behavioral plasticity. The context of the encounter set-
ting, as well as the behavior of individual animals, like-
ly influences the resulting relationship between bears
and wolves at any given time.
Alaska Brown [Grizzly] Bears (Ursus arctos) and
Gray Wolves (Canis lupus) are sympatric over much
of their range and often compete for access to the
same food resources (Adams et al. 1995). As sym-
patric, apical predators, bears and wolves probably
interact frequently, although reports in the scientific
literature are scant. The accounts reported illustrate
the variable nature of Brown Bear — Gray Wolf inter-
actions, and range from mutual tolerance (Lent 1964),
to competitive (Adams et al. 1995; Hornbeck and
Horejsi 1986; Ballard 1982), to predatory (Ballard
1980; Hayes and Mossop 1987). This note describes
additional Brown Bear — Gray Wolf interactions ob-
served at Katmai National Park and Preserve on the
Alaska Peninsula, approximately 400 km southwest
of Anchorage, Alaska.
Wolves harass bears
On 24 June 2001, while conducting Brown Bear
research at Hallo Bay (154° 05’ W, 58° 27’ N) on the
Katmai coast, the authors observed a pack of five
wolves harass a pair of courting Brown Bears on the
edge of extensive salt marsh meadows (Carex spp.,
Plantago spp., Triglochin spp.). Prior to this observa-
tion, we had repeatedly heard wolves “chorus howI-
ing” (Harrington and Asa 2003), and noted that the
pack was gradually nearing our research field camp
situated on the far end of the meadow. Anticipating
their arrival, we positioned ourselves where we could
observe them when they entered the meadow. Although
it was late in the evening (2230 h Alaska Daylight
Time), it was still light enough to see so we patiently
waited while scanning the meadow. About 400 m south
of our position, a pair of Brown Bears foraged on
sedges in the meadow near a willow-alder (Salix spp.,
Alnus spp.) thicket. After we waited 10 minutes, the
wolf pack suddenly appeared, emerging from the dense
thicket about 25 m north of the two bears. The wolves
trotted single file in the direction of the bears. Three
of the five wolves had black-gray coats, similar in pat-
tern to that of the German Shepherd (C. domesticus)
breed of domestic dog; one wolf’s coat was pure white;
the other coal black. All five wolves appeared to be
mature adults, standing nearly 1 m at the shoulder and
similar in stature.
As one, the wolves circled south from the meadow’s
center toward the bears, which by then were focused
on the wolves. The five wolves lined up, head-to-head,
with the large male Brown Bear with < 2 m separating
the lead wolf and the bear. Suddenly, one wolf rushed
the maie bear, which in turn lunged and swatted at the
attacking wolf with its foreleg. Leaping forward, duck-
ing the bear’s defensive swat, then breaking away, the
wolves took turns harassing the male bear. The bear
responded to the attack with short lunges and aggres-
sive paw swats while slowly backing away. About a
minute into the confrontation, two wolves circled the
bear and lunge-nipped at his unprotected hindquarters.
In defense, the male bear swiftly spun around and swat-
ted at the closest attacker, but the wolf dodged the bear’s
swinging paw then trotted a few meters away, tail wag-
ging high. While the male bear counter-attacked the
wolves formerly at his rear, the other three wolves, now
at his unprotected hindquarters also began a nipping
attack, to which the bear again whirled around, lunged,
growled, and aggressively swatted at the wolves. The
wolves easily outmaneuvered the large bear’s paw
swipes and lunges with quick, evasive maneuvers.
The wolves and male bear repeated this attack-count-
er attack interaction several times before a group of
three wolves split from the pack and rushed the female
bear that had been watching from a distance of about
10 meters, near the edge of the thicket. Repeating the
same lunge, nip, and run strategy, the two groups of
wolves attacked each bear, which rapidly spun around
to defend themselves from the lunging-biting wolves.
At this point, approximately 10-20 meters separated
the two bears as they fended off the wolves. During
these aggressive interactions, neither wolves nor bears
were observed making physical contact, although the
confrontation appeared quite serious. After 5 minutes
of sustained confrontation, two wolves abruptly termi-
nated their attack and began chasing each other in tight
circles a short distance from the other wolves, wag-
ging tails held high. Moments later, the remaining three
wolves also withdrew, excitedly darted about, wagging
tails, and then joined the others. After regrouping about
30 m from the bears, all wolves participated in a series
of long, drawn-out “chorus” howls. From the forest
to the west, responding howls (possibly from a single
wolf) were heard in apparent reply. Moments later,
the pack trotted southward into the rapidly dimming
twilight, away from the bears and researchers. The
entire interaction took approximately 20 minutes from
the time the wolves were observed entering the mead-
ow to when they disappeared into the dusk.
To the best of our knowledge, there had been no
food source from which the wolves were attempting
to drive the bears. It appeared to us that this wolf pack
had encountered and approached these two bears and
attempted to test, or harass, them for a short period
before breaking off the encounter and moving on.
Wolves steal fish from bears
In mid-July 2001, a pair of Gray Wolves was ob-
served stealing Chum Salmon (Oncorhynchus keta)
from Brown Bears at Middle Creek where it empties
into Hallo Bay on the Katmai coast. National Park
Service (NPS) ranger Stephens Harper first saw the
wolves when they trotted past the rangers’ camp at
0830 h, heading to the nearby beach. Bears and wolves
frequent the tidal flats because the stream channel is
quite shallow at low tide, thus making salmon more
vulnerable to predation. Harper walked to the stream
mouth a few minutes before noon and observed two
wolves and five single adult bears fishing in close
proximity to one another.
Both wolves were gray with black highlights; one
appeared mature, while the other was younger, lankier,
and smaller (Figure 1). Fishing at the river mouth were
five adult single bears. The younger wolf bedded on a
gravel bar some distance from the bears while the other,
much closer, visually scanned them, apparently wait-
ing for one to catch a fish successfully. Once a bear
caught a fish, the older wolf would move in, head low,
and attempt to steal it by suddenly lunging and snag-
ging a portion away from the bear. In response, the
THE CANADIAN FIELD-NATURALIST
Vol. 118
bear would protect its quarry by bolting and running
after the wolf. Although there was a lot of chasing up
and down the stream banks, the wolf easily outran and
outmaneuvered these bears. This strategy worked,
however, in getting bears to abandon what was left of
the fish and the wolf would circle back around and eat
these scraps. In turn, the older wolf would trot over
to where the other was bedded, regurgitate a portion,
and then head back to where the bears were fishing.
During the entire hour that Harper watched, the wolf
determinedly attempted to snatch fish from bears.
Although these wolves attempted to catch salmon for
themselves on several occasions, they were unsuccess-
ful. One wolf, however, scavenged a Starry Flounder
(Platichthys stellatus) lying on the beach that had
been exposed at low tide.
Wolf displaces a bear from a moose carcass
In June 1997, an NPS employee observed a single
wolf feeding on a Moose (Alces alces) carcass near a
gravel pit adjacent to the Valley of Ten Thousand
Smokes Road, approximately 13 km from Brooks
Camp. Adjacent to the gravel pit is a wetland-pond
complex impounded by a Beaver (Castor canadensis)
dam. The following day, NPS employees Jim Gavin and
Tom Ferguson observed a wolf and bear simultaneous-
ly at the site. The wolf was gray with black highlights,
appeared mature, but thin. The bear was a young fe-
male, approximately 4 years of age. Initially, only the
bear fed on the carcass while the bedded wolf watched
from 40 m distant. After a while, the wolf moved in
close and began harassing the bear by charging and
biting at its hind legs. The wolf’s constant attacks dis-
rupted the bear’s feeding as it defended itself. After
1.5 min of intense harassment, the bear took flight into
the forest and the wolf usurped the carcass and started
feeding. After approximately 10 min of feeding, the
satiated wolf trotted off into the forest, reappeared
20 min later, then repeated the process several times,
likely caching food (L. Adams, USGS research biol-
ogist, personal communication), or transporting it to
young at a den nearby. Gavin observed the wolf feed
in this manner for three consecutive days. On the third
day, while the wolf was absent, the bear returned and
resumed control of the Moose carcass. The wolf re-
appeared but did not approach any closer than 40 m
to the feeding bear. Gavin did not observe the wolf
attempt to displace the bear as before, although his
observation sessions were only 30 min daily.
Bears and wolves fishing together
Chum Salmon enter freshwater to spawn in Hallo
Bay’s Middle Creek from early July through August.
In 2001, Brown Bears and wolves were repeatedly
observed fishing side-by-side (approximately 5 m apart)
at this location with no apparent interactions or obvious
concern toward the other species. Like bears, wolves
sat patiently on the gravel bank and scanned the water
for incoming salmon. Upon catching sight of an incom-
2004
ing salmon, both bears and wolves would leap into the
stream and attempt to capture it. Both bears and wolves
appeared indifferent to one another, completely fo-
cused on fishing.
Similarly, in August 1992, NPS rangers B. Holmes
and S. Klenzendorf observed a lone wolf and several
bears fishing in close association for 2 h at Margo
Creek (155° 03’ W, 58° 29’ N) in the western portion
of Katmai National Park. At 1210 h on 13 August, an
old female Brown Bear was fishing when a wolf ap-
peared suddenly on the riverbank, watched the bear,
and then sat down. The wolf was moderate in size and
of gray coloration. The wolf wandered in the direction
of the bear, entered the creek and retrieved a spawn-
ing Red Salmon (Oncorhynchus nerka). As the wolf
fed, the bear wandered downstream towards the wolf.
Consequently, the wolf abandoned its catch, moved
quickly away, picked up another salmon, and then
moved into the nearby White Spruce (Picea glauca)
forest. At 1245 h, the wolf reappeared from the forest,
plunged into the creek and emerged with a live salmon.
Carrying the salmon in its mouth, the wolf disappeared
again into the heavy cover of the forest. At 1255 h, the
wolf reappeared and entered the creek in search of sal-
mon. As the wolf waded about searching for fish, the
same bear waded downstream until she and the wolf
were about 20 m apart. In apparent response, the wolf
abruptly ceased fishing, climbed out of the river and
sat and watched the bear as it sought fish in that section
of stream. Twenty minutes later, the wolf moved up-
stream and caught a salmon. As the wolf fed, a large
adult male bear suddenly appeared thus causing the
wolf to leave the area. The large male bear quickly
caught a fish, then left the river, at which time the wolf
reappeared. Moments later, the wolf caught a fish then
reentered the forest. The observers left at 1402 h, im-
pressed with the degree of tolerance the two species
appeared to have for one another.
Wolf and bears traveling together
In June 1989, Aleska Szweda, an NPS employee
stationed at Brooks Camp (155° 05’ W, 58°33 ‘ N) in
the western portion of Katmai National Park, observed
a lone wolf traveling in the company of two Brown
Bears. Szweda was driving along the park road, approx-
imately 8 km from Brooks Camp, when she noticed
what appeared to be two bears in the middle of the
roadway, approximately 400 m ahead. The lumbering
vehicle’s approach prompted the bears to abandon the
roadway suddenly, exposing a wolf that had appar-
ently been in their immediate company (<2 m). The
wolf too left the road, following the bears into the
forest.
The following day, five park visitors reported see-
ing two bears and a wolf cross the Brooks River at a
location known locally as the Oxbow. It was generally
believed that these were the same three observed by
Szweda the day previous along the park road, 8 km
distant. The bears and wolf were clearly traveling as
SMITH, PARTRIDGE, and SCHOEN: INTERACTIONS OF BEARS AND WOLVES
249
FIGURE 1. Gray Wolf at Hallo Bay, Katmai National Park and
Preserve, Alaska (Kent Fredriksson photograph).
a group as they worked their way down the riverbank,
probed the riverbed for the shallowest crossing, and
then emerged on the other side. It was reported that
the trio fed together in an unusual manner; when the
bears caught fish they fed only upon the brains and
skin, leaving the rest for the wolf which, sitting im-
mediately adjacent, would spring forward, snatch and
eat the remainder. It is not unusual to see Red Foxes
(Vulpes vulpes) or gulls (Larus spp.) attempting to
snatch fish scraps from Brown Bears on salmon streams.
But bears in these instances are far from cooperative,
often lunging at the would-be thief, catching and killing
them on occasion (T. Smith, personal observation).
However, in this case, the bears tolerated the wolf’s
presence and, according to observers, did nothing to
discourage its very close (1 m) proximity to them.
Acknowledgments
We gratefully acknowledge the contributions of
Brian Holmes, Ronald Squibb, Tamara Olson, Kerry
Sullivan, Jim Gavin, Aleska Szweda, Stephens Harper,
and Layne Adams. We also thank Rick Clark and Troy
Hamon of Katmai National Park for funding Brown
Bear research in the park.
Literature Cited
Adams, L. G., F. J. Singer, and B. W. Dale. 1995. Caribou
calf mortality in Denali National Park, Alaska. Journal of
Wildlife Management 59: 584-594.
Ballard, W. B. 1980. Brown Bear kills Gray Wolf. Canadian
Field-Naturalist 94: 91.
Ballard, W. B. 1982. Gray wolf-brown bear relationships in
the Nelchina Basin of south-central Alaska. Pages 71-80
in Wolves of the world: perspectives of behavior, ecology,
and conservation. Edited by F. H. Harrington and P. C.
Paquet. Noyes Publications, Park Ridge, New Jersey.
Gilbert, B. K. 1989. Behavioral plasticity and bear-human
conflicts. Pages 1-8 in Bear-People Conflicts: Proceedings
of a Symposium on Management Strategies. Edited by
M. Bromley. Yellowknife, Northwest Territories.
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Vol. 118
Gittleman, J. L. 1986. Carnivore brain size, behavioral ecol-
ogy and phylogeny. Journal of Mammalogy 67: 23-36.
Harrington, F. H., and C. S. Asa. 2003. Wolf communica-
tion. Pages 66-103 in Wolves: behavior, ecology and con-
servation. Edited by L. David Mech and Luigi Boitani.
The University of Chicago Press. Chicago, Illinois.
Hayes, R. D., and D. H. Mossop. 1987. Interactions of wolves,
Canis lupus, and brown bears, Ursus arctos, at a wolf den
in the northern Yukon. Canadian Field-Naturalist 101: 603-
604.
Hornbeck, G. F., and B. L. Horejsi. 1986. Grizzly bear,
Ursus arctos, usurps wolf, Canis lupus, kill. Canadian Field-
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Received 17 February 2003
Accepted 2 December 2003
Wild Turkey, Meleagris gallopavo silvestris, Behavior in Central
Ontario During Winter
Linu P. Ncuyen,! JOSEF HAMR,” and GLENN H. PARKER!
'Department of Biology, Laurentian University, Ramsey Lake Road, Sudbury, Ontario P3E 2C6 Canada
*Northern Environmental Heritage Institute, Cambrian College of Applied Arts and Technology, 1400 Barrydowne Road,
Sudbury, Ontario P3A 3V8 Canada
3Present address: Watershed Ecosystem Graduate Program, Trent University, 1600 West Bank Drive, Peterborough, Ontario
K9J 7B8 Canada
Nguyen, Linh P., Josef Hamr, and Glenn H. Parker. 2004. Wild Turkey, Meleagris gallopavo silvestris, Behavior in Central
Ontario During Winter. Canadian Field-Naturalist 118(2): 251-255.
Home range size, food habits, and roost site selection are described for the Eastern Wild Turkey (Meleagris gallopavo
silvestris) introduced on the Precambrian Shield in central Ontario during the winters 1999 and 2000. Monthly home range
size was correlated primarily to snow depth, although it was also likely associated to other factors, including food avail-
ability and/or roost site availability. Ferns and allies were used more than available, whereas monocots were used less than
expected. Roost site-selection was primarily influenced by tree height. If the Eastern Wild Turkey is to expand its northern
range in Ontario, winter food and roost site availability may be the primary determinants for successful introductions.
Key Words: Eastern Wild Turkey, Meleagris gallopavo silvestris, home range size, roost site, food availability, Ontario.
The Eastern Wild Turkey (Meleagris gallopavo sil-
vestris) is a large, highly adaptable gallinaceous bird
that is common throughout southern Ontario as a result
of introductions in the last 20 years (Bellamy 2001).
For northern turkey populations, winter is the most
stressful season for satisfying energy demands (Ober-
lag et al. 1990). Variations in home range size and re-
source selection appear to be governed by snow depth
(Porter et al. 1980; Vander Haegen et al. 1989) and,
to a lesser extent, ambient temperature (Oberlag et al.
1990). Numerous accounts of turkey winter biology
(e.g., Glover and Bailey 1949; Wunz and Hayden 1975;
Porter et al. 1980; Kilpatrick et al. 1988; Vander Haegen
et al. 1989), refer primarily to studies conducted in the
United States. The winter biology of turkeys in these
southern habitats may be different from that of birds
living in Ontario due to inherent differences in climate
and habitat. Hence, we report on home range size,
food habits, and roost site use by Eastern Wild Turkeys
introduced to the Precambrian Shield in central Ontar-
io during the winters 1999 and 2000. It was hypothe-
sized that turkey movement and forage availability were
inversely related to snow depth. It was also hypothe-
sized that the tallest trees provided optimum wild tur-
key roost sites due to their sturdiness.
Study Area
This study was conducted from November to March
1999/2000 and 2000/2001 near Noélville, approximate-
ly 60 km southeast of Sudbury, Ontario (46°10'N,
80°25'W). The 169-km/? study area was located within
the Great Lakes—St. Lawrence Ecotonal Forest Region
(Rowe 1972), characterized by flat to rolling topog-
raphy, interrupted by rock outcrops and narrow valleys.
The habitat consisted of 20% softwood forests, 37%
hardwood forests, 28% abandoned pasture and hay-
fields, and 15% residential areas and rock outcrops.
Beef farming was the dominant land use, with many
fields cultivated for corn silage or pasture grasses.
The forested areas were dominated by White Birch
(Betula papyrifera) and Trembling Aspen (Populus
tremuloides), interspersed with Balsam Fir (Abies
balsamea), Eastern White and Red Pine (Pinus .strobus,
P. resinosa), Red Oak (Quercus rubra), White Spruce
(Picea glauca), Red and Sugar Maple (Acer rubrum,
A. saccharum), and Eastern Hemlock (Tsuga canaden-
sis). Shrubs included raspberries (Rubus spp.), Bracken
Fern (Pteridium aquilinum), blueberries (Vaccinium
spp.), Beaked Hazel (Corylus cornuta), and asters
(Aster spp.).
January, the coldest month of the year, had a mean
temperature of —13.9°C and —10.5°C in 2000 and 2001,
respectively. Total snowfall was 216.0 cm in 1999-
2000 (10.0% below the 30-year norm) and 328.3 cm
in 2000-2001 (22.2% above the 30-year norm). Snow
depths exceeded 25 cm for 38 days in 1999-2000 and
111 days in 2000-2001.
Methods
Capture and Radio-Tracking
Wild Turkeys were captured with rocket nets (Hawk-
ins et al. 1968) in southern Ontario and upper New
York for introduction to the study area in February
and March 1999 (10 males and 26 females) and
March 2000 (13 females). Female turkeys were fitted
with backpack-style, 32.5 g (1% of mean body mass),
mortality-mode VHF radio-transmitters (Holohil Sys-
tems Ltd., Carp, Ontario). We tracked radio-fitted birds
two to four days per week, or until battery failure, from
1999 to 2001. Locations of birds were determined by
251
Diy)
triangulation using >3 locations (Heezen and Tester
1967) taken less than 15 minutes apart with a 2-element
H antenna and portable receiver-scanner (Model STR-
1000, Lotek Engineering Inc., Newmarket, Ontario).
Average telemetry error was 156.9 m + 21.1 SE (n=
40).
Home Range
Monthly home range sizes were calculated using
the 100% minimum convex polygon method (White
and Garrott 1990). All spatial analyses were conducted
using an ArcView GIS software (Environmental Sys-
tems Research Institute, Redlands, California), with the
Animal Movement Analysis (Hooge and Eichenlaub
1997) and Spatial Analyst Extensions.
Forage Selection
Active turkey feeding areas were identified by tracks,
and forage plants were identified and collected. Crop
contents from dead specimens provided a supplemen-
tal source of information. Forage species eaten were
recorded regardless of the number of bites using a
modified point-quarter method (Jost et al. 1999) during
2000-2001. Point samples of available plants adjacent
to turkey tracks in the herb (less than 0.5 m) and shrub
(0.5 to 2.0 m) layers were selected randomly and
identified. Plants were grouped into five classes: (1)
mosses, (2) ferns and allies, (3) conifers and allies,
(4) monocots, and (5) dicots.
Roost Site
Roost sites were found by (1) observing commonly
used trees, (2) finding turkey droppings under trees
(Hoffman 1968), (3) examining areas where Wild Tur-
keys were common after snowfalls, or (4) locating
radio-fitted birds on trees before sunset. Locations of
roost sites were determined using a Global Positioning
System (GARMIN International Inc., Olathe, Kansas).
Equal numbers of random trees that may have pro-
vided potential roost sites within our study area were
generated in ArcView GIS. Random trees were located
using a Global Positioning System, and trees that had
diameter at breast height (dbh) less than 10.2 cm were
discarded (Kilpatrick et al. 1988).
Elevation, tree dbh, percent canopy cover, canopy
density, distance to habitat edge, distance to open water,
and tree height for actual and selected trees were mea-
sured. Elevation was measured with an altimeter, tree
dbh with a diameter tape, percent canopy cover by
averaging readings at each compass directions (N, S,
W, E) using a convex spherical densiometer, canopy
density by counting tree trunks of dbh =10.2 cm with-
in 5 m of actual roost sites, and tree height from esti-
mates on a subjectively selected “average” tree. Dis-
tances to habitat edge and open water were also deter-
mined by plotting roost sites on Ontario Base Maps
(OBM) and Forest Resource Inventory (FRI) maps.
The used habitat variables either had been previously
described in the literature (Tzilkowski 1971; Kilpatrick
et al. 1988; Chamberlain et al. 2000), or were hypoth-
THE CANADIAN FIELD-NATURALIST
Vol. 118
esized correlates based on the winter biology of the
species.
Statistical Analyses
Data were pooled to maintain sufficient sample
size, unless otherwise noted (Alldredge and Ratti 1986;
Thomas and Taylor 1990). Home range sizes were
compared between years using the Mann-Whitney U-
test. Monthly home ranges were compared using the
Kruskal Wallis test (Zar 1999). Two measurements
used to examine the effects of winter on monthly home
range size were (1) number of days with snow depths
over 25 cm (Porter et al. 1980), and (2) number of
days with minimum temperature less than —16.2°C
(Oberlag et al. 1990). Spearman rank-order correlation
analyses were used to compare mean monthly home
range size with these two variables. The number of
days with snow depth over 25 cm and the number of
days with minimum temperature less than —16.2°C
were also compared between years using the Mann-
Whitney U-test.
Chi-square analysis was used to compare the fre-
quencies of plants browsed by turkeys to availability
(Neu et al. 1974). When forage selection differed, a
Bonferroni Z-test was used to identify plants that
were browsed more or less than availability (Byers et
al. 1984). A series of one-way analyses of variance
(ANOVA) was used to compare each habitat variable
associated with roosting and random sites. Pearson cor-
relation analyses were performed for the significant
habitat variables. In order to minimize artifacts from
environmental variations in habitat characteristics, an
analysis of covariance (ANCOVA) was used to deter-
mine significant habitat variables. All analyses were
conducted using Statistical Package for the Social
Sciences (SPSS Inc., Chicago, Illinois) with signifi-
cance level set at a = 0.10.
Results
Home Range
We obtained 441 locations from 12 radio-fitted
turkeys from November 1999 to March 2000 and
from November 2000 to January 2001. Mean winter
home range size differed between years (U = 142.0,
P =0.002), as did monthly home range size (Novem-
ber: U = 9.0, P = 0.083; December: U = 8.0, P = 0.060:
January: U = 3.0, P = 0.020). In addition, home range
size differed among months in the two years (c? = 7.79,
df = 4, P = 0.100; Table 1). Monthly home range size
was correlated with the number of days with snow
depth more than 25 cm (7, = —0.71, n= 59, P = 0.050)
and the number of days with minimum temperature
less than —16.2°C (r, = 0.75, n= 59, P = 0.031).
The number of days with snow depth over 25 cm
differed (U = 4.0, P = 0.095) between 1999-2000
(9.60 + 5.91 days, n = 5) and 2000-2001 (22.6 + 4.88
days, n = 5), while the number of days with mini-
mum temperature less than —16.2°C did not differ
(U = 10.5, P = 0.690) between 1999-2000 (10.00 +
2004 NGUYEN, HAmr, and PARKER: WILD TURKEY BEHAVIOR 255
TABLE |. Winter home range size (ha) of Eastern Wild Turkey hens in Noélville, near Sudbury, Ontario, 1999-2001 (SE =
standard error of the mean).
1999-2000 2000-2001 1999-2001 (Pooled Data)
n Mean SE n Mean SE n Mean SE
Winter 9 249 60 4 58 19 13 204 47
Monthly
November 9 399 198 5 90, 54 14 288 132
December 9 145 60 5) 4] 8 14 108 40
January 9 302 130 4 38 10 13 221 95
February 9 75 27 - re - 9 15 27
March 9 323 170 - - - 9 323 170
4.15 days, n = 5) and 2000-2001 (11.40 + 3.63 days, Pine, and White Spruce, were used in proportion to
n= 5). In 1999-2000, snow was generally packed or availability. Monocots, including Quackgrass (Elymus
crusted with seeps and small streams remaining un- repens) and Timothy (Phleum pratense), were used less
frozen. In 2000-2001, deep, powdery snow was com- _ than available, while dicots, including ash (Fraxinus
mon, and most seeps were frozen by mid-winter. spp.), aster, Beaked Hazel, burdock, Choke Cherry
(Prunus virginiana), Dogwood (Cornus stolonifera),
Evening Primrose (Oenothera biennis), Fireweed (Epi-
lobium angustifolium), goldenrod, Northern Wild Rai-
sin (Viburnum cassinoides), raspberry (Rubus spp.),
Soybean, Speckled Alder (Alnus incana), Swamp
Thistle (Cirsium muticum), and willow (Salix spp.)
were used in proportion to availability.
Forage Selection
Wild Turkeys foraged primarily on clovers (Trifo-
lium spp.), asters (Aster spp.), goldenrods (Solidago
spp.), and fertile fronds of the Sensitive Fern (Onoclea
sensibilis) in the winter 1999-2000. Turkeys avoided
species such as Cattail (Typha latifolia) and Meadow
Sweet (Spiraea latifolia). Crops (n = 2) contained grass
seeds and Sensitive Fern spore heads in late winter, Roost Site Characteristics
confirming observations of turkeys feeding in the field. Trembling Aspen, American Basswood (Tilia ameri-
Ostrich Fern (Matteuccia struthiopteris), Trembling cana), Jack Pine (Pinus banksiana), Eastern White
Aspen (P. tremuloides) buds, Corn (Zea mays), Smooth Pine, White Spruce, and Eastern White Cedar (Thuja
Wild Rose (Rosa blanda), and ragged moss (Brachy- occidentalis) were used as roost sites. Tree heights at
thecium spp.) were other winter foods. Burdocks roosting sites averaged 13.9 + 0.8 m, and were higher
(Arctium spp.), Sensitive Fern, and Soybeans (Glycine _ than the tree heights (8.8 + 0.7 m) measured at ran-
max) comprised 21.4%, 23.0%, and 37.4% of the tur- dom sites (F, 5, = 20.98, P = 0.0001; Table 3). Mean
keys’ diet, respectively, in 2000-2001. dbh of trees associated with roost sites, 37.7 + 3.0 cm,
Forages used by turkeys differed from availability was significantly larger (F, 5, = 15.69, P = 0.0007)
(c? = 40.38, df = 4, P < 0.0001; Table 2). Mosses _ than tree dbhs on random sites (24.1 + 1.7 cm). Roost
were used in proportion to availability while ferns and __ site topographical elevations averaged 217.1 + 7.1 m
allies, including Bracken (Pteridium aquilinum) and and were significantly higher (F, 5, = 4.49, P = 0.0455)
Sensitive Ferns, were selected more than available. than the 188.8 + 11.3 m measured at random sites. Can-
Conifer and allies, including Balsam Fir, Eastern White opy cover (73.3 + 8.8%), tree density (849.3 + 127.7
TABLE 2. Chi-square analysis and Bonferroni Confidence Intervals for winter ground forage used by Eastern Wild Turkeys
during winter in Noélville, near Sudbury, Ontario (v7 = 40.38, df = 4, P < 0.0001).
Forage Forage Forage Proportion Proportion 90% Confidence
Class Selected Available Selected Available Interval on Proportion
Mosses 0.1 1.0 0.001 0.004 0.000-0.006°
Ferns and allies 43.0 32.0 0.230 0.124 0.158-0.302°
Conifers and allies 5.0 4.0 0.027 0.016 0.000-0.055°
Monocots 0.1 13.0 0.001 0.050 0.000-0.006*
Dicots 139.0 208.0 0.743 0.806 0.669-0.817°
Total 187.2 258.0
“Proportions greater than the upper confidence limit indicates use less than available.
Proportions within the confidence limit indicates use equal to availability.
‘Proportions less than the lower confidence limit indicates selection greater than available.
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 3. Comparison of physiographic characteristics of Eastern Wild Turkey roost (n = 12) and random (n = 12) sites in
Noélville, near Sudbury, Ontario.
Roost sites
Habitat characteristic Mean SE
Height (m) 13:9 0.8
Tree dbh (cm) B07 3.0
Canopy coverage (%) 133 8.8
Density (trees/ha) 849.3 127
Elevation (m) PAIN HA
Distance to habitat edge (m) 97.5 Del
Distance to open water (m) ABS 18.6
trees/ha), distance to clearing (97.5 + 21.1 m), and dis-
tance to open water (73.5 + 18.6 m) of roost trees did
not differ (all P > 0.10) from those at random sites.
Height of roost site was correlated with tree dbh
(r= 0.78, n = 24, P = 0.003). There was no correlation
between elevation and tree dbh (r = —0.36, n = 24,
P = 0.245) nor elevation and tree height (7 = 0.04, n
= 24, P = 0.900). Tree height was primarily responsi-
ble for the differences between roosting and random
sites, regardless of the covariate tree dbh (F, 5, = 3.45,
P = 0.077). Tree dbh did not differ between roosting
and random sites once the covariate height was statis-
tically controlled (F, 5, = 15.87, P = 0.513).
Discussion
Winter mean home range sizes for turkeys released
in northern Ontario (204 + 47 ha) were similar to
those of turkeys introduced to Indiana (Miller et al.
1985), and Iowa (Little and Varland 1981), but exceed-
ed those reported in Ohio (Clark 1985) and in southern
Ontario (Weaver 1989). Although previous studies
reported a decline in monthly home range size be-
tween November to March (Porter 1977; Miller et al.
1985), this pattern was not observed in 1999-2000.
This suggested that movement in late winter (1999-
2000) was not limited by snow depth. On several occa-
sions when snow covered local food resources, birds
increased flight distance to otherwise unused parts of
the home range. Snow depth was inversely related to
winter and monthly home range size, confirming data
from previous studies in Minnesota (Porter 1977),
Indiana (Miller et al. 1985), Pennsylvania (Wunz and
Hayden 1975), and southern Ontario (Weaver 1989).
Glover and Bailey (1949) described the Wild Turkey
as a nomadic feeder with a tendency to sample a wide
variety of forages, primarily dictated by their avail-
ability. The heavy use of ferns and allies was almost
exclusively due to the selection of fertile fronds of
the Sensitive Fern found in lowland hardwood sites
and along seeps. Decker et al. (1991) reported that
Sensitive Ferns were foraged in large quantities by
Wild Turkeys because of their high nutritional content
(crude protein 18.6%) and/or the high availability of
Random sites
Mean SE F P
8.8 0.7 20.98 0.0001
24.1 N57 15.69 0.0007
70.4 9.7 0.05 0.8303
764.3 110.9 0.25 0.6206
188.8 ARS 4.49 0.0455
64.8 7-7 1.42 0.2468
122.1 34.7 152 0.2303
this food in concentrated, relatively snow-free patches.
Vander Haegen et al. (1989) reported that fields spread
with manure were also important sources of winter
food in Massachusetts, but the value of manure to win-
tering turkeys in central Ontario was questionable, as
emaciated birds were observed to ignore manure piles.
Glover and Bailey (1949) reported wariness by turkeys
of supplemental feeding sites with corn and oats in
West Virginia when natural forage (e.g., wild grape,
Vitis spp.) was absent.
Standing crops, such as Soybean or clover, provid-
ed nutritious food in moderate snow conditions during
early winter. Soybeans contain protein, but also pro-
duce trypsin inhibitors, which lower digestibility and
fat absorption (McNaughton and Reece 1980, in Loesch
and Kaminski 1989). Post-mortems in winter 2000-
2001 (n = 5) verified that emaciated turkeys were
under severe nutritional stress, and had catabolized
significant amounts of muscle tissue.
Forages that were present in the study area, but may
have been underestimated in use, included conifer and
hardwood trees. Although primarily ground feeders,
Eastern Wild Turkeys are capable of flight, but forage
obtained in the tree-canopy layer is difficult to sys-
tematically record. Turkeys were observed feeding on
Trembling Aspen buds on several occasions; however,
the results indicate that prolonged periods of deep snow
severely limited food availability for Wild Turkeys in
northern Ontario.
Roosting sites of turkeys were the tallest and largest
trees, usually conifers, which were found at higher
elevations. Conifers may reduce wind speed and heat
loss (Kilpatrick et al. 1988). Tzilkowski (1971) found
that turkey winter roosts were dominated by large decid-
uous trees in Pennsylvania, suggesting that tree height
and sturdiness were important factors. However, Cham-
berlain et al. (2000) suggested that turkeys roost in the
nearest suitable habitat at the end of the day. Although
roost sites were closer to open water than random sites,
this proximity appeared to be due to forage availability.
Turkeys used snow to meet winter water requirements
in this study. Exum et al. (1985) argued against Wild
Turkey dependence on open water in southern Ala-
1
ii
2004
bama during spring and summer; however, Kilpatrick
et al. (1988) suggested that winter foods in Rhode Is-
land were too low in water content to meet the species’
needs. Roosting sites may have been closer to water
because of the accelerated growth of trees associated
with moist environments (Kilpatrick et al. 1988).
The results of this study suggest that (1) winter food
and roost site availability are the primary factors deter-
mining successful turkey introductions in northern On-
tario, (2) stands of Soybean or Corn are not sufficient
to support Wild Turkey populations unless natural foods
are available, and (3) snow depth is an important
parameter influencing successful reintroduction of
this species on the Precambrian Shield.
Acknowledgments
Financial and logistic support was provided by the
West Arm/French River Wild Turkey Chapter, Ontario
Federation of Anglers and Hunters, Cambrian College
of Applied Arts and Technology, Laurentian University,
Ontario Ministry of Natural Resources, Sudbury Dis-
trict, and the Ontario Living Legacy Fund. We thank
J. Craig and other landowners in Noélville for allow-
ing fieldwork on their property, M. N. Hall for the
Ontario Base Maps and Forest Resource Inventory
data, and G. M. Courtin for meteorological data.
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Received 24 March 2003
Accepted 15 November 2004
Fifteenth Census of Seabird Populations in the Sanctuaries of the
North Shore of the Gulf of St. Lawrence, 1998-1999
JEAN-FRANCOIS RAIL and GILLES CHAPDELAINE
Canadian Wildlife Service, P. O. Box 10100, Ste-Foy, Québec G1V 4H5 Canada
Rail, Jean-Francois, and Gilles Chapdelaine. 2004. Fifteenth census of seabird populations in the sanctuaries of the North
Shore of the Gulf of St. Lawrence, 1998-1999. Canadian Field-Naturalist 118(2): 256-263.
For the first time since the tradition began in 1925, the quinquennial census of seabirds in the Migratory Bird Sanctuaries of the
North Shore of the Gulf of St. Lawrence was divided between two years in 1998-1999. Trends between 1993 and 1998-1999
were variable across species and sanctuaries. In particular, following the large decreases in both species noted in 1993, the
1998-1999 survey showed that Black-legged Kittiwakes had declined further, while the number of Herring Gulls had stabilized.
Alcids were all doing well except for the Atlantic Puffin which showed severe yet unexplained drops at all major colonies.
Law enforcement efforts appear reflected in seabird population trends, as well-patrolled sanctuaries such as St. Mary’s Islands
seem to do well, whereas many species at the Baie des Loups and Ile a la Brume sanctuaries are far from their historical levels.
In addition to a better law enforcement program, research is needed in order to identify other conservation problems that
some species may be facing.
Pour la premiere fois depuis 1925, l’inventaire quinquennal des oiseaux marins des refuges d’ oiseaux migrateurs de la Céte-
Nord du Golfe Saint-Laurent fut mené sur deux ans, soit en 1998 et 1999. Les tendances des populations entre 1993 et 1998-
1999 étaient variables selon |’espéce et le refuge. En particulier, suite a une décroissance notée chez les deux espéces en 1993,
Vinventaire de 1998-1999 a démontré que la Mouette tridactyle avait encore diminué, tandis que le nombre de Goélands
argentés s’ était stabilisé. Les populations d’ Alcidés ont toutes semblé en bonne santé sauf celle du Macareux moine dont les
colonies importantes ont diminué de facon sévére et inexpliquée. Les efforts de protection par l’application de la loi se reflétent
visiblement dans les tendances des populations d’ oiseaux de mer, puisque les refuges les mieux surveillés comme celui des
Iles Sainte-Marie vont bien, alors que plusieurs espéces aux refuges de Baie des Loups et de l’ile 4 la Brume sont loin de leurs
niveaux historiques. En plus d’un meilleur programme d’ application de la loi, la recherche est nécessaire pour identifier les
autres problémes de conservation auxquels certaines espéces font face.
Key Words: Seabirds, populations, sanctuaries, Gulf of St. Lawrence, Atlantic Puffin, larids, alcids.
Apart from its major use in providing updated infor-
mation on seabird numbers and distribution through-
out the migratory bird sanctuaries on the North Shore of
the Gulf of St. Lawrence (Figure 1), another major ap-
plication of the results of this traditional survey is in
identifying trends. Follow-up censuses have been car-
ried out fairly regularly since the first census in 1925
(Lewis 1925, 1931, 1937, 1942; Hewitt 1950; Tener
1951; Lemieux 1956; Moisan 1962; Moisan and Fyfe
1967; Nettleship and Lock 1973; Chapdelaine 1980,
1995; Chapdelaine and Brousseau 1984, 1991), provid-
ing the trends over a period of approximately 75 years,
including the present survey. This survey also provides
one of the ways we monitor the broader marine envi-
ronment. In effect, these wide-ranging birds are acting
as our sampling agents. As human impact on the seas
increases, whether directly by exploitation of resources
or marine pollution, or less directly by factors such as
global warming, early indications of changes are vital.
Clearly any changes in the size of seabird breeding col-
onies are of major importance to conservationists to ori-
ent any concrete action to be taken or to seabird biol-
ogists to learn more about the regulation of seabird
numbers and the wide range of factors known to influ-
ence the birds.
This article presents the current status of the 15 ma-
rine bird species breeding in the sanctuaries in 1998-
1999, and compares them with those of the 1993 census.
Scientific names are given in Table 1.
Methods
The census of seabirds in the sanctuaries of the North
Shore of the Gulf of St. Lawrence was conducted over
two years. All of the technical details of this census
(methods, estimates calculations, mapping of the col-
onies, weather conditions) are discussed in Rail and
Chapdelaine (2002) and summarized below for each
family of birds.
GaviiDs — We counted all Red-throated Loon nests by
systematically walking around the ponds on the islands
of each sanctuary. In a few exceptional cases we noted
the presence of adults instead of landing on the island.
HyDROBATIDS — We conducted a systematic count of
active burrows. A burrow was considered active if we
were able to reach an adult inside, or detect signs of
recent occupation (soil freshly excavated or oily odour
characteristic of petrels at the entrance of the burrow).
ANATIDS — On Corossol Island, we used a system
of quadrats from which we extrapolated and average
density (nests/ha) for the entire area deemed suitable
256
RAIL and CHAPDELAINE: CENSUS OF SEABIRD POPULATIONS
_/Me du Corossol —~Betchouane
Gaspé Peninsula
NEW BRUNSWICK
ic Seaiiwiune Soran ogg “Gu, GF
Watshishou
lle a la Brume
Gulf of St. Lawrence f~ = 4
LABRADOR 57°00' W
52°00' N
QUEBEC
yew Baie de Brador
“ Saint-Augustin
} ib Gros Mécatina
\
t
‘i Ce ony 2 oe lles Sainte-Mari
) logging es Sainte-Marie,
lles aux Perroquets
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NEWFOUNDLAND
ee
FiGurE |. Location of the sanctuaries of the North Shore of the Gulf of St. Lawrence.
for Common Eiders (Chapdelaine 1978*). In the Bet-
chouane Bird Sanctuary, we conducted a systematic
nest count on Calculot Island, and (as in preceding
censuses) used a system of line-transects of varying
length on Innu Island (see Caughley 1977). In sanc-
tuaries featuring many islands (e.g., Watshishou, ile a
la Brume, Baie des Loups), we counted all the nests
on at least 27% of the land area and extrapolated an
average density over the entire area of all the islands.
On the Iles aux Perroquets and [les Sainte-Marie sanc-
tuaries, extrapolation was done after systematic counts
were made on most large islands, covering 57% and
98% of total land area, respectively (but see Rail and
Chapdelaine 2002 for details).
PHALACROCORACIDS — Systematic counts of all Great
and Double-crested Cormorant nests were carried out.
At the Corossol Island colony, Double-crested Cormo-
rant nests in treetops were counted from an elevated
lookout point.
Larips — In the large Herring Gull colony of Coros-
sol Island, we sampled sub-colonies where the number
of nests (Np) and the number of adults (Ni) were
determined. Then, using the factor k (k=Np/Ni), we
estimated the number of pairs in sectors where we
counted only the number of adults present. In the
Betchouane Sanctuary, all gull nests were counted sys-
tematically, and were attributed to Herring and Great
Black-backed gulls according to the observed propor-
tions of adults of both species. In the other sanctu-
aries all larids were censused with a combination of
est counts and adult counts. Proportions of Arctic and
Common terns in mixed tern colonies were not always
determined, so the results for the two species are com-
bined in Table 1. All Black-legged Kittiwake nests
attended by adults were counted.
ALCIDS — We carried out systematic counts of eggs
and active burrows in colonies of Atlantic Puffins,
Razorbills and Common Murres that could be accessed
with minimal disturbance. Elsewhere we counted indi-
viduals at the colony and on adjacent waters from a
distance. All colonies with large numbers of Common
Murres were carefully avoided because of their sensi-
tivity to disturbance. In particular, at the Iles Sainte-
Marie Sanctuary, where 87% of breeding Common
Murres on the North Shore are found, 98% of the
population estimate for the Common Murre results
from adult counts. For Atlantic Puffins nesting on the
Blacklands Island in the Baie des Loups Sanctuary, we
used the factor k method described above for larids.
On Ile aux Perroquets in the Baie de Brador Sanctuary,
we used evenly spaced grids and line transects to de-
limit the area of both the puffin and Razorbill colonies,
evaluate mean nest densities, and then extrapolated
the populations (see Nettleship 1973* ; Chapdelaine
1978*). The Black Guillemot population was estimated
from adult bird counts around the islands, although
exceptionally we recorded a pair when a nest was
found with no adult in sight.
Vol. 118
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2004 RaiL and CHAPDELAINE: CENSUS OF SEABIRD POPULATIONS 259
TABLE 2. Changes in the numbers of seabirds in sanctuaries on the North Shore of the Gulf of St Lawrence, Québec, 1988 to
1998-1999.
Years of survey Compound annual growth*
rate by period
Species 1988 1993 1998-1999 1988-1993 1993-1998**
Red-throated Loon 76 66 80 -2.82% 3.21%
Leach’s Storm-Petrel 1744 1840 718 1.07% -18.78%
Great Cormorant 86 78 340 -1.95% 24.54%
Double-crested Cormorant 4558 3472 2830 -5.44% -3.49%
Common Eider 8536 14548 13072 10.66% -2.10%
Ring-billed Gull 288 104 484 -20.37% 31.04%
Herring Gull 16195 4879 4929 -24.00% 0.49%
Great Black-backed Gull 1883 2284 2381 3.86% 1.15%
Black-legged Kittiwake 8536 6294 3816 -6.09% -10.02%
Caspian Tern 15 0 0 -100.00% -
Common and Arctic Terns 1350 545 294 -18.14% -12.03%
Common Murre 26049 30829 30111 S370 -0.39%
Razorbill 7036 8389 13953 35200 8.58%
Black Guillemot 521 411 651 -4.74% 8.70 %
Atlantic Puffin 35142 46684 29030 5.68% -7.92%
log. N (t) - log. N (0)
so — 100%
t
** Populations in sanctuaries censused in 1999 were back-calculated to 1998 to get the compound annual growth rate for
all North Shore sanctuaries after 5 years
Results
In the eight sanctuaries censused in 1993 and 1998-
1999 (Gros Mecatina excluded), the total number of
birds had decreased by 15% or 17 734 individuals (see
Table 1 for details). This is mostly due to the dra-
matic 38% decline of the Atlantic Puffin (-17 654 indi-
viduals), which was by far the most abundant seabird
in the North Shore sanctuaries in 1993 (but was out-
numbered by the Common Murre in 1999). Leach’s
Storm-Petrels, Black-legged Kittiwakes and Common
and Arctic Terns also declined at a very rapid rate
between 1993 and 1998-1999 (Table 2). Double-crested
Cormorants numbers also diminished. The Razorbill is
the only abundant species showing a large increase,
with the 1998-1999 population estimate exceeding by
5564 individuals the result of 1993 (+66%). This species
has made a spectacular comeback since 1972, when less
than 3000 individuals were recorded in the sanctuaries
(compared to 14 341 in 1998-1999). The small popula-
tions of Great Cormorants, Ring-billed Gulls and Black
Guillemots also grew rapidly between 1993 and 1998-
1999, as did Red-throated Loons but more slowly. In
four species, numbers appeared rather stabilized, the
Common Eider and Herring Gull after having showed
very sharp trends between 1988 and 1993 (annual
growth rates of +11% and -24%, respectively), the
Great Black-backed Gull and Common Murre follow-
ing less striking but significant rises (annual growth
rate of +3.9 and +3.4%, respectively). Finally, no Cas-
pian Terns were found for the second quinquennial
census in a row.
We visited the Corossol Island Sanctuary on 30 and
31 May 1998. Major increases in large gulls (Herring
and Great Black-backed gulls) were noted. Populations
of alcids also expanded, and in particular the number
of Black Guillemots more than doubled compared to
1993. Puffins were recorded for the first time during
quinquennial censuses, bringing up to 10 the number
of seabird species breeding there. The Common Eider
was also more abundant. On the other hand, the colony
of Leach’s Storm-Petrels was reduced to less than half
between 1993 and 1998, and Black-legged Kittiwakes
also declined quite rapidly. Double-crested Cormorants
were down 25%, and colony localization had seemed
to change a bit, possibly prompted by forest decay
caused by their long-term occupation (nests are in tree-
tops of conifers) in some areas.
On 2 and 3 June 1998, we visited the Betchouane
Bird Sanctuary. The most important change in the sea-
bird community was the 36% decrease in Common
Eider, by far the most abundant bird there. The Razor-
bill apparently continued its spectacular comeback,
with a 72% population increase between 1993 and
1998. Herring Gulls, Great Black-backed Gulls, Black-
legged Kittiwakes and Atlantic Puffins were almost
stable or slightly increasing.
260
After a tremendous population explosion following
1982, the population growth of the Common Eider in
Watshishou appeared to have slowed down consid-
erably between 1993 and 1998. The Black Guillemot
population increased threefold during the same period.
Double-crested Cormorant and Great Black-backed
Gull numbers showed opposite trends; the former spe-
cies underwent a 50% increase whereas the latter was
reduced by half. Herring Gull population size appeared
slightly reduced compared to 1993, but the 1998 result
was by far the highest for the species in Watshishou,
except for 1993. The 1998 survey confirmed a cata-
strophic (-96%) and inexplicable decline of terns in
Watshishou since 1988. In the past, this sanctuary, con-
sisting of more than 200 islands, always had a fair
number of terns (range 128 — 1490 individuals), and
was the most important sanctuary on the North Shore
in that regard. In 1998, however, despite better cover-
age (more islands were visited than in previous cen-
suses), we found only 19 breeding pairs distributed
in 5 very small colonies. The Watshishou Bird Sanc-
tuary was visited on 6, 7 and 8 June 1998.
The following year (in 1999), seabirds were cen-
sused on 14 June at the Ile 4 la Brume Sanctuary. The
Common Eider had decreased slightly since 1993,
but was still relatively abundant. Population trends
were up for Herring and Ring-billed gulls; however
numbers of these two species are rather small and
tended to vary a lot in the past. The number of Great
Black-backed Gulls dropped further between 1993
and 1999, reaching its lowest level ever in 1999. Terns
declined sharply during the same period, and in fact
since 1988 their population trends at the Ile a la Brume
(-84%) and Watshishou sanctuaries are similar. Status
of the very small populations of Red-throated Loon
and Razorbill are still precarious, as their numbers
remained stable between 1993 and 1999 at two and
eight individuals, respectively. Finally, no Caspian
Terns were found for the second quinquennial census
in a row at Ile a la Brume, the only traditional breed-
ing site for this species in the Province of Québec.
We visited the Baie des Loups Bird Sanctuary on
18 June. The most abundant bird there, the Atlantic
Puffin, had declined by 40% since 1993. The Great
Black-backed Gull population also decreased notice-
ably (36%). Breeding Leach’s Storm-Petrels apparent-
ly deserted the sanctuary, which leaves the Corossol
Island Sanctuary as the only active breeding site of that
species on the North Shore, and maybe in the whole
province. On the brighter side, the Common Eider pop-
ulation increased by 50%. Also, the Common Murre
and the Razorbill, once abundant in the sanctuary but
which had declined steadily up to the very low and
worrying levels observed in 1993, bounced back and
increased threefold between 1993 and 1999. Red-
throated Loon, Herring Gull, terns, and Black Guille-
mot numbers remained fairly stable.
THE CANADIAN FIELD-NATURALIST
Vol. 118
The Iles aux Perroquets Bird Sanctuary was visited
on 11 and 21 June 1999. The population of Atlantic
Puffin showed a similar drop (-53%) as in the other
large colonies on the North Shore. In contrast to the
general upward trend observed in these species at the
other sanctuaries, a decrease in Common Murres and
Razorbills was noted at the Iles aux Perroquets Bird
Sanctuary in 1999. The number of Common Eiders
declined only slightly. Except for the Black-legged
Kittiwakes whose population collapsed (-82%) between
1993 and 1999, numbers of larids were quite stable.
With only 11 nests found in 1999, the kittiwake may
well disappear as a breeding species at the Iles aux
Perroquets in the future. On the positive side, the two
smallest seabird populations breeding in the sanctuary
in 1993, those of the Red-throated Loon and Black
Guillemot, both showed large increases (140% and
164%, respectively). Also worthy of notice is the addi-
tion of the Great Cormorant as a breeding species in
the sanctuary.
The Iles Sainte-Marie Bird Sanctuary (visited on
10, 11, 13, 17 and 19 June) was again found to have
the highest seabird diversity (12 breeding species)
and abundance (total of 39 316 individuals). Common
Murres represented two-thirds of the seabird popula-
tion with an estimated 26 156 breeding birds. The
number of murres appeared quite stable between 1993
and 1999, after the spectacular and steady recovery
of the species following 1972 (when only 4120 birds
were counted). Razorbills show the same long-term
trend as murres, but were still going up in 1999 (116%
rise compared to 1993). The Great Cormorant colony
expanded unexpectedly (+318%) to become the largest
of this species on the North Shore. Increases were noted
in Black-legged Kittiwakes, Black Guillemots and terns
as well. Numbers of Double-crested Cormorants, Com-
mon Eiders, and Atlantic Puffins were reduced rough-
ly by half. Herring Gulls were again found to be declin-
ing very sharply, whereas Great Black-backed Gulls
showed a moderate decrease. Finally, the number of
Red-throated Loons in 1999 was only one pair short of
the highest counts which were recorded on the two pre-
ceding censuses.
A little farther to the east, a few small offshore
islands constitute the Gros Mécatina Bird Sanctuary,
which was created in 1996. On 23 June 1999, the sanc-
tuary was included for the first time in a quinquennial
census. Species diversity was impressive for such a
small sanctuary, as nine seabird species were found
breeding. Numbers of each species were low though,
and the most abundant species was the Razorbill with
388 birds observed. According to naturalists such as
Coues (1862), these islands were once inhabited by tens
of thousands of Common Murres, so the sanctuary has
definite potential for seabird conservation if it is well
protected.
2004
The Baie de Brador Bird Sanctuary is well-known
for its colonies of Atlantic Puffin and Razorbill. On 28
and 29 June 1999 however, we were quite surprised
to discover the addition of Black-legged Kittiwakes
and terns breeding there for the first time, as well as
Common Murres which had not bred there since
1965. Herring Gulls and Great Black-backed Gulls
seemed well established as breeders for the second
census in a row (they were present in very small num-
bers or absent prior to 1993). Also, as in most other
sanctuaries, Razorbill numbers grew very fast between
1993 and 1999 (+175%). Nevertheless, all these results
were darkened by the finding that Atlantic Puffins had
declined by a third since 1993, when the population
seemed on its way to get back to historic levels.
Because it has always been the stronghold of puffins
in our province, the Baie de Brador Bird Sanctuary
plays a leading role in the conservation of the species
in Québec.
Discussion
Total number of seabirds recorded in 1998-1999 in
the North Shore Bird Sanctuaries dropped 15% (or
17 734 birds, Gros Mécatina excluded). But most of
this decrease could be attributed to the Atlantic Puffin
whose 38% decline represent a loss of 17551 birds.
Population trends in other species were variable, as
four species increased rapidly, four species decreased
at a fast rate, and the others showed more stable or
moderate trends. Numbers of Razorbills and Black
Guillemots increased at a very rapid rate in almost
every sanctuary (where they are present). The only Great
Cormorant colony recorded during the 1993 census was
found at the [les Sainte-Marie Bird Sanctuary; by
1999, that colony had grown so much that immigration
must be partly involved. Also, three new colonies of
this species were found elsewhere in the sanctuaries
in 1999. The Ring-billed Gull is the last seabird species
which increased at a very fast rate since 1993. How-
ever, this species is poorly represented in the North
Shore Bird Sanctuaries, where their numbers always
fluctuated widely in the past. Instead of suggesting a
real population trend, our results may rather reflect
colony displacements as the species exhibits poor site
fidelity on the North Shore.
The Atlantic Puffin was not the only species show-
ing a sharp decline between the last two censuses of
the North Shore sanctuaries. The case of the Leach’s
Storm-Petrel is equally worrying; the species was found
breeding in four sanctuaries in 1988, but in 1998-
1999 only the Corossol Island colony was still active,
and its number of nests was reduced to less than half
compared to 1993. Moreover, this may be the only
Leach’s Storm-Petrel colony left in the whole province.
Thus the status of the species appears precarious in
Québec. The Black-legged Kittiwake was found breed-
ing in six sanctuaries in 1998-1999, whereas in the past
it had been breeding in no more than four sanctuaries.
RAIL and CHAPDELAINE: CENSUS OF SEABIRD POPULATIONS
261
However, over 90% of the kittiwakes in the sanctu-
aries are concentrated at the Corossol Island colony,
where a 39% drop was observed between 1993 and
1998. In fact the colony decreased by 55% since 1988
and the trend was even faster in the last five years.
Observations made on diet and breeding success of
larids at Corossol Island in 1996-1998 showed that
kittiwake breeding success was severely affected by
Herring Gull predation on large chicks, especially when
capelin appeared less available. The poor kittiwake
productivity measured in 1997-1998 (0.60 and 0.27
young fledged per pair, respectively) means that re-
cruitment is likely not enough to compensate for nat-
ural mortality, so that further decline of the colony is
expected. Terns, after the fashion of Ring-billed Gulls,
are poorly represented in the sanctuaries and their
population trends partly reflect the unpredictability
of their breeding activities. However, their numbers
dropped severely for a second quinquennial census in
a row, resulting in a 80% decline since 1988. The case
of the Watshishou Bird Sanctuary, which has always
been the most important for terns, is particularly intrigu-
ing as that tern population reached an unprecedented
low level in 1998.
Among species with near-stable population trends
between 1993 and 1998-1999 are the Common Eider
and the Common Murre, two species whose numbers
finally appeared to level off after spectacular increases
were noted in each of the four preceding censuses.
Herring Gull population trends on the North Shore
(and especially at Corossol Island) have been corre-
lated with cod fishery, an industry that provided signif-
icant amounts of fish offal available to gulls (Chap-
delaine and Rail 1997). After a boom in the early 1980s,
cod fishery and Herring Gull populations collapsed
concurrently in the late 1980s-early 1990s. But in 1998-
1999 it seemed that after a drastic (-78%) decline be-
tween 1988 and 1993, the Herring Gull population was
stabilized, perhaps to a more “natural” level. The num-
ber of Red-throated Loons increased only slightly be-
tween the last two surveys, yet the 1998-1999 total
(82 individuals) is the highest ever recorded in the
sanctuaries. The Double-crested Cormorant population
declined but only at a slow rate after 1993, and in 1998-
1999 the total population estimate for the sanctuaries
was still the third highest since 1925. The steady rise
of Great Black-backed Gull numbers continued to slow
down to be nearly stable between 1993 and 1998. Final-
ly, the Caspian Tern did not breed in 1993 and 1999 at
the fle 4 la Brume Sanctuary, where it consistently nest-
ed between 1925 and 1988. The more time passes by,
the more unlikely this species will be back, unless
appropriate measures are taken to prevent disturbance
of the only breeding site of Caspian Terns in Québec.
While some population trends varied regionally,
others suggest large-scale factors are involved. In
particular, Black-legged Kittiwake and Herring Gull
declines since the end of the 1980s are reported not only
262
in North Shore sanctuaries, but also at all large colo-
nies around the Gaspé Peninsula and at the Magdalen
Islands (Chapdelaine et al. 2003*). Atlantic Puffin num-
bers dropped at all major North Shore concentrations
between 1993 and 1999. On the other hand, Razorbill
colonies continued to expand everywhere in the Gulf
and in the Estuary (Chapdelaine et al. 2001), and the
small populations of Great Cormorant on the North
Shore and around the Gaspé Peninsula grew signifi-
cantly since 1988-1990. So far we have presented some
evidence that the Herring Gull population had been
influenced by cod fishery activities (Chapdelaine and
Rail 1997), and that an abundance of small fish such
as sandlance (Ammodytes sp.) and Capelin (Mallotus
villosus) had a positive effect on alcid breeding per-
formance and populations (Chapdelaine and Brousseau
1991, 1996; Rail et al. 1996). But most population
trends are left unexplained.
The fact that law enforcement efforts have not been
distributed uniformly across sanctuaries probably ex-
plains why, in sanctuaries such as Ile a la Brume and
Baie des Loups, many seabird populations are at low
levels and signs of disturbance are omnipresent. Con-
versely, the well-patrolled [es Sainte-Marie Bird
Sanctuary appears in good shape. Seabird conservation
in North Shore bird sanctuaries face many challenges:
ecotourism, disturbance, poaching, episodic fox inva-
sion in the sanctuaries, seabird bycatch in nearby fish-
ing nets, along with ecological factors at all scales. This
stresses the need to maintain and improve law enforce-
ment and public educational programs, and highlights
the importance of research to tackle the factors respon-
sible for the observed seabird population trends.
Acknowledgments
Many thanks to all those who contributed to this.
Fieldwork was carried out with the help of our col-
leagues Pierre Brousseau and Jocelyn Thibault, Gilles
Falardeau with his assistants Linda Burr and Daniel
Daigneault, and Canadian Wildlife Service wardens
Freddy Strickland and Wilson Evans. Members of Parks
Canada in Mingan and assisting volunteers also gave
us a big hand, as well as Andrew Rowsell from Fish-
eries and Oceans Canada in Blanc-Sablon. Finally,
our special thaughts go to M. Gallienne and his family
for their hospitality on Corossol Island.
Documents Cited (marked * in text)
Chapdelaine, G. 1978. Onziéme inventaire des oiseaux colo-
niaux des refuges de la c6te nord du Golfe Saint-Laurent
et révision globale de la fluctuation des populations depuis
1925 jusqu’a 1977. Service canadien de la faune, région
du Québec, Environnement Canada, Sainte-Foy, 166 pages.
Chapdelaine, G., P. Brousseau, and J.-F. Rail. 2003.
Banque informatisée des oiseaux marins du Québec
(BIOMQ). Database. Last update 12 March 2003. Environ-
ment Canada, Canadian Wildlife Service, Québec Region.
Nettleship, D. N. 1973. Census of seabirds in the sanctuaries
of the North Shore of the Gulf of St. Lawrence, summer
THE CANADIAN FIELD-NATURALIST
Vol. 118
1972. Studies on northern seabirds No 20. Canadian Wild-
life Service Report, Ottawa, 160 pages.
Literature Cited
Caughley, G. 1977. Analysis of vertebrate populations. John
Wiley and Sons, London.
Chapdelaine, G. 1980. Onziéme inventaire et analyse des
fluctuations des populations d’oiseaux marins dans les
refuges de la Cote Nord du Golfe Saint-Laurent. Cana-
dian Field-Naturalist 94: 34-42.
Chapdelaine, G. 1995. Fourteenth census of seabird popu-
lations in the sanctuaries of the North Shore of the Gulf
of St. Lawrence, 1993. Canadian Field-Naturalist 109:
220-226.
Chapdelaine, G., and P. Brousseau. 1984. Douzieme inven-
taire des populations d’ oiseaux marins dans les refuges de
la Cote-Nord du golfe du Saint-Laurent. Canadian Field-
Naturalist 98: 178-183.
Chapdelaine, G., and P. Brousseau. 1991. Thirteenth cen-
sus of seabird populations in the sanctuaries of the North
Shore of the Gulf St. Lawrence, 1982-1988. Canadian
Field-Naturalist 105: 60-66.
Chapdelaine, G., and P. Brousseau. 1996. Diet of Razor-
bill Alca torda chicks and breeding success in the St.
Mary’s Islands, Gulf of St. Lawrence, Québec, Canada,
1990-1992. Pages 27-37 in Studies of high-latitude sea-
birds. 4. Trophic relationships and energetics of endotherms
in cold ocean systems. Edited by W. A. Montevecchi.
Canadian Wildlife Service Occasional Paper 91. Ottawa.
Chapdelaine, G., A. W. Diamond, R. Elliot, and G. J.
Robertson. 2001. Status and population trends of the
Razorbill in eastern North America. Canadian Wildlife
Service Occasional Paper 105. Ottawa.
Chapdelaine, G., and J.-F. Rail. 1997. Relationship between
cod fishery activities and the population of herring gulls
on the North Shore of the Gulf of St Lawrence, Québec,
Canada. ICES Journal of Marine Science 54: 708-713.
Coues, E. 1862. Notes on the ornithology of Labrador. Pro-
ceedings of the Academy of Natural Sciences of Phila-
delphia (1861): 215-257.
Hewitt, O. H. 1950. Fifth census of non-passerine birds in
the bird sanctuaries of the North Shore of the Gulf of St.
Lawrence. Canadian Field-Naturalist 64: 73-76.
Lemieux, L. 1956. Seventh census of nonpasserine birds in
the bird sanctuaries of the North Shore of the Gulf of St.
Lawrence. Canadian Field-Naturalist 70: 183-185.
Lewis, H. F. 1925. The new bird sanctuaries in the Gulf of
St. Lawrence. Canadian Field-Naturalist 39: 177-179.
Lewis, H. F. 1931. Five years’ progress in the bird sanctu-
aries of the North Shore of the Gulf of St. Lawrence.
Canadian Field-Naturalist 45: 73-78.
Lewis, H. F. 1937. A decade of progress in the bird sanctu-
aries of the North Shore of the Gulf of St. Lawrence. Can-
adian Field-Naturalist 51: 51-55.
Lewis, H. F. 1942. Fourth census of non-passerine birds in
the bird sanctuaries of the North Shore of the Gulf of St.
Lawrence. Canadian Field-Naturalist 56: 5-8.
Moisan, G. 1962. Eighth census of non-passerine birds in
the bird sanctuaries of the North Shore of the Gulf of St.
Lawrence. Canadian Field-Naturalist 76: 78-82.
Moisan, G., and R. W. Fyfe. 1967. Ninth census of non-
passerine birds in the sanctuaries of the North Shore of
the Gulf of St. Lawrence. Canadian-Field-Naturalist 81:
67-70.
2004
Nettleship, D. N., and A. R. Lock. 1973. Tenth census of
seabirds in the sanctuaries of the North Shore of the Gulf
of St. Lawrence. Canadian Field-Naturalist 87: 395-402.
Rail, J.-F, and G. Chapdelaine. 2002. Quinziéme inven-
taire des oiseaux marins dans les refuges de la Cote-Nord :
techniques et résultats détaillés. Série de rapports tech-
niques No. 392. Service canadien de la faune, région du
Québec, Environnement Canada, Sainte-Foy, xvi + 307
pages.
Rail, J.-F., G. Chapdelaine, P. Brousseau, and J.-P. L.
Savard. 1996. Utilisation des oiseaux marins comme bio-
RAIL and CHAPDELAINE: CENSUS OF SEABIRD POPULATIONS
263
indicateurs de l’écosystéme du Saint-Laurent. Série de rap-
ports techniques No. 254. Service canadien de la faune,
région du Québec, Environnement Canada, Sainte-Foy, ii
+ 113 pages.
Tener, J. S. 1951. Sixth census of non-passerine birds in the
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Received 16 June 2003
Accepted 5 July 2004
Notes
Observations of Above-Surface Littoral Foraging in Two Sea Ducks,
Barrow’s Goldeneye, Bucephala islandica, and Surf Scoter, Melanitta
perspicillata, in Coastal Southwestern British Columbia
DEBORAH L. LACROIX!, KENNETH G. WRIGHT?, and DANIEL KENT?
'Centre for Wildlife Ecology, Simon Fraser University, Burnaby, British Columbia VSA 1S6 Canada
26090 Blink Bonnie Road, West Vancouver, British Columbia V7W 1V8 Canada
>Vancouver Aquarium Marine Science Centre, Vancouver, British Columbia V6B 3X8 Canada
Lacroix, Deborah L., Kenneth G. Wright, and Daniel Kent. 2004. Observation of above-surface littoral foraging in two sea
ducks, Barrow’s Goldeneye, Bucephala islandica, and Surf Scoter, Melanitta perspicillata, in coastal southwestern
British Columbia. Canadian Field-Naturalist 118(2): 264-265.
Barrow’s Goldeneyes (Bucephala islandica) and Surf Scoters (Melanitta perspicillata) were observed on four separate occa-
sions, by three different observers, foraging on Bay Mussels (Mytilus trossulus) above the water surface. This unique foraging
behaviour could be attributed to diurnal spring tides and reduced lower intertidal mussel abundance.
Key Words: Barrow’s Goldeneye, Bucephala islandica, Surf Scoter, Melanitta perspicillata, foraging behaviour, sea ducks,
Bay Mussels, Mytilus trossulus, British Columbia.
The sea ducks, Barrow’s Goldeneye (Bucephala
islandica) and Surf Scoter (Melanitta perspicillata),
winter in abundance along the coast of British Colum-
bia where they forage diurnally on marine inverte-
brates in bays, harbours, beaches, and inlets (Bellrose
1980; Vermeer 1981, 1982; Vermeer and Bourne 1984;
Campbell et al. 1990; Savard et al. 1998; Eadie et al.
2000). In rocky habitats, both sea ducks forage pre-
dominantly on Bay Mussels (Mytilus trossulus) (for-
merly classified as M. edulis; McDonald and Koehn
1988, McDonald et al. 1991) (Vermeer and Levings
1977; Hirsch 1980; Vermeer 1981, 1982; Vermeer and
Bourne 1984; Lacroix 2001). Both sea ducks dive to
locate and retrieve mussels. Mussels are pried from the
substrate and swallowed whole (Savard et al. 1998;
Eadie et al. 2000).
Three observers, on four separate occasions, ob-
served Surf Scoters and/or Barrow’s Goldeneyes for-
aging on Bay Mussels above the water surface in coastal
southwestern British Columbia. The first observation,
on 22 February 1999, involved juvenile male and fe-
male Surf Scoters and Barrow’s Goldeneyes eating
exposed mussels at a breakwater on Popham Island.
The event was photo-documented by D. Kent. On the
second occasion, on 7 March 1999, 1 juvenile male and
7 females, mostly juveniles, Barrow’s Goldeneyes and
3 Surf Scoters, (1 female and 2 immature males), re-
moved mussels from a rocky point at Cape Roger
Curtis, while they sat on a reef, 1.5 m above the water
line. Later that day a flock of approximately 12 Bar-
row’s Goldeneyes, mostly juveniles, was seen feeding on
mussels while hauled out on a reef on Hermit Island.
This above-surface foraging tactic was also noticed
later in March when three juvenile Surf Scoters, and
six Barrow’s Goldeneyes, mostly juveniles, fed on ex-
posed mussels on large boulders. All the observations
coincided with low diurnal tides. The tide height ranged
between 1.74 to 2.16 m, above Chart Datum (a.c.d.).
We are unaware of any previously published or unpub-
lished accounts of this foraging behaviour. Our multiple
observations suggest that the behaviour occurs frequent-
ly but has gone unreported.
All of these observations were made during late
February and March in Howe Sound and Burrard
Inlet, British Columbia, located in the same geograph-
ic vicinity (49°19.32’N, 123°09.92’W — 49°21.60’N,
123°29.15’W). These observations share several sim-
ilar characteristics including: (1) all ducks were feed-
ing on Bay Mussels; (2) the observations were made
during low diurnal tides; (3) only small groups, often
consisting of mixed-species flocks, were exhibiting this
foraging behaviour, and (4) these foraging groups
consisted mostly of juveniles.
Discussion
Bay Mussels are a dominant species in protected
coastal rocky intertidal areas (Seed and Suchanek
1992: Ricketts et al. 1995). In our observation area,
the vertical distribution of the Bay Mussel ranges from
1.5 to 3.7 m, a.c.d. (Quayle 1978). Although Bay Mus-
sels are intertidal, mussel beds are rarely completely
exposed during daylight hours in winter as the lowest
low tides of the semidiurnal tidal regime occur at night
(Thomson 1981). As winter advances into spring, the
lowest low tides are diurnal; therefore expose mussel
beds during daylight hours (Figure 1). Exposed mussels
264
2004
FIGURE |
Percent of daylight hours
fully submerged
Oct Nov Dec Jan Feb Mar Apr May
Time
Ficure |. The percent of daylight hours that Bay Mussel beds
are completely submerged in coastal British Columbia.
Mussel submergence time was estimated by calculat-
ing the number of hours the tide was above 3.7 m,
a.c.d, using Canadian tide charts (1999), during day-
light hours, between sunrise and sunset.
may be more vulnerable to diving ducks such as Surf
Scoter and Barrow’s Goldeneye as the ducks do not
need to expend energy diving to reach the mussels.
However, Smeathers and Vincent (1979) found that
mussels exposed to air have twice the tensile strength
of those submerged. If the exposed mussels have un-
dergone some degree of desiccation, they may require
more energy to remove than submerged ones, and
may therefore, not be as profitable as first postulated.
Alternatively, juvenile and sub-adult Surf Scoters and
Barrow’s Goldeneyes may be forced to feed on exposed
mussels owing to the reduced mussel abundance and
distribution from over-winter predation. The lower por-
tion of the distribution of Bay Mussels is determined
by biological factors, primarily predation from the
Ochre Sea Star (Pisaster ochraceus) (Seed and Sucha-
nek 1992; Quayle 1978) and sea ducks (Lacroix 2001).
Through the winter, the combination of sea star and sea
duck predation may eliminate the lower distribution
of mussels, hence reducing their overall abundance.
It is therefore plausible that the ducks observed were
forced to forage on the less profitable prey (1.e., the ex-
posed mussels) because there are few or no submerged
mussels in the lower portion of their distribution.
Acknowledgments
We thank R. W. Butler and A. J. Erskine for making
valuable suggestions to the manuscript. D. L. Lacroix
received funding from a postgraduate NSERC schol-
arship and from the Canadian Wildlife Service Geor-
gia Basin Initiative.
Literature Cited
Bellrose, F. C. 1980. Ducks, geese and swans of North Amer-
ica. Stackpole Books, Harrisburg, Pennsylvania. 540 pages.
Campbell, R. W., N. K. Dawe, I. McTaggart-Cowan, J.
M. Cooper, and G. W. Kaiser. 1990. The birds of British
NOTES
265
Columbia. Volume |. Nonpasserines, introduction and
loons through waterfowl. Royal British Columbia Museum,
Victoria, British Columbia. 513 pages.
Canadian Hydrographic Service, Fisheries and Oceans
Canada. 1999. Canadian tide and current tables. Volume
5. Minister of Fisheries and Oceans Canada. 120 pages.
Eadie, J. M., J.-P. Savard, and M. L. Mallory. 2000.
Barrow’s Goldeneye (Bucephala islandica). Pages 1-32
in The Birds of North America. (548). Edited by A. Poole
and F. Gill. The Academy of Natural Sciences, Philadelphia,
Pennsylvania and the American Ornithologists’ Union,
Washington, D.C.
Hirsch, K. V. 1980. Winter ecology of sea ducks in the inland
marine waters of Washington. M.Sc. thesis, University of
Washington, Seattle, Washington. 92 pages
Lacroix, D. L. 2001. Foraging impacts and patterns of win-
tering surf scoters feeding on bay mussels in coastal Strait
of Georgia, British Columbia. M.Sc. thesis, Simon Fraser
University, Burnaby, British Columbia. 126 pages.
McDonald, J. H., and R. K. Koehn. 1988. The mussels
Mytilus galloprovincialis and M. trossulus on the Pacific
coast of North America. Marine Biology 99: 111-118.
McDonald, J. H., R. Seed, and R. K. Koehn. 1991. Allo-
zymes and morphometric characters of three species of
Mytilus in the Northern and Southern Hemispheres. Marine
Biology 111: 323-333.
Quayle, D. B. 1978. A preliminary report on the possibili-
ties of mussel culture in British Columbia. Fisheries and
Marine Service Technical Report 815. 37 pages.
Ricketts, E. F., J. Calvin, J. W. Hedgpeth, and D. W. Philips.
1995. Between pacific tides. Fifth Edition. Stanford Uni-
versity Press, Stanford, California.
Savard, J-P. L., D. Bordage, and A. Reed. 1998. Surf Scoter
(Melanitta perspicillata). Pages 1-28 in The Birds of North
America. (363) Edited by A. Poole and F. Gill. The Aca-
demy of Natural Sciences, Philadelphia, Pennsylvania and
the American Ornithologists’ Union, Washington, D.C.
Seed, R., and T. H. Suchanek. 1992. Population and com-
munity ecology of Mytilus. Pages 87-157 in The mussel
Mytilus: ecology, physiology, genetics and culture. Edited
by E. Gosling. Developments in Aquaculture and Fisher-
ies Science 25, Elsevier, Amsterdam. 589 pages.
Smeathers, J. B., and J. F. Vincent. 1979. Mechanical prop-
erties of mussel byssus threads. Journal of Molluscan
Studies 45: 219-230.
Thomson, R. E. 1981. Oceanography of the British Columbia
coast. Canadian Special Publication Fisheries and Aquatic
Science 56. 291 pages.
Vermeer, K. 1981. Food and populations of Surf Scoters in
British Columbia. Wildfowl] 32: 107-116.
Vermeer, K. 1982. Food and distribution of three Bucephala
species in British Columbia. Wildfowl 33: 22-30.
Vermeer, K., and N. Bourne. 1984. The White-winged Scoter
diet in British Columbia waters: resource partitioning with
other scoters. Pages 62-73 in Marine birds: their feeding
ecology and commercial fisheries relationships. Edited by
D. N. Nettleship, G. A. Sanger, and P. F. Springer. Pro-
ceedings of the Pacific Seabird Group Symposium, Seattle,
Washington, 1982.
Vermeer, K., and C. D. Levings. 1977. Populations, biomass
and food habits of ducks on the Fraser Delta intertidal
area, British Columbia. Wildfowl 28: 49-60.
Received 23 July 2001
Accepted 6 August 2004
266
THE CANADIAN FIELD-NATURALIST
Vol. 118
New Records of Cyperaceae and Juncaceae from the Yukon Territory
Stuart A. HARRIS! AND PETER W. BALL?
'Department of Geography, University of Calgary, Calgary, Alberta T3A 1E4 Canada
*Department of Botany, Erindale College, University of Toronto in Mississauga, Mississauga, Ontario LSL 1C6 Canada
Harris, Stuart A., and Peter W. Ball. 2004. New records of Cyperaceae and Juncaceae from the Yukon Territory. Canadian
Field-Naturalist 118(2): 269-270.
Two new species of Cyperaceae are reported, viz., Carex hoodii, and Eleocharis elliptica. Also, range extensions for eight
species of Carex, Eriophorum, and Juncus are listed.
Key Words: Vascular plants, Yukon Territory, new records, range extensions.
In the last ten years, considerable advances have
taken place in the knowledge of the vascular flora of
the Yukon Territory (Cody, 1996, 2000; Cody et al.,
1998, 2000, 2001, 2002, 2003). In spite of this, the
flora is still incompletely known, as indicated by the
frequent and substantial additions.
In 1980, the first author commenced detailed field
studies of the distribution of permafrost in the south
and central Yukon Territory, together with the nature
and dynamics of the associated landforms (Harris
1998, 2004; see also Wall et al. 1987). As part of the
work, plants were collected and have been system-
atically identified. For the more difficult groups, the
material was sent to specialists who have helped in
the identification. P.W.B. carried out the task of iden-
tifying the Cyperaceae and some of the Juncaceae.
The result is a substantial collection of sheets that are
in the collection of the first author (UAC #60 000 —
74 000). Comparison of these with the published lists
of species and their distributions indicates that there
are at least two species not previously described for
the Yukon Territory, as well as some range extensions
and name changes of varying importance. This paper
will describe these changes. The nomenclature used
follows that in the recent Flora of North America,
volume 23 (Flora of North America Editorial Com-
mittee 2002).
Species New to the Yukon
CYPERACEAE
Carex Hoodii Boott — YUKON. Hart River road at
1180 m elevation, east of the Dempster Highway at
km 78, about 138°14'W., 64°30'N. (UAC 66735).
It occurs on the wet shrub tundra between the clumps of
Betula glandulosa and Salix spp., and is unlike any of the
other Carex species. This species should be added to the list
of rare plants in the Yukon (Douglas et al. 1981).
Eleocharis elliptica Kunth. — YUKON. Klondike River
bridge, Dempster Highway at 138°44'W., 63°59'N.
(UAC 70230).
This North American species is widespread in Alberta
(Moss 1983, page 158), and should be looked for elsewhere
in the southern Yukon Territory. It is characterised by yellow,
orange or brown achenes with 12-20 vertical ridges. It should
be added to the list of rare plants of the Yukon Territory
(Douglas et al. 1981).
Range Extensions in the Yukon
CYPERACEAE
Carex foenea Willdenow — YUKON. Tagish Camp-
ground, 134°15'W., 60°19'N. (UAC 70310), and Lucky
Lake, east of Watson Lake, 134°30'W., 60°O1'N. (UAC
61656).
It is probably present at scattered localities across the south-
ern Yukon Territory in wet places in Lodgepole Pine forests.
It has previously been found in three localities (Cody, 1994,
page 149: Cody et al. 1998, page 301) including Watson Lake.
Carex glareosa Wahlenburg — YUKON. Minto Landing
in grassy glades at 136°53'W., 62°03'N. (UAC 70268).
Douglas et al. (1981), and Cody (1994, page 440; 1996;
Cody et al. 1998, page 301) have previously reported it from
north of the 69" parallel, but this represents a large extension
of its range southwards by some 7° of latitude.
Carex lapponica O. F. Lang — YUKON. Sheldon Lake,
131°13'W., 61°38'N. (UAC 70271).
Cody et al. (1988, page 301) had earlier collected it in the
extreme southeast of the Territory.
Carex magellanica Lamark ssp. irrigua (Wahlenburg)
Hiitonen — YUKON. Watson Lake at 128°41'W., 60°03'N.
(UAC 73050).
It was previously collected further west and north (Cody,
1996, page 157) and further east (Cody et al. 1998, page 302).
Carex marina Dewey — YUKON. Minto Landing, at
136°53'W., 62°03'N. (UAC 66965), as a rare compo-
nent of the grassy open areas in the boreal forest along
the river bank, close to the steep, grassy, south-facing
slopes of the valley walls.
This is presumably an extension of its limited range in
adjacent south-central Alaska in the rain shadow of the
Wrangel Mountains (Hultén, 1968, page 239). Cody (1996,
page 157) only reported it from Herschel Island, the Lower
Blow River delta (Cody et al. 1998, page 303), and the Mal-
colm River delta.
Carex pachystachya Chamisso ex Steudel — YUKON.
Macmillan Pass between 1097 m and 1250 m at
130°30'W., 63°21'N. and 130°06'W., 63°23'N. (UAC
61619, 61620), Tombstone Mountain Campground,
km 75, Dempster Highway, about 138°14'W., 64°30'N.
(UAC 61615), and Dragon Lake, North Canol Road,
131°20'W., 62°33'N. (UAC 70287).
2004
These sites represent a large range extension from the
south Yukon (Cody 1996, page 162) to the northern limit of
the Boreal Forest. Harris (1998, page 269) previously listed
it as being present at km 161.7, Robert Campbell Highway.
It’s rarity needs to be verified.
JUNCACEAE
Juncus stygius Linnaeus ssp. americanus (Buch.)
Hultn — YUKON. Thermokarst Mounds, South Fork,
Blackstone River, Dempster Highway at 138°22'W.,
64°48'N., July 1987 (UAC 70257).
Cody (1996, page 190) previously reported it from the
Keno Hill area, while Cody et al. (1998, page 305) found it
at Coal River in the southeast Yukon.
Literature Cited
Cody, W. J. 1994. The flora of the Yukon Territory: Additions,
range extensions and comments. Canadian Field-Natural-
ist 108: 428-476.
Cody, W. J. 1996. Flora of the Yukon Territory. NRC
Research Press, Ottawa, Ontario, Canada. 643 pages.
Cody, W. J. 2000. Flora of the Yukon Territory. 2" Edition,
NRC Research Press, Ottawa, Ontario, Canada. 669 pages.
Cody, W. J., C. E. Kennedy, and B. Bennett. 1998. New
records of vascular plants in the Yukon Territory. Canadian
Field-Naturalist 112: 289-328.
Cody, W. J., C. E. Kennedy, and B. Bennett. 2000. New
records of vascular plants in the Territory II. Canadian
Field-Naturalist 114: 417-443.
Cody, W. J., C. E. Kennedy, and B. Bennett. 2001. New
records of vascular plants in the Yukon Territory III.
Canadian Field-Naturalist 115: 301-322.
NOTES
267
Cody, W. J., C. E. Kennedy, B. Bennett, and V. Loewan.
2002. New records of vascular plants in the Yukon Terri-
tory [V. Canadian Field-Naturalist 116: 446-474.
Cody, W. J., C. E. Kennedy, B. Bennett, and J. Staniforth.
2003. New records of vascular plants in the Yukon Terri-
tory [V. Canadian Field-Naturalist 117: 278-301.
Douglas, G. W., G. W. Argus, H. L. Dickson, and D. F.
Brunton. 1981. The rare vascular plants of the Yukon.
Syllogeus #28. National Museums of Canada, Ottawa.
61 pages.
Flora of North America Editorial Commitee. 2002. Flora
of North America 23. Oxford University Press, New York.
608 pages.
Harris, S. A. 1998. Effects of vegetation cover on soil heat
flux in the southern Yukon Territory. Erdkunde 52: 265-285.
Harris, S. A. 2004. Source areas of North Cordilleran en-
demic flora: Evidence from Sheep and Outpost Mountains,
Kluane National Park, Yukon Territory. Erdkunde 58:
62-81.
Hultén, E. 1968. Flora of Alaska and neighbouring Terri-
tories. Stanford University Press, Stanford. 1008 pages.
Moss, E. H. 1983. Flora of Alberta. 24 Edition, revised by
John G. Packer. University of Toronto Press, Toronto. 687
pages.
Wahl, H. E., D. B. Fraser, A. C. Harvey, and J. B. Maxwell.
1987. Climate of Yukon. Climatological Studies #40.
Atmospherric Environment Service, Environment Canada.
323 pages.
Received 21 February 2002
Accepted 21 August 2004
“Ashkui’ Vernal Ice-cover Phenomena and Their Ecological Role in
Southern Labrador
SHAUNA M. BAILLie!, CORINNE D. WILKERSON? and TINA L. NEWBURY?
‘Biology Department, P.O. Box 5000, St. Francis Xavier University, Antigonish, Nova Scotia B2G 2W5; e-mail:: sbaillie@
stfx.ca
* Biology Department, Memorial University of Newfoundland, St. John’s, Newfoundland A1B 3X9; e-mail: r34cdw @mun.ca
3 10 Highland Avenue, Corner Brook, Newfoundland A2H 2Y5; e-mail: tinalnewbury @hotmail.com
Baillie, Shauna M., Corinne D. Wilkerson, and L. Tina Newbury. 2004. “Ashkui’” vernal ice-cover phenomena and their ecological
role in southern Labrador 2002. Canadian Field-Naturalist 118(2): 267-269.
This is the first documented incident of River Otter (Lutra canadensis) feeding on Common Goldeneye (Bucephala clangula)
in a little studied region, southern Labrador. Our observations were made during spring staging when waterfowl aggregate
at open water sites in frozen lakes and rivers, locally known as ashkui. We suggest that otters and raptors opportunistically
forage on staging waterfowl at ashkui.
Key Words: River Otter, Lutra canadensis, Common Goldeneye, Bucephala, clangula, Bald Eagle, Haliaeetus leuco-
cephalus, predator-prey interactions, staging waterfowl, ashkui, Labrador.
Ashkui (singular and plural form) is the Innu name
given to sites of open water in river and lake systems
within the frozen spring landscape of Labrador (Flet-
cher and Breeze 2000*). Migratory waterfowl, includ-
ing Common Goldeneye (Bucephala clangula), use
ashkui as staging areas enroute to their breeding
grounds. These birds arrive in groups of tens to hun-
dreds to rest and rebuild energy reserves by feeding on
invertebrates, fish, seeds and other plant material at
ashkui (Newbury 2002*). Beaver (Castor canadensis),
River Otter (Lutra canadensis) and Muskrat (Ondatra
zibethicus), have been observed at these sites. Osprey
(Pandion haliaetus) and Bald Eagle (Haliaeetus leu-
cocephalus) are known to fish at ashkui (Fletcher and
Breeze 2000*). The temporal existence, number and
distribution of ashkui sites are influenced by a high
268
degree of inter-annual variability in the onset of spring
thaw. As the winter snows disintegrate and waterfowl
await availability of breeding habitat, they may be sus-
ceptible to predation. In 2002, the opening of ashkui
occurred two weeks later than in previous years (un-
published data, Environment Canada, St. John’s, New-
foundland).
Our observations were made during a study exam-
ining the effects of military low level flying on the
behaviour of staging waterfowl at Lac Fourmont in
southern Labrador (52°00'N, 60°15'W; Newbury
2004*). While conducting waterfowl behavioural ob-
servations, we witnessed a River Otter feeding on a
male Common Goldeneye. We also observed a Bald
Eagle attack another goldeneye resting on the ice.
Study Area
Lac Fourmont is situated within the Boreal Forest
Region of eastern Canada and is influenced by con-
tinental climatic regimes (Lopoukhine et al. 1977*).
This region is covered with ice and snow until daily
spring thaw temperatures rise to 5.1°C in May (30 year
average for Goose Bay, Labrador; Environment Canada
Meteorological Service, St. John’s, Newfoundland).
Daytime average temperatures were 4.1°C in May
2002 and ranged from 4.0 to 9.0°C for May during
the years 1993 to 2002. River width at the observa-
tion location was approximately | km, and the ashkui
site was 20 m in breadth. Ice breadth from ashkui to
shoreline was approximately 50 m. Forest stands were
composed of mainly Black Spruce (Picea mariana)
and Balsam Fir (Abies balsamea) interspersed with
approximately 10 % Paper Birch (Betula papyrifera),
Balsam Poplar (Populus balsamifera), and Trembling
Aspen (Populus tremuloides). Lake-edge shrubs con-
sisted of willows (Salix spp.) and alders (Alnus rugosa
and A. crispa). River and bank substrate was composed
of coarse-grained sand and pebbles with exposed boul-
ders and bedrock of gneiss and mafic intrusions. River
basin and landscape were low gradient with shallow
sloping banks, wide flood plain and low relief hills.
We conducted daily observations on waterfowl be-
haviour from blinds using a Swarovski 60x spotting
scope from 9:00 to 12:00 and 13:00 to 16:00 between
26 April and 27 May 2002. Also, we conducted thir-
teen random 1.5 h watches during dawn and dusk.
Observations
Fourteen species of waterfowl occupied the Lac
Fourmont ashkui. Daily waterfowl numbers at the
ashkui ranged from 34 to 376 during this study. A
single River Otter was noted at the ashkui during at
least five observation days. The number of sightings of
mature and immature Bald Eagles, Osprey and Rough-
legged Hawk (Buteo lagopus) totaled 7, 2, 1 and 1,
respectively, over 8 non-consecutive study days.
On 6 May 2002 at 11:35, we observed a River Otter
grasping a male Common Goldeneye on the ice, ap-
THE CANADIAN FIELD-NATURALIST
Vol. 118
proximately 70 m from our observation blind on the
south side of the ashkui. Although the capture was not
observed, the goldeneye was alive and struggling when
the otter was initially observed. The otter sat on its
rear haunches with the goldeneye braced in its fore-
paws and consumed the head of the duck first before
eating the breast muscles and abdominal viscera. After
approximately 10 minutes of feeding, the otter slipped
into the water and swam downstream without the car-
cass remains. We did not observe the fate of the duck
carcass, as it was no longer visible on the ice when
the otter left the feeding site. The bird flock, during
this observation period, comprised mainly 65 Com-
mon Goldeneyes, 27 Black Ducks, 113 Canada Geese
(Branta canadensis).
On 18 May 2002 at 16:03, we observed a Bald
Eagle circle the ashkui and plunge downward toward
a small group of Common Goldeneyes resting and
sleeping on the ice, approximately 150 m from our
position. Upon impact, the eagle initially captured a
goldeneye. The eagle then struggled with the golden-
eye while standing on the ice edge but was unable to
maintain its grasp. The goldeneye fell from the ice to
the water then became inter-mixed with the flock. This
interaction lasted approximately one minute and, we
were unable to identify the attacked goldeneye after
its escape. The eagle then flew to the other side of the
ashkui and rested on the ice. The bird flock, during
this observation, comprised mainly 7 Common Gol-
deneyes, 29 Black Ducks (Anas rubripes), 67 Canada
Geese (Branta canadensis), 11 Greater Scaup (Aythya
marila) and 20 Ring-necked Ducks (Aythya collards).
Discussion
Fish are often the main prey of River Otter and rap-
torial predators (Chubbs and Trimper 1998; Lariviére
and Walton 1998; Fletcher and Breeze 2000*; Heath
et al. 2001; Jedrzejewska et al. 2001). Studies in the
Great Lakes and North American boreal ecosystems
have shown that the diet of River Otter comprises
mostly fish (Lariviere and Walton 1998). However,
otters have been known to feed opportunistically on
small mammals, molluscs, reptiles, birds and fruits
(Lariviére and Walton 1998). In west-central Idaho,
otters supplemented their fish diet with invertebrates
and reptiles (Melquist and Hornocker 1983). In Great
Britain and Ireland, otters consume primarily fish, and
lesser amounts of small mammals, medium-sized mam-
mals, birds, herpetofauna, earthworms, other inverte-
brates and carrion of large mammals (McDonald 2002).
Jedrzejewska et al. (2001) showed that otters special-
ize on prey taken from water. It is plausible that an
otter fishing for fish under water may opportunisti-
cally capture diving goldeneyes. Although River Otters
were known to occasionally feed on birds (Lariviére
and Walton 1998), we believe that this was the first
documented case of an otter feeding on a Common
Goldeneye.
2004
Instances of Bald Eagles preying on duck species
are not rare (Jackman et al. 1999; Heath et al. 2001).
_ Although fish dominate their diet, Bald Eagles have
been reported to modify foraging behaviour and may
forage opportunistically on staging waterfowl in situa-
tions where return on such effort makes them econom-
ical (Brown et al. 1998; Jackman et al. 1999).
The temporal existence, number and distribution of
ashkui, in southern Labrador during spring, may influ-
ence the spatial and temporal distribution of piscivo-
rous predators and migratory waterfowl by limiting
the availability of open-water feeding and resting areas.
Migratory waterfowl arriving from southern destina-
tions must accumulate in greater concentrations when
ashkui openings are limited. Though the behaviour
and distribution of River Otter were not documented
for Labrador, Lariviére and Walton (1998) stated that
otters made heavy use of ashkui in winter and “almost
exclusively” used open water for locomotion and
_ foraging (Madsen and Prang 2001; Ruiz-Olmo et al.
2001). Piscivorous raptors returning to breeding areas
must travel to and congregate at available ashkui to
_ fish. It was likely that spatial and temporal distribution
of ashkui also affected predator-prey interactions.
Our observations are examples of opportunistic for-
aging events on waterfowl by predators that appear to
use ashkui regardless of the presence of waterfowl.
Further investigations in Labrador are needed to under-
stand better the ecological importance of the tem-
poral and spatial distribution of ashkui to mammalian
and raptorial predators.
Acknowledgments
This project was funded in partnership by the In-
stitute for Environmental Monitoring and Research
(IEMR), the Canadian Wildlife Service (CWS), McGill
University and the Department of National Defence
(DND), and by the Northern Scientific Training Pro-
gram. Many thanks to Sean Sharpe (IEMR), Tony
Chubbs (DND) and Roger Titman (McGill University)
for invaluable discussion, advice and/or informal manu-
script review. Jean Sealy (CWS), Scott Gilliland (CWS)
and Dawn Laing (DND) helped us with literature
searches. Thanks to Keith Chaulk (CWS), Bruce Whif-
fen (Environment Canada) and Sarah Hall (CWS) for
providing information on weather and ice conditions.
Documents Cited [marked * in text]
Fletcher, C., and H. Breeze. 2000. Ashkui sites in the low-
level flight training area, Labrador. Report prepared under
NOTES
269
contract to Institute for Environmental Monitoring and
Research (1.E.M.R.). Gorsebrook Research Institute for
Atlantic Canada Studies, Saint Mary’s University, Halifax,
Nova Scotia. 22 pages.
Lopoukhine, N., N. A. Prout, and H. E. Hirvonen. 1977.
The ecological land classification of Labrador. Ecologi-
cal Land Classification Series, Number 4. Fisheries and
Environment Canada. Halifax, Nova Scotia.
Newbury, Tina L. 2002. Effect of low-level flights on the
behaviour of spring staging waterfowl in Central Labrador.
M.Sc. thesis Proposal. McGill University. Ste. Anne-de-
Bellevue, Quebec, Canada.
Newbury, Tina L. 2004. Effect of low-level military jet over-
flights on the behaviour of spring-staging waterfowl at Lac
Fourmont ashkui, Labrador, Canada. M.Sc. thesis. McGill
University. Ste. Anne-de-Bellevue, Quebec, Canada.
Literature Cited
Brown, B. T., L. E. Stevens, and T. A. Yates. 1998. Influ-
ences of fluctuating riverflows on Bald Eagle foraging
behaviour. Condor 100: 745-748.
Chubbs, Tony E., and Perry G. Trimper. 1998 The diet of
nesting Ospreys, Pandion haliaetus, in Labrador. Canadian
Field-Naturalist 112: 502-505.
Heath, Joel P., Geoff Goodyear, and Joe Brazil. 2001.
Observation of a Golden Eagle, Aquila chrysaetos, attack
on a Harlequin Duck, Histrionicus histrionicus, in northern
Labrador. Canadian Field-Naturalist 115: 515-516.
Jackman, R. E., W. G. Hunt, J. M. Jenkins and P. J.
Detrich. 1999. Prey of nesting bald eagles in northern
California. Journal of Raptor Research 332: 87-96.
Jedrzejewska B., V. E. Sidorovich, M. M. Pikulik, and W.
Jedrejewski. 2001. Feeding habits of the otter’and the
American mink in Bialowieza Primeval Forest (Poland)
compared to other Eurasian populations. Ecography 242:
165-180.
Lariviere. Serge, and Lyle R. Walton. 1998. Lutra cana-
densis. Mammalian Species (587) American Society of
Mammalogists. Pages 1-8.
Madsen, A. B., and A. Prang. 2001 Habitat factors and the
presence or absence of Otters Lutra lutra in Denmark. Acta
Theriologica 46: 171-179.
McDonald, R. A. 2002. Resource partitioning among British
and Irish mustelids. Journal of Animal Ecology 71: 185-
200.
Melquist, W. E. and M. G. Hornocker. 1983. Ecology of
river otters in west central Idaho. Wildlife Monographs 83:
1-60.
Ruiz-Almo. J., J. M. Lopez-Martin, and S. Palazon. 2001.
The influence of fish abundance on the otter (Lutra lutra)
population in Iberian Mediterranean habitats. Journal of
Zoology 254: 325-336.
Received 28 June 2002
Accepted 19 October 2004
270 THE CANADIAN FIELD-NATURALIST Vol. 118
Sea Otter, Enhydra lutris, Sightings off Haida Gwaii / Queen
Charlotte Islands, British Columbia, 1972-2002
KIMBERLY RAUM-SURYAN!3, KENNETH PITCHER!, and RICHARD LAMY?
' Alaska Department of Fish and Game, Division of Wildlife Conservation, 525 W. 67 Avenue, Anchorage, Alaska 99518 USA;
e-mail: kraumsuryan @charter.net
? Gwaii Haanas National Park Reserve/Haida Heritage Site, P.O. Box 37, 120 Second Avenue, Queen Charlotte, British Columbia
VOT 1SO Canada
>Current address: 928 NW Cottage Street, Newport, Oregon 97365 USA
Raum-Suryan, Kimberly, Kenneth Pitcher, and Richard Lamy. 2004. Sea Otter, Enhydra lutris, sightings off Haida Gwaii/Queen
Charlotte Islands, British Columbia, 1972-2002. Canadian Field-Naturalist 118(2): 270-272.
On 27 June 2001 we observed and photographed a Sea Otter (Enhydra lutris) adjacent to a Steller Sea Lion (Eumetopias
jubatus) haulout near Sgang Gwaay (Anthony Island), Haida Gwaii / Queen Charlotte Islands. This is one of only eight
documented sightings of Sea Otters in these waters during the past 30 years. These sightings may represent the beginning of
the expansion of Sea Otters to their former range off Haida Gwaii.
Key Words: Sea Otter, Enhydra lutris, Haida Gwaii, Queen Charlotte Islands, British Columbia.
The Sea Otter (Enhydra lutris) once ranged in near-
shore waters along the North Pacific Rim from Japan
to Baja California. The worldwide population of Sea
Otters in the early 1700s was estimated to be between
150 000 (Kenyon 1969) and 300 000 animals (John-
son 1982). Middens (human food waste mounds) in-
dicate that aboriginal people, including the Haida,
hunted Sea Otters (Simenstad et al. 1978; Acheson
1998; Sloan 2004). Although this harvest may have
caused local reductions of Sea Otter populations near
village sites (Simenstad et al. 1978), the species was
abundant throughout its range prior to commercial ex-
ploitation. Following the advent of commercial hunting
in 1741, the worldwide population of Sea Otters de-
clined to less than 2000 animals by 1911, limited to
remnant groups throughout the range (Kenyon 1969).
Many of these remnant groups (including one group
located off the Haida Gwaii / Queen Charlotte Islands,
British Columbia, Canada) were extirpated, likely due
to their small size (Watson et al. 1997). The last Sea
Otter recorded from Haida Gwaii was before 1920
(Kenyon 1969) and the last recorded in British Colum-
bia, near Vancouver Island (prior to reintroduction),
was in 1929 (Cowan and Guiguet 1960; Kenyon 1969).
In 1911 an International Treaty provided protection
of Sea Otters from additional exploitation. Furthermore,
to aid in the recovery of Sea Otters, various translo-
cation projects were conducted from the 1950s to
early 1970s in the Pacific coastal United States and
Canada (Kenyon and Spencer 1960; Kenyon 1969;
Burris and McKnight 1973; Bigg and MacAskie 1978;
Jameson et al. 1982; Jameson et al. 1986; Riedman
and Estes 1990). Since reintroduction, the Sea Otter
population in British Columbia has increased 18.6%
per year from 70 animals in 1977 to an estimated 2 500
animals in 1998 (Watson 2000). Although Sea Otters
continue to expand their range along Vancouver Island
and the central coast of British Columbia (Watson
2000; Figure 1), sightings off Haida Gwaii / Queen
Charlotte Islands remain rare.
On 27 June 2001 we observed and photographed a
Sea Otter of unknown sex adjacent to a Steller Sea Lion
haulout (52°04.966’ N, 131°13.811° W) just south of
Sgang Gwaay (Anthony Island), Haida Gwaii / Queen
Charlotte Islands (Figure 1). The Sea Otter was swim-
ming on its back eating a sea urchin (Strongylocentrotus
sp.). We observed the otter for approximately 30 min-
utes as it swam and dove. This observation is one of
only eight documented sightings (Edie 1973; Taylor
and Gough 1977; Heise et al. 2003) of Sea Otters in
waters surrounding Haida Gwaii / Queen Charlotte
Islands during the past 30 years (Figure 1).
This sighting raises some interesting questions
regarding the origin of this individual and whether or
not Sea Otters are expanding their range to include
the Haida Gwaii / Queen Charlotte Islands once again.
Kenyon (1969) suggested that the most significant
factor limiting the spread of Sea Otter populations is a
tendency of individual Sea Otters to occupy a limited
home range. Although Sea Otters are not known to
migrate, as populations increase, males generally are
the first to explore new areas and their presence some-
times indicates imminent range reoccupation (Loughlin
1980; Garshelis et al. 1984; Pitcher 1989). Garshelis
and Garshelis (1984) recorded long-distance move-
ments of > 100 km for five adult territorial males.
They postulated that the Sea Otters might have left
an area of limited food resources to travel to an area
where food was more abundant. When Sea Otters were
extirpated, many of their primary benthic invertebrate
prey became larger and more abundant (Estes and
Palmisano 1974; Garshelis et al. 1986). When Sea Otters
recolonize they initially encounter more abundant and
larger prey resources than may be expected to persist,
leading to densities of Sea Otters in recovering popu-
lations greater than those that can be sustainable over
Southeast
Alaska
NOTES 27)
51 introduced in 1965
International
Boundary
Haida Gwaii /
Queen Charlotte
Islands
July 1999
August 1990
August 1976
June 2001
July 1972
@ Sea Otter sightings
A Sea Otter translocation sites
C»> Current Sea Otter range
@ August 2002
55 introduced in 1965
Ga British Columbia
Wd
D : 2 IN s a
Q
VY
Goose Islands
Group
89 introduced between 1969 and 197
200 Kilometers
134° 132° 130° 128° 126°
FicureE 1. Sightings of Sea Otters around Haida Gwaii / Queen Charlotte Islands, locations of Sea Otter translocations
nearest Haida Gwaii, and current Sea Otter distribution in Southeast Alaska and British Columbia (map adapted
from Parks Canada Report 038, Living marine legacy of Gwaii Haanas. IV: Marine mammal baseline to 2003 and
marine mammal-related management issues throughout the Haida Gwaii region by Heise et al. 2003).
time (Bodkin et al. 2000). As prey is consumed, Sea
Otter densities should decline and fluctuate at an equil-
ibrium density (Estes 1990) through decreased repro-
duction, increased mortality, or through emigration
(Bodkin et al. 2000).
Sea Otter population increases in the Aleutian Islands
were achieved largely by range expansion over deep,
wide ocean passes (Estes 1990). Unless the Sea Otter
we observed is a member of a previously undetected
group off Haida Gwaii / Queen Charlotte Islands, this
individual would have had to travel at least 175 km
across an open expanse of water from the nearest
known group of otters along the British Columbia coast
(Figure 1). If this individual traveled from southeast
272
Alaska or northern Vancouver Island, the distance would
be even greater. If Sea Otter populations have reached
or exceeded carrying capacity in certain regions of
British Columbia or southeast Alaska (Watson et al.
1997; Watson 2000), this may be the beginning of the
expansion of Sea Otters to their former range off Haida
Gwaii / Queen Charlotte Islands. This range expansion
may be particularly important given the precipitous
population decline of Western Alaska Sea Otters dur-
ing the past 15 years (Doroff et al. 2003) and the pro-
posal to list the population as threatened under the
United States Endangered Species Act (Federal Regis-
ter: 11 February 2004; Volume 69, Number 28).
Acknowledgments
We thank the Gwaii Haanas National Park Reserve
and Haida Heritage Site for allowing us to conduct
Steller Sea Lion surveys (Research Permit 01-01) off
Haida Gwaii, thereby allowing us to observe the Sea
Otter mentioned. We are grateful to Jane Watson, Norm
Sloan, Tom Gelatt, and two anonymous reviewers for
their comments regarding this note.
Literature Cited
Acheson, S. 1998. In the wake of the ya’aats’ xaatgaay [Iron
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T. J. Evans. 2003. Sea otter population declines in the
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Edie, A. G. 1973. Sea otter sighting at Cape St. James, Bri-
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Social organization of sea otters in Prince William Sound,
Alaska. Canadian Journal of Zoology 62: 2648-2658.
THE CANADIAN FIELD-NATURALIST
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Garshelis, D. L., J. A. Garshelis, and A. T. Kimker. 1986.
Sea otter time budgets and prey relationships in Alaska.
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J. K. B. Ford. 2003. Living marine legacy of Gwaii Haanas
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Simenstad, C. A., J. A. Estes, and K. W. Kenyon. 1978.
Aleuts, sea otters, and alternate stable-state communities.
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Sloan, N. A. 2004. Northern abalone: Using an invertebrate
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Taylor, R., and B. Gough. 1977. New sighting of sea otter
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Watson, J. C. 2000. The effects of sea otters (Enhydra lutris)
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Received 6 August 2002
Accepted 26 August 2004
ISABELLE SCHMELZER! and FRANK PHILLIPS”
NOTES
273
_ First Record of a Barred Owl, Strix varia, in Labrador
'Department of Environment and Conservation, Wildlife Division, Government of Newfoundland and Labrador. P.O. Box 2007,
Corner Brook, Newfoundland A2H 7S1 Canada; e-mail: [sabelleSchmelzer@ gov.nl.ca
"Department of Natural Resources, Forestry Division, Government of Newfoundland and Labrador, Goose Bay, Labrador
AOP 1CO Canada
Schmelzer, Isabelle, and Frank Phillips. 2004. First record of a Barred Owl, Strix varia, for Labrador. Canadian Field-Naturalist
118(2): 273-276.
A Barred Owl (Strix varia) was heard calling in central Labrador, Canada in 2001, and a dead owl was found in the same
area in 2004. These are the first confirmed records for the Province of Newfoundland and Labrador.
Key Words: Strix varia, Barred Owl, range, vagrant, Newfoundland and Labrador.
Barred Owls (Strix varia) are common in southern
Canadian forests from British Columbia through Nova
Scotia (AOU 1998), occurring in mixed evergreen and
mature deciduous woodlands, but also into the boreal
forest in the northern portion of its range (Erskine
1977; Godfrey 1986; Mazur et al. 1998). There are no
confirmed records of Barred Owls for the Province of
Newfoundland and Labrador (Todd 1963; ACCDC
2004*). We document two occurrences of a Barred
Owl near Happy Valley — Goose Bay, Labrador, three
years apart.
On the evening of 24 August 2001, at 22:00 hrs, a
lone Barred Owl was heard calling in the forest north
of Happy- Valley Goose Bay, Labrador, along the banks
of the Goose River (53° 24'N, 60° 26'W) by one of
the authors (IS) (Figure 1). The owl called continu-
ously for several minutes from the same location,
approximately 250 m away. The song was made up
of the characteristic pattern of 8 hoots, separated into
two parts by a pause after 4 hoots, and ending with a
characteristic descending pitch on the last hoot (‘hoo-
hoo hoohoo, hoohoo hoohooahhw’ ). The calls of this
owl may be unfamiliar to residents of Labrador, but
Barred Owl calls are very distinctive, and were imme-
diately recognizable to one of the authors (IS). The
only other owl species in the area with which the calls
could possibly be confused is the Great Horned Owl
(Bubo virginianus), whose call is of a deeper tone, and
consists of five or six hoots, beginning with one em-
phatic hoot, followed by several shorter and quieter
calls, and ending with two long hoots on the same pitch
(‘Hooo! hoohoohoo Hoooo, Hoooo’). The calls of the
two owls differ in tone, pattern and rhythm, and are not
difficult to tell apart by experienced listeners.
Using a vocal imitation of the call, the author at-
tempted to elicit a callback. The owl responded by
leaving its perch, approaching her, and selecting a new
perch within 50 m of her location. It made no other
movements, and she was able to elicit vocal respons-
es to her calls for nearly an hour. During this period,
the owl occasionally varied its call either by repeat-
ing only the last section ‘hoohooahhw’, or by short-
ening the first section to a rising series of 3 notes
followed immediately by the distinctive descending
cackle (‘hoohoohoo hoohooahhw’ ). Unfortunately, due
to darkness and heavy forest cover, the owl was not
sighted. At the time of observation, the air temperature
was 10°C, winds were calm, and the skies were clear.
Tourists camped at the site reported hearing the same
calls during the previous evening.
On the evenings of 26, 28, and 31 August, at approx-
imately 22:00, IS returned to the area to perform a
nocturnal callback survey (using a vocal imitation of
the call) to check for the presence of the owl. Roads
and paths in forested areas within 10 km of the origi-
nal sighting were surveyed, with stops every 0.3 —
0.5 km, and several minutes spent at each’ station
calling and listening for a response. No Barred owls
were detected during these subsequent surveys.
The second observation occurred three years later,
in virtually the same location (53° 27'N 60° 18'W, on
16 July 2004 (Figure 1). A dead owl was seen on the
side of Route 530, at approximately 08:00 hrs. On
closer inspection, the owl carcass showed no obvious
sign of injury or illness, and was completely intact,
with no sign of scavenging, and no fly larvae. The
eyes were present and moist (not sunken, retracted,
or absent as in older kills). Given the abundance of
foxes (Vulpes vulpes), Ravens (Corvus corax), Gray
Jays (Perisoreus canadensis) and other scavengers, it
is the opinion of the authors that the owl had been
dead for a few hours at most.
Field marks on the owl included dark eyes, vertical
barring on the belly and short, horizontal bars across
the chest, all characteristic of Barred Owls (Figure 2).
The owl was also assessed using the criteria of Pyle
(1997). The lack of down on the head and contour
feathers, flight feathers that were broad and uniform in
color and wear, and the presence of squared bars on
the primary coverts all suggest the bird was an adult
(After Hatch Year or AHY). On dissection, the owl
was determined to be a female by the presence of an
ovary. No brood patch was present.
Barred owls have been observed in Québec north
of the St. Lawrence River (Gagnon and Bombardier
1996). The breeding range has been reported to extend
274
Quebec
Grebe 1992
0) 150 300 450
Kilometers Ve
ay
THE CANADIAN FIELD-NATURALIST
Vol. 118
FiGure 1. A summary of Barred Owl records in Labrador and nearby Quebec. Further description of the records is given in
the text.
to 50° North in eastern Canada (David 1980; Godfrey
1986). Our review of the literature, however, revealed
several sightings north of this latitude in Québec. For
example, a Barred Owl was reported near Lac aux
Cédres, 52° 00'N, 67° 07'W, near the Labrador border
in 1917 (Todd 1963). It has been reported more recently
further west near Nemiscau, 51° 42'N, 76° 15'W, and
Lake Evans, 50° 55'N, 77° 00'W, (Grebe 1992). Addi-
tionally, Comeau referred to the bird as “tolerably
common” near Godbout, 49° 19'N, 67° 18'W, on the
North Shore of the Gulf of St. Lawrence (in Merriam
1882), and a specimen was captured at Lac Paterson
in Roberval County (50° 11'N, longitude not specified)
in 1954 (Godfrey 1957). Nonetheless, the occurrence
of the owl in central Labrador is 500 km distant from
the nearest previous report, and 700 km outside regions
where the species is noted regularly.
During the past several decades, the geographic
range of the Barred Owl has expanded in western
North America, and most recent discussion has focused
on its movements into the Pacific Northwest (Levy
1999; Boxall and Stepney 1982; Wright and Hay-
ward 1998). However, on the basis of sightings in
Quebec north of the St. Lawrence River, Harper (1958)
proposed that the range of the Barred Owl was also
extending northward in eastern North America. Al-
though the Gulf of St. Lawrence and the Strait of
Belle Isle present significant barriers to occurrence
on the island of Newfoundland, the forests of Quebec
and Labrador are continuous and present no obsta-
cles to movement. The environs of Happy Valley —
Goose Bay, including the Churchill River valley and
coastal plain surrounding Lake Melville, belong to
the “High Boreal Forest’ ecoregions, (Government of
Newfoundland and Labrador 2004*) and consist of
mature, dense mixed deciduous/coniferous forest on
sandy soil. Predominant tree species are Trembling
Aspen (Populus tremuloides) and White Birch (Betula
papyrifera), with coniferous species such as Balsam
Fir (Abies balsamea), and White and Black spruce
(Picea glauca, P. mariana) occurring secondarily.
Suitable breeding habitat for Barred Owls is often
associated with the presence of snags used as nest
cavities (Haney 1997), but also nests of other raptors
or corvids (Elderkin 1987). This region features the
most favorable climate in all of Labrador, including a
growing season of 120-140 days. Conversely, the up-
land plateaus of central and western Labrador are
2004
FiGureE 2: Adult female Barred Owl collected near Happy
Valley — Goose Bay in July 2004, which showed char-
acteristic gray-brown coloration, yellow bill, vertical
barring on the belly and horizontal barring on the chest.
Flight feathers (right wing shown) are broad and uni-
form in colour and wear, suggesting an adult bird
that has not yet molted.
characterized by a subarctic forest and climate, and
border the former ecoregion to the north and west.
The elevation, vegetative communities, and severe cli-
mate may pose a barrier to an eastward expansion from
northern Québec. To the south and east however, broad
river valleys and mixedwood boreal forests predomi-
nate.
In the absence of evidence of breeding, it is un-
known whether this record represents a possible range
expansion by the Barred Owl, or simply documents
the occurrence of a vagrant bird in potentially suit-
able habitat on two separate occasions. The fact that
in One instance the owl was an adult female, and that
she was found within the breeding season, does not
NOTES
275
preclude range expansion as a possible explanation.
The absence of geographical barriers to movement
from northeastern Quebec, particularly from the north
shore of the St. Lawrence, into south-central Labrador
supports this notion. The establishment of owl surveys
in Labrador should help to clarify such questions, and
others, in the future.
Acknowledgements
We extend thanks to John Thomas and Joe Brazil for
sharing their knowledge of bird records for Labrador,
and for encouraging us to contribute and document
our own sightings. Bruce Rodrigues used his banding
expertise to sex and age the owl specimen. Chris
Earley, Paul Linegar, and Bruce Mactavish provided
constructive and useful comments on earlier drafts of
the manuscript.
Documents Cited (marked * in text)
Atlantic Canada Conservation Data Center. 2004.
Species Rarity Ranks: Labrador Birds, August 2004. P.O.
Box 6416, Sackville, New Brunswick. E4L 1G6 http://
www.accde. com.
Government of Newfoundland and Labrador. 2004.
Department of Natural Resources-Forestry. Ecoregions of
Labrador. http://www.gov.nf.ca/forestry/maps/eco_lab.stm.
GREBE. 1992. Compexe Grande-Baleine. Avant-projet,
phase II. Compte réndu de I’ étude télémétrique de I’ Aigle
royal réalisée dans le complexe Grande Baleine en juin
1992; mission G4. Report for Hydro Québec vice prési-
dence environnement Montréal. 63 pages.
Literature Cited
American Ornithologists’ Union (AOU). 1998. Check-list
of North American Birds, 7 edition. American Ornitho-
logists’ Union. Allen Press, Inc. Lawrence Kansas. 829
pages.
Boxall, P. C., and P. H. R. Stepney. 1982. The distribution
and status of the Barred owl (Strix varia) in Alberta (Can-
ada). Canadian Field-Naturalist 96: 46-50.
David, N. 1980. Etat et distribution des oiseaux du Québec
méridional. Cahiers d’ ornithologie Victor-Gaboriault, (3).
Club des ornithologues du Québec, Charlesbourg. 213
pages.
Elderkin, M. F. 1987. The breeding and feeding ecology of
a Barred owl, Strix varia Barton, population in King’s
County, Nova Scotia. M.Sc. thesis, Acadia University,
Wolfville, Nova Scotia. 203 pages.
Erskine, A. J. 1977. Birds in boreal Canada: communities,
densities and adaptations. Canadian Wildlife Service.
Report Series number 41. 73 pages.
Gagnon, C., and M. Bombardier. 1996. Barred Owl in The
Breeding Birds of Québec: Atlas of the breeding birds of
southern Québec. Edited by J. Gauthier and Y. Aubry.
Association québécoise des groupes des ornithologues,
Province of Québec Society for the Protection of Birds,
Canadian Wildlife Service, Environment Canada, Québec
Region Montréal. 1302 pages.
Godfrey, W. E. 1957. Some distributional notes on Canadian
birds. Canadian Field-Naturalist 70: 136-138.
Godfrey, W. E. 1986. The birds of Canada, revised edition.
National Museum of Natural Sciences, Ottawa. 595 pages.
276
Haney, J. C. 1997. Spatial incidence of Barred owl (Strix
varia) reproduction in old-growth forest of the Appala-
chian Plateau. Journal of Raptor Research 31: 241-252.
Harper, F. 1958. Birds of the Ungava Peninsula. Museum
of Natural History, University of Kansas. Miscellaneous
Publications number 17. 171 pages.
Levy, S. 1999. Owl vs. owl. Natural History 108: 28-32.
Mazur, K. M., S. D. Frith, and P. C. James. 1998. Barred
owl home range and habitat selection in the boreal forest
of central Saskatchewan. Auk 115: 746-754.
Merriam, C. Hart. 1882. List of birds ascertained to occur
within ten miles from Point de Monts, Province of Qué-
bec, Canada; based chiefly upon the notes of Napoleon
THE CANADIAN FIELD-NATURALIST
Vol. 118
A. Comeau. Bulletin of the Nuttall Ornithological Club
8: 244-245.
Pyle, P. 1997. Identification guide to North American birds
— part 1. Slate Creek Press, Bolinas, California, USA.
Todd, W. E. C. 1963. Birds of the Labrador Peninsula and
Adjacent Areas. A distributional list. University of Toronto
Press, Toronto. 819 pages.
Wright, A. L., and G. D. Hayward. 1998. Barred owl range
expansion into the central Idaho wilderness. Journal of
Raptor Research 32: 77-81.
Received 23 January 2002
Accepted 30 August 2004
Forked Three-awned Grass, Aristida basiramea Engelm. ex Vasey:
A New Addition to the Flora of Quebec
JACQUES BRISSON
Institut de recherche en biologie végétale, Université de Montréal, 4101, Sherbrooke Street East, Montréal, Québec H1X 2B2
Canada
Brisson, Jacques. 2004. Forked Three-awned Grass, Aristida basiramea Engelm. ex Vasey: a new addition to the flora of Quebec.
Canadian Field-Naturalist 118(2): 276-277.
A population of Forked Three-awned Grass (Aristida basiramea Engelm. ex Vasey; Poaceae) was found for the first time in
Quebec, on a sand barren of the Cazaville region (Haut-Saint-Laurent). The only other region where this species is known
in Canada is on the southern side of Georgian Bay in Ontario.
Key Words: Aristida basiramea, Forked Three-awned Grass, Poaceae, rare plants, Quebec
Une population d’Aristida basiramea Engelm. ex Vasey (Poaceae) fut trouvée pour la premiére fois au Québec, dans une
lande sableuse de la région de Cazaville (Haut-Saint-Laurent). Le seul autre endroit ot: l’espéce est présente au Canada est
sur le coté sud de la Baie Georgienne en Ontario.
Mots-clés : Aristida basiramea, Poaceae, plantes rares, Québec
In September 2001, during an ecological survey near
Cazaville, in the Haut-Saint-Laurent region of south-
ern Quebec, a population of Forked Three-awned Grass
(Aristida basiramea Engelm. ex Vasey) was found in
a dry, sandy grass-field. Other populations were later
located in similar habitats nearby. This is the first
time the species has been reported for Quebec. In
Canada, A. basiramea is known from four extant
naturally-occurring sites located in southern Ontario,
three of which are in Simcoe County, and one in
Muskoka County (Allen 2001). The extent of
occurrence in Ontario only totals 16 hectares. There
is also one adventive station in northwestern Ontario,
at Rainy River (Allen 2001). A few other reports
exist, such as one in Norfolk County in Ontario, and a
few more in Manitoba. However, the locality of the
Norfolk specimen may be the result of a labelling
error (Reznicek 1984), while the reports from
Manitoba are considered questionable due to the
absence of existing specimens (Scoggan 1957; Allen
2001). Thus, the Cazaville area becomes the second
area in Canada where the presence of the species is
confirmed. The species is listed as rare in Ontario
(Reznicek 1984) and is considered threatened in Can-
ada (COSEWIC 2003). On the basis of the newly
discovered population, A. basiramea should be added
to the list of rare vascular plants likely to be designated
threatened or vulnerable (Labrecque and Lavoie 2002).
The genus Aristida is represented by 250 to 300 spe-
cies, 29 of which are native to North America north
of Mexico (Flora of North America Editorial Com-
mittee 2003). A. basiramea is an annual plant from
30 to 60 cm high characterized by glumes of unequal
length and 1-flowered spikelets terminated by three
long awns, one in the middle with a twisted base and
two shorter straight awns on each side. It is abundant
on dry sterile or sandy soil in the midwestern states.
At the northeastern periphery of its range in the United
States, it forms disjunct populations on dry lands and
along sandy roadsides, some populations of which ap-
pear to be adventive. The closest reports of A. basira-
mea south of the border with Québec were from Platts-
burg, Clinton Co., New York (S. J. Smith, 25 July 1965,
NYS); Columbia, northern Coos Co., New Hampshire
(A. S. Pease, 17 September 1955, NEBC); and Avon,
Franklin Co., Maine (A. Haines, 26 October 1990,
MAINE). The species is recognized as rare in Maine,
Iowa and Colorado (Allen 2001).
The Cazaville area (45°03’ N, 74°22’ W) is located
in the Mixed Plain Ecozone of the St-Lawrence Low-
land Ecoregion (Ecological Stratification Working
Group 1995). The area is characterized by a vast sandy
plain of littoral origin dating from the last post-gla-
cial period. White Pine (Pinus strobus) forests were
abundant before European settlement (Brisson and
Bouchard 2003), but today, the area is occupied by
sandy, grassy fields, sand barrens and secondary forests
of Red Maple (Acer rubrum), Trembling Aspen (Popu-
lus tremuloides) and Gray Birch (Betula populifolia).
Aristida basiramea was found on open, sandy grass-
field with Poa compressa, Danthonia spicata, and vari-
ous types of lichens. The sandy plain of Cazaville is
host to other rare plant species. The northernmost
colony of Monarda punctata, a species rare for Quebec
and Canada, was recently found nearby (Boudreault
and Brisson 1994). As well, Hedeoma hispida, consid-
ered rare for Quebec (Labrecque and Lavoie 2002),
is also found on the sandy plain.
Specimens of A. basiramea were deposited at the
Marie-Victorin Herbarium (MT: Brisson Number JBO1-
25)
Acknowledgments
I thank Stuart Hay (Marie-Victorin Herbarium) and
Stephen Darbyshire (Agriculture and Agri-Food Can-
ada), who reviewed the manuscript and provided useful
information. I am also grateful to Richard Mitchell
(Biological Survey, New York State Museum) and Ray
Angelo (Harvard University Herbaria, New England
Botanical Club) for kindly providing information on
A. basiramea in the U.S.
NOTES
Documents Cited (marked * in text)
Allen, G. M. 2001. COSEWIC Status Report on Forked
Three-awned Grass. Committee on the Status of Endan-
gered Wildlife in Canada. Environment Canada, Ottawa,
Ontario. 26 pages.
Literature Cited
Boudreault, C., and J. Brisson. 1994. Une addition a la flore
du Québec: Monarda punctata var. villicaulis (Lamiaceae).
Canadian Field-Naturalist 108: 499-500.
Brisson, J., and A. Bouchard. 2003. Human activities caused
major changes in tree species composition in southern
Quebec, Canada. Ecoscience 10: 236-246.
COSEWIC. 2003. Canadian Species at Risk, November
2003. Committee on the Status of Endangered Wildlife in
Canada. 44 pages.
Ecological Stratification Working Group. 1995. A National
Ecological Framework for Canada. Agriculture and Agri-
Food Canada, Research Branch, and Centre for Land and
Biological Resources Research and Environment Canada,
State of the Environment Directorate, Ecozone Analysis
Branch, Ottawa/Hull. Report and National map at 1:
7 500 000 scale.
Flora of North America Editorial Committee. 2003. Flora
of North America North of Mexico. Volume 25: Poaceae.
(Part 2). New York and Oxford. 814 pages.
Labrecque, J., and G. Lavoie. 2002. Les plantes vasculaires
menacées ou vulnérables du Québec. Gouvernement du
Québec, Ministére de l’environnement. Direction du patri-
moine écologique et du développement durable, Québec,
200 pages.
Reznicek, A. A. 1984. Poaceae — Aristida basiramea . One
page in Atlas of the rare vascular plants of Ontario. Edited
by G. W. Argus and D. J. White. 1982-1987. National
Museum of Natural Sciences. Looseleaf.
Scoggan, H. J. 1957. Flora of Manitoba. National Museum
of Canada, Bulletin 140. 619 pages.
Received 30 November 2001
Accepted 21 June 2004
278 THE CANADIAN FIELD-NATURALIST Vol. 118
Evidence for the Use of Vocalization to Coordinate the Killing of a
White-Tailed Deer, Odocoileus virginianus, by Coyotes, Canis latrans
ERICH M. Muntz! and BRENT R. PATTERSON?
Department of Natural Resources, Wildlife Division, 136 Exhibition Street, Kentville, Nova Scotia B4N 4E5 Canada
‘Current address: Parks Canada Agency, Cape Breton Highlands National Park of Canada, Ingonish Beach, Nova Scotia
BOC 1L0 Canada
*Current address: Ontario Ministry of Natural Resources, Wildlife Research and Development Section, 300 Water Street, 3"
Floor North, Peterborough, Ontario K9J 8M5 Canada; e-mail: brent.patterson@mnr.gov.on.ca. Author to whom
correspondence should be addressed.
Muntz, Erich M., and Brent R. Patterson. 2004. Evidence for the use of vocalization to coordinate the killing of a White-Tailed
deer, Odocoileus virginianus, by Coyotes, Canis latrans. Canadian Field-Naturalist 118(2): 278-280.
Among the social canids, howling is largely accepted as playing a role in territory maintenance. However, its role in commu-
nication within packs, such as announcing departures from den and rendezvous sites and coordinating reunions or movements,
remains largely speculative. We report an observation where a radio-collared adult male Coyote (Canis latrans) and his mate
seemed to summon two other Coyotes (presumed to be their offspring) from ~700 m away to join in the successful pursuit
of an adult male White-tailed Deer (Odocoileus virginianus). Our observation suggests that Coyotes can use vocalization as
an effective means of coordinating social activities such as the hunting of large prey.
Key Words: Eastern Coyote, Canis latrans, predation, vocalization, social organization, Nova Scotia.
Auditory communication serves an important role
in the social ecology of the Canidae (Harrington and
Mech 1978, 1979; Theberge and Falls 1967; Gese
and Ruff 1998). Howling is a means of long-distance
communication that apparently can be heard at dis-
tances of > 6 km (McCarley 1975; Harrington and Mech
1979). Among Coyotes (Canis latrans) and Wolves
(Canis lupus), howling is largely accepted as playing
a role in territory maintenance (Joslin 1967, Harrington
and Mech 1978, 1979; Gese et al. 1988). Intrapack
communicatory roles, such as announcing departures
from den and rendezvous sites, and coordinating re-
unions or movements remain largely speculative (The-
berge and Falls 1967; Mech 1970; Harrington and
Mech 1978). Bender et al. (1996) suggested that howl-
ing among Coyotes might serve to reunify packs to
facilitate the hunting of ungulates. Herein we report a
case where a breeding pair of Coyotes in pursuit of a
large White-tailed Deer (Odocoileus virginianus) was
able to entice two other Coyotes to join the pursuit
from ~700 m away.
Observation
We interpreted the details of the chase while snow-
tracking a radio-collared Coyote and his mate on 27
February 1994 as part of a study of the effects of the
distribution and abundance of Snowshoe Hares, Lepus
americanus, and White-tailed Deer on the life history
of Coyotes in Nova Scotia (Patterson and Messier
2000, 2001; Patterson et al. 1998). The actual event
probably occurred during the previous night.
Radio-collared Coyote AM3 and his mate were
traveling west on a snow-covered (10-15 cm) secondary
road | km east of Kejimkujik National Park (44°20'N,
65°15'W) when they abruptly veered due north.
Lengthened strides indicated that their pace increased,
and after 40 m the pair jumped three deer, of which
two headed west and the other east. Both Coyotes
chased the deer that ran to the east. After 280 m the
two Coyotes split up, with the larger radio-collared
male chasing the deer down a steep bank into a bowl-
shaped depression. AM3 then swung wide to the left
of the deer, apparently in an attempt to steer the deer
into the path of the other Coyote that had remained
on the rim of the depression. The second Coyote cir-
cled the depression and ran down the opposite side in
front of the deer. We interpreted this as an effort to
prevent the deer from leaving the depression.
Within 3 m of the second Coyote’s resumption of
the chase, both Coyotes attacked the deer and drew hair
but no blood. The deer escaped and again attempted to
run up the side of the depression when AM3 swung to
the right and turned the deer back down into the depres-
sion, where the second Coyote was waiting and again
resumed the chase. The Coyotes attacked the deer again
at 383 m where a larger area of snow was trampled
down than during the first attack. There was more
hair strewn about, but still no blood. At this point two
more Coyotes became involved in the chase. At 390 m
more hair was detected as well as blood, indicating
another attack. The deer broke away once more only to
be attacked again at 397 m. After escaping yet again
the deer made a long run across the middle of the
depression. Considerable amounts of blood and hair
strewn about a 20 x 30 m packed-down area at 590 m
indicated a more serious struggle. The deer made one
final escape and was pulled down by the front end at
630 m, with tracks indicating that the deer was drag-
2004
ging at least two of the Coyotes, which appear to have
been hanging off its sides. After dragging the Coyotes
~ for 40 m the deer was killed at the 670 m mark.
Examination of the carcass revealed that the deer
was a large 3.5 year old buck that showed no obvious
debilitations and was apparently in good health (>80%
femur marrow fat content and other visible body fat
reserves). We believe that the deer would likely have
escaped if it could have got out of the depression. The
two Coyotes initially involved in the chase appeared
to have trouble drawing blood from the deer until the
other two Coyotes joined them. Backtracking later
revealed that the two Coyotes that joined the chase in
progress had been traveling in another direction when
they abruptly turned and trotted 690 m in a direct line
to join the chase. Forest cover was dense, precluding
any possibility that these Coyotes observed the chase
prior to joining in. AM3 and his mate were typically
accompanied by two of their young of the year when
traveling in winter 1994 (Patterson and Messier 2001).
We believe that the two Coyotes that joined the chase
“in progress” were probably these same juveniles that
had been temporarily disassociated from their parents.
We speculate that they must have heard AM3 or his
mate howling or yipping and were able to determine
that it would be to their benefit to join the breeding
pair promptly.
Discussion
Although we can not verify that howling was used
to draw the other two Coyotes to the scene of the chase,
we can think of only one other means by which two
Coyotes ~700 m away in forested cover may have been
able to so directly and rapidly locate the scene of the
chase. White-tailed Deer can snort loudly when alarmed,
but snorts are generally only given when a deer per-
ceives danger but does not feel directly threatened
(Hirth and McCullough 1977; Marchinton and Hirth
1984). Furthermore, snorts are more likely to be given
by maternal family groups than by bucks (Hirth and
McCullough 1977). Thus it seems unlikely that snort-
ing by the buck alerted the other two Coyotes to the
chase.
Among forest-dwelling eastern Coyotes increased
reproductive fitness and inclusive fitness for juveniles
before dispersal seem to be the ultimate factors influ-
encing group living (Messier and Barrette 1982; Pat-
terson and Messier 2001). Increased efficiency at using
large prey appears to be a secondary benefit (Gese et
al. 1988; Messier and Barrette 1982; Patterson and
Messier 2001). Coyotes in Nova Scotia were more suc-
cessful at killing deer when thick snow cover impeded
deer movements (Patterson and Messier 2000). There
was only 10-15 cm of snow on the ground during the
event described here and our observations suggest that
in this particular incidence the snow cover may have
been a hindrance to the Coyotes, thus benefiting the
NOTES
279
deer. It was clear that AM3 and his mate were having
difficulty subduing the deer on their own. We believe
that they would not likely have been able to make phys-
ical contact with the deer if it had not entered the
depression. Although Patterson and Messier (2000) did
not detect a consistent increase in deer killing rates
for groups of 2-5 Coyotes, groups of >4 Coyotes
killed proportionately more deer (Patterson 1999). We
suspect that larger group sizes may be more advan-
tageous in hunting large prey in the absence of other
contributing factors such as thick snowcover or glare
ice. The proximate mechanism is likely an increase
in the probability of at least one member of the group
making physical contact with the deer and slowing it
down enough for other group members to assist in
dispatching it. Our observation supports this idea and
suggests that Coyotes can use howling as an effective
means of coordinating social activities such as the
hunting of large prey.
Acknowledgments
This work was supported by Parks Canada, the
Nova Scotia Department of Natural Resources and
Acadia University. We appreciate comments by D. O.
Joly on an earlier draft of the manuscript.
Literature Cited
Bender, D. J., E. M. Bayne, and R. M. Brigham. 1996. Lunar
condition influences coyote (Canis latrans) howling.
American Midland Naturalist 136: 413-417.
Gese, E. M., and R. L. Ruff. 1998. Howling by coyotes
(Canis latrans): variation among social classes, seasons,
and pack sizes. Canadian Journal of Zoology 76: 1037-
1043.
Gese, E. M., O. J. Rongstad, and W. R. Mytton. 1988.
Relationship between coyote group size and diet in south-
eastern Colorado. Journal of Wildlife Management 52:
647-653.
Harrington, F. H., and L. D. Mech. 1978. Howling at two
Minnesota wolf pack summer homesites. Canadian Journal
of Zoology 56: 2024-2028.
Harrington, F. H., and L. D. Mech. 1979. Wolf howling and
its role in territory maintenance. Behaviour 68: 207-249.
Hirth, D. H., and D. R. McCullough. 1977. Evolution of
alarm signals in ungulates with special reference to white-
tailed deer. American Naturalist 111: 31-42.
Joslin, P. W. B. 1967. Movements and homesites of timber
wolves in Algonquin Park. American Zoologist 7: 279-288.
Marchinton, R. L., and D. H. Hirth. 1984. Behavior. Pages
129-168 in White-tailed deer: Ecology and Management.
Edited by L. K. Halls. Stackpole Books, Harrisburg,
Pennsylvania.
McCarley, H. 1975. Long distance vocalizations of coyotes
(Canis latrans). Journal of Mammalogy 56: 847-856.
Mech, L. D. 1970. The wolf: the ecology and behavior of an
endangered species. Natural History Press, New York.
384 pages.
Messier, F., and C. Barrette. 1982. The social system of the
coyote (Canis latrans) in a forested habitat. Canadian Jour-
nal of Zoology 60: 1743-1753.
280
Patterson, B. R. 1999. The effects of prey distribution and
abundance on eastern coyote life history and predation
on white-tailed deer. Ph.D. thesis, University of Saskat-
chewan, Saskatoon, 204 pages.
Patterson, B. R., L. K. Benjamin, and F. Messier. 1998.
Prey Switching and feeding habits of Eastern Coyotes in
Relation to Snowshoe Hare and White-Tailed Deer Densi-
ties. Canadian Journal of Zoology 76: 1885-1897.
Patterson, B. R., and F. Messier. 2000. Factors Influencing
killing rates of White-Tailed Deer by Coyotes in Eastern
Canada. Journal of Wildlife Management 64: 721-732.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Patterson, B. R., and F. Messier. 2001. Social organization
and space use of Coyotes in Eastern Canada relative to
prey distribution and abundance. Journal of Mammalogy
82: 463-477.
Theberge, J. B., and J. B. Falls. 1967. Howling as a means of
communication in timber wolves. American Zoologist 7:
331 -338.
Received 24 September 2002
Accepted 11 October 2004
Book Reviews
ZOOLOGY
Fish of Alberta
By Amanda Joynt and Michael G. Sullivan. 2003. Lone
Pine Publishing, Edmonton, Alberta. 176 pages. $18.95.
ISBN 1-55105-191-5.
This book is a popular account of the 54 established
and 11 more rare fishes of Alberta. It consists of
Acknowledgements, Foreword (by J. S. Nelson, the
expert on fishes of Alberta), Reference Guide, Intro-
duction, Keys to the Fishes, Species Accounts, Size
Comparisons, Other Alberta Fishes (the rarer species),
Glossary, Checklist, Selected References, Further Infor-
mation, Index of Scientific Names, Index of Com-
mon Names and About the Authors. These are mostly
self-explanatory. The Reference Guide is a colour
pictorial summary of each of the 54 species while
Size Comparisons show the fish in relation to a loonie
or a page in the book. The Glossary, Selected Refer-
ences and Further Information sections are short but
give some additional sources and explications of terms.
Schreckstoff is misspelled and the term “alarm sub-
stance” is more user-friendly. Laterally compressed
is a tautonym, as compressed means flattened from
side to side. For a more complete listing of terms
used in ichthyology see www.briancoad.com.
The ichthyofauna includes 16 families with min-
nows (Cyprinidae) having 17 species, 3 introduced;
trouts (Salmonidae) 16 species, 6 introduced; and suck-
ers (Catostomidae) 7 species. Other families are lam-
preys, sturgeons, mooneyes, bullhead catfishes, pikes,
trout-perches, cods, livebearers (2 species introduced
to the Banff hot spring marshes), sticklebacks (1
introduced), sculpins, sunfishes (introduced), perches
and cichlids (1 introduced to the Banff marshes).
The Introduction has information about identifying
fishes, the lives of fishes, adaptations to life in water,
the underwater world, drainage basins of Alberta, top
Alberta fishwatching sites and fishwatching (“not yet
a popular sport’), history of fishes and conservation
issues. Key words are in bold text and some, but not
all of these, have illustrations. One illustration, of Bull
Trout and Walleye larvae used to explain reproductive
strategies, is confusing in that these two distinctive
species have the same larva illustrated.
The Species Accounts comprise two pages for each
established species, in landscape orientation. This
requires some twisting for reading introductory and
other sections that have a standard orientation. None-
theless, the landscape arrangement enables the fish
illustrations to spread across the broadest reach of
the page. Each Account has an introductory section,
Viewing Tips (localities and habitats where the fish
can be seen), Feeding, Spawning, Other Names, Did
You Know? (an anecdote or interesting factoid), ID
(identification characters), Similar Species, Status,
Habitat, Length and Weight, the colour illustration and
a colour, shaded distribution map.
Generally, the book is a good, popular treatment of
this fish fauna written in a readable style that is not as
dry as more scientific accounts. Some errors occur, per-
haps as a result of this style or perhaps from the more
pedantic viewpoint of the reviewer; e.g., in the Long-
nose Sucker account pharyngeal teeth are said to be in
the mouth which could mislead the reader into thinking
these throat teeth are readily visible.
The definition of “fish” and “fishes” is given on page
10 in the Introduction, fish being a single individual
or more than one individual of a single species while
fishes refers to more than one species. Curiously, the
book is wrongly titled. The Reference Guide has a col-
our code for groups of species but since these colours
are various shades of green and blue, they do not lend
themselves to a ready means of locating species groups.
The fish illustrations are positioned with the head to
the right, not a problem for most users, but somewhat
disconcerting to those familiar with most fish books
where traditionally the head faces left. The colour illus-
trations lack the details that can be included on line
drawings, so certain critical features are not always
visible. The illustrations have streaks of white meant as
highlights but in some specimens look like a colour
pattern.
Scientific names are given for all species and are ac-
curate and, although Stizostedion may now be correctly
Sander, the decision to leave it as the more familiar
North American genus is probably apposite for infor-
mation retrieval. Conversely, the Arctic Lamprey is
given its newer name, Lampetra camtschatica, which
is less well known than the older version, L. japonica,
which is not mentioned and would inhibit search for
information in other books. Common names are stan-
dard and include the Northern Pikeminnow, although
its former name Northern Squawfish was not so much
an “unpopular” designation as a derogatory one.
Despite the minor criticisms outlined above, this
book is a good introductory guide to Alberta’s fishes.
Alberta seems well served in this respect with Nelson
and Paetz’s earlier book (1992). The older work pro-
vides a more detailed account of the fish fauna and
may be more suited to the serious student of Alberta’s
281
fishes — there is an extensive list of references (24
pages compared to only 11 references in Joynt and
Sullivan). The book reviewed here has accounts for
65 species while Nelson and Paetz have a more
complete analysis of 59 species and a further 29
species recorded as rare or doubtful for Alberta.
Sharks
By Andrea and Antonella Ferrari. 2002. Firefly Books, Tor-
onto, Ontario. 256 pages. $24.95. ISBN 1-55209-629-7.
Sharks are the most popular of fishes for publica-
tions as people seem to have a fascination for organ-
isms that can eat you (although more sharks are killed
by people than the reverse). This is one of many that
have appeared on this topic.
Despite its title, the book covers the appearance and
behaviour of 120 species of sharks and rays. Coverage
is therefore not complete as sharks and rays number
over 1000 species (as the Foreword states), the aim be-
ing to give an overview of the main groups by select-
ing typical and unusual or fascinating species. Four
species of rabbitfishes (out of about 31 species in the
Chimaeriformes) are also mentioned.
The book has an Introduction of 77 pages with
descriptions of anatomy and biology. Three pages are
devoted, deservedly, to explaining the ampullae of
Lorenzini, an important feature of shark anatomy and
biology, first discovered by an Italian scientist in the
seventeenth century and, surely by coincidence, this
book has Italian authors and is a translation from an
Italian version. This is followed by how to avoid sharks,
how to assist them (by not eating them or buying shark
teeth), marine organisms more dangerous than sharks
(mostly venomous sea snakes, cone shells, sea urchins,
jellyfishes and fishes, but also fish that bite divers en-
thusiastically), and personal accounts of shark encoun-
ters. The Entries section describes the sharks, rays and
rabbitfishes (153 pages), the Appendices (17 pages)
give a Classification of Sharks (but not rays or rabbit-
fishes), an Index, Bibliography and Websites (each a
page long), and Photographic Credits. The websites
“Catalog of Fishes” and “FishBase” are not quoted,
although these give entry to much of the names, biol-
ogy and literature on sharks and rays world-wide for
the more serious student. There are pictorial keys to
In Search of the Golden Frog
By Martha Crump. 2002. University of Chicago Press, 5801
Ellis Avenue, Chicago, Illinois 60637 USA. xiv + 298
pages, Cloth US$27.
Any young person thinking of taking a degree in
one of the biological sciences, particularly if they plan
to become a field biologist, should read this book.
The author, currently Adjunct Professor of Biology at
Northern Arizona University, chronicles her life from
THE CANADIAN FIELD-NATURALIST
Vol. 118
Literature Cited
Nelson, J. S., and M. J. Paetz. 1992. The Fishes of Alberta. The
University of Alberta Press, Edmonton and the University of
Calgary Press. 2"4 Edition, 437 pages.
BRIAN W. COAD
Canadian Museum of Nature, P.O. Box 3443, Station D,
Ottawa, Ontario K1P 6P4 Canada
the shark and ray orders but not any for families or
species so the book cannot be used, nor is it meant, as
a field guide.
The Entries section describes each selected species,
allotting half to two pages per species. There is an
annoying symbol system at the top of each account
to indicate when the shark is active and its danger
level with respect to humans. This information could
easily have been included in the text. A distribution
map is given but at | x 2 cm can only convey a
general impression of where these sharks and rays
are found. The map for the Bluntnose Shark is in-
accurate, for example, showing it in Canadian Arctic
waters when it was first caught at its northern limit in
Nova Scotian waters in 1989 (Gilhen and Coad 1991).
The common and scientific names are given but the
author and date of the scientific name is always in
parentheses (here and in the Classification of Sharks).
The authors (or text editor?) seem not to be aware
that parentheses are only used when the species is
placed in a genus other than the one it was originally
described under. The text comprises the Family to
which the shark or ray belongs, Range, Habitat, Size,
and Habits. All parts of the book are richly illustrated
with colour photographs, over 450 in all.
Despite the comments above, this book is a good
general introduction to sharks and rays. It is lavishly
illustrated, as all such books must be, of a convenient
size, and with a reasonable price.
Literature Cited
Gilhen, John, and Brian W. Coad. 1991. The bluntnose sixgill shark
Hexanchus griseus (Bonnatere, 1788), new to the fish fauna of At-
lantic Canada. Proceedings of the Nova Scotian Institute of Science,
39 (1989): 75-77.
BRIAN W. COAD
Canadian Museum of Nature, P.O. Box 3443, Station D,
Ottawa, Ontario K1P 6P4 Canada
her postgraduate work in 1968 through various projects
to 1998. The book concentrates on the field programs
that are the real love of Professor Crump’s life. Her
main interests are reptiles and amphibians, but her
passion is frogs.
Taking advantage of an opportunity offered by her
discerning professor, she joins a team going to the
Amazon section of Ecuador. From this exposure which
2004
reinforces her desire to work in the field, she returns
| repeatedly to work in South America. Her narrative
_ includes her excitement at being a scientist and mak-
ing discoveries to contribute to her profession. She
also chronicles some of the problems she encounters.
These do not include frightening encounters with large
or dangerous animals. The hazards fall into two cate-
gories. The small pests, mosquitoes, chiggers, chigoes,
bot flies and ants, causes plenty of discomfort. But it is
the large pest, humans, that causes the greatest levels
of concern. She notes the ordinary people are by and
large, friendly and helpful. It is the bandits, police,
_ military, industrialists and rioting natives that disrupt
her life.
As I started to read this book I became very dis-
concerted. In the past few years I have looked for
amphibians and reptiles in tropical jungles on many
_ occasions. My success rate is very low. The author
travels to the same locations in South America and
immediately starts finding many individuals of multi-
ple species. My estimation of my frog finding prowess
dropped page by page. By the time the author reaches
the 1990s, however, her success rate has plummeted.
By 1996 she says “we hug and screech with excite-
ment” on finding one frog. I realize that my lack of
success is due less to my incompetence than to the
Conversations with an Eagle
By Brenda Cox. 2002. Greystone Books, Douglas & McIntyre
Publishing Group, 2323 Quebec Street, Vancouver, Brit-
ish Columbia VST 487. 261 pages, paperback.
This is a story of dedication to an eagle rather than
conversations with one. Brenda Cox was a volunteer
worker at a raptor rehabilitation centre south of Van-
couver (Orphaned Wild Life — OWL), and became
enthralled with raptors of all kinds. Her special inter-
est was a Bald Eagle, which was three months old
when it arrived at the Centre, and her book describes
the trials and tribulations of her efforts to train Ichabod
so that she could be used in the OWL education pro-
gramme.
In the course of the story there are passages de-
scribing the methods used to rehabilitate owls, hawks
and eagles. When the eagle was still young its behav-
iour was typically fearful, but the bird became more
and more aggressive towards Cox, such that she had
to stand against a pillar armed with a household mop
to protect herself if she was attacked. In spite of the
danger, she persisted in training the bird to come to
her gloved arm, and eventually it obeyed three com-
mands: Up, Wait and Off. But it was always uncer-
tain whether the bird would cooperate or not on any
given day. She enlisted the help of expert falconers in
the Vancouver area. They were doubtful whether a
Book REVIEWS
rapid loss of frogs in my lifetime. This is even more
depressing. When I go to Monteverde next spring I
have little hope of seeing the fabulous Golden Frog.
On 7 April 1987 this author saw “over one hundred
dazzling bright golden toads“ at one small pool at
Monteverde.
The author also deserves another accolade for, while
she 1s pursuing her scientific research, she is also be-
ing a parent to two children. I was delighted with the
way she involved them in her work and gave them
opportunities to broaden their knowledge. This may
have made her life harder and certainly caused her
concerns, but I am sure these children will benefit.
So if you want to find out about the life of a field
researcher read this entertaining book. Follow the trials
of first reaching the field locations using often unreli-
able local transport. Join in meals that are good, bad,
or bizarre. Meet local people, many of whom care
greatly about their environment. Find out how a sci-
entist collects data and uses it to create a new under-
standing of our planet.
Roy JOHN
2193 Emard Crescent, Ottawa, Ontario, K1J 6K5 Canada
Bald Eagle could be reliably trained, though they
helped and advised her. Bald Eagles have seldom been
trained successfully, while Golden Eagles have been
used by falconers in many parts of the world. Cox
was able to train the eagle such that she could take
her from her cage to a perch in a field, using jesses
and a stout leash attached to her waist, but there were
increasing dangerous attacks which inflicted talon
wounds on Cox’s head, arms and feet.
After several years, the OWL management decided
that they would never be able to use the bird in their
programme and asked Cox to remove it from the facil-
ity. In its new quarters, shortly afterwards the bird
developed a lung disease and was euthanized. Cox’s
dedication to her volunteer job is remarkable since, in
the course of the seven years, she did not have steady
employment or reliable housing or transportation.
Since Ichabod’s death, she has now found a steady
career: as a conductor with British Columbia Rail,
and watches the wild raptors along the railway lines.
Her story would appeal to someone interested in
raptor rehabilitation methods and the lore of falconry.
JANE ATKINSON
255 Malcolm Circle, Dorval, Quebec H9S 1T6 Canada
284
THE CANADIAN FIELD-NATURALIST
Vol. 118
North American Owls, Biology and Natural History, Second Edition
Paul A. Johnsgard. 2002. Smithsonian Institution Press, Wash-
ington. 298 pages, 42 colour plates, 69 multi-figured black-
and-white maps and sketches, 10 tables, 2 graphs. $46.25
Canadian, hardcover. US$27.95.
Although Dr. Johnsgard’s long history of produc-
ing books about birds is well known, his entry to the
“owl-lover’s camp” is more recent. The first edition of
this book came out in 1988 and immediately became
the standard reference book for owls of the United
States and Canada. For the second edition, 14 years
later, Johnsgard has added twelve species of Mexican
owls and nearly doubled the number of references
(although, contrary to convention, many of the recent
references are not mentioned by name in the text!).
Extremely few changes have been made to the excel-
lent introductory chapters, but this leaves them less up-
to-date than the individual species accounts. Often he
cites the authors of the Birds of North America account,
rather than the original observers who merit the credit;
an example is Gottfred and Gottfred’s new informa-
tion concerning courtship and copulation of the Great
Horned Owl, published in Blue Jay in 1996.
The strengths of the first edition have been main-
tained: the introductory chapters and species accounts
are neatly arranged; maps of each species’ range are
detailed; Johnsgard’s pen-and-ink sketches of aspects
of behaviour are delightful; the colour plates and pho-
tographs are superb. Johnsgard writes well, but in a
few occasions new material has been interjected clum-
sily, marring the previous smooth flow of information
in the first edition.
Some compromises were necessary. To make room
for the twelve Mexican species, detailed descriptions
of plumage have been omitted in this second edition.
This does not excuse three sloppy errors. Johnsgard
tells of the Pygmy Owl range extending altitudinally
to 37 000 meters in Mexico, whereas the quoted source
gave a credible 3700 m. A paper by Jack Holt on Great
Horned Owls in the Cincinnati region is credited to
Denver Holt. Thirdly, when Johnsgard withdrew his
overdrawn sketch of the “false eye-spots” on the back
of the Northern Pygmy Owl’s head from the first edi-
tion and substituted a more realistic sketch of the Fer-
ruginous Pygmy Owl in the second edition, he failed
to change the figure numbers in the text to comply
with this change.
These minor caveats aside, this masterful second
edition will be welcomed by owl enthusiasts around
the world, and should be purchased even by those own-
ing the first edition. It is written more for the scientist
than the amateur, but, by identifying deficiencies in
our current knowledge, this book should offer possi-
bilities for future study by graduate students and others
who love our night-time friends.
Johnsgard’s exquisite sketches, 10 coloured paint-
ings of owls by Louis Agassiz Fuertes, and 31 fine col-
our photographs, including nine of Mexican owls, make
this an unusually attractive book. Buy it!
MARTEN J. STOFFEL
Box 183, RR#4, Saskatoon, Saskatchewan S7K 3J7 Canada
The Mountain White-Crowned Sparrow: Migration and Reproduction at High Altitude
By Martin L. Morton. 2002. Studies in Avian Biology
Number 24. Cooper Ornithological Society, Camarillo,
California. 236 pages, 8 colour plates, pencil illustrations
heading each chapter. U.S.$27.
The northern limit of the distribution of the Moun-
tain White-Crowned Sparrow (Zonotrichia leucophrys
oriantha) extends slightly into southern British Colum-
bia, Alberta and Saskatchewan. Its main breeding range
is in mountainous regions of the western U.S. Here
in Waterton Lakes National Park we’re at the contact
zone between oriantha and Z. |. gambelii.
Morton’s 25-year study of oriantha in the Tioga
Pass area of California’s Sierra Nevada ranks with P.
J. Greenwood’s lengthy study of the Great Tit (Parus
major) in Europe and G. E. Woofenden’s work with
the Florida Scrub Jay (Aphelocoma coerulescens) in
showing the value of continuous long-term field inves-
tigations in advancing a broad spectrum of ideas and
hypotheses in avian biology. Morton’s focus is differ-
ent, however, in emphasizing physiology more than
behaviour or ecology. In 1968, Morton recognized
that there were significant gaps in knowledge of mi-
gratory passerines on their summering grounds, espe-
cially in mountains where large variations in environ-
mental conditions occur.
As my interests lie more with natural history, life
history data (age at maturity, number, size and sex ratio
of offspring, dispersal and survival rates) and ecolog-
ical factors than with physiology, I found Morton’s
first three chapters on Migration Arrival, Social System
and Behavior, and Demography of most interest (al-
though a bit disappointing at only one-quarter of the
book’s pages). The dynamics of arrival of oriantha
varied greatly from year-to-year depending upon the
amount of remaining snowpack and the frequency of
spring storms, as well as by age and sex. By trapping
and colour-marking individuals, the researchers found
that older males (age 2+ years) generally arrive ear-
liest, followed by one-year-old males, older females
and one-year-old females. Throughout the monograph,
Morton does an excellent job of analysing observed
data in terms of costs and benefits, and ecological fact-
2004
ors, in this case, suggesting that older, experienced
birds knew the migration route and recognized the
_ breeding area once they reached it, even it if was snow-
covered.
Morton’s efforts over many reproductive seasons
made it possible to measure mate fidelity, age of mates,
frequency of polygamous pairings, agressive behav-
iours, and the functions of vocalizations, in addition
to the usual study of territory establishment, pairing,
and between-year breeding dispersal.
Although I expected the chapters on Gonadal Con-
dition, and Body Size and Body Condition, to be of
less personal interest, Morton’s explanations of the
connections between physiology and behaviour, and
| description of the role of environmental cues in annual
_ cycles made these sections much more interesting than
anticipated. Environmental factors are either ultimate
(e.g., availability of an adequate food supply, predation
pressure, weather patterns) or proximate (e.g., photo-
| period, ambient temperature) in their effects on the
timing of reproduction.
Nest history (chapters 7, 8, 9 and 10 on Nests and
Eggs, Nestlings and Fledglings, Nest Failure and
Book REVIEWS
Reproductive Success, respectively) provided reliable
information on physiological and behavioural respons-
es of breeding birds to environmental variation, often
to the level of individuals because of Morton’s use of
marked birds. And the researchers determined that
the snowpack, because of its effects on nesting sched-
ules and nest locations, was a stronger environmental
factor on reproductive success than sub-freezing tem-
peratures or summer storms. Oriantha exhibited plas-
ticity in responding to snow conditions by abandon-
ing ground-nesting and building their nests in elevated
sites when there was more snow, as opposed to Her-
mit Thrushes (Catharus guttatus) or Dark-eyed Juncos
(Junco hyemalis), which nested on the ground no
matter what the environmental conditions.
Morton’s study shows that challenges posed by en-
vironmental variation often can be met with existing
behavioural and physiological responses; adaptation
occurs through flexibility rather than through acqui-
sition of new abilities or mechanisms.
CynpI M. SMITH
Box 5, Waterton Park, Alberta TOK 2MO Canada
Seabird Bycatch: Trends, Roadblocks, and Solutions
Edited by Edward F. Melvin and Julia K. Parrish. 2001. Uni-
versity of Alaska Sea Grant AK-SG-01-01, Fairbanks,
Alaska. viii + 206 pages. U.S.$20.00.
The incidental catch of various water birds and other
aquatic organisms (e.g., turtles, sea otters, porpoises,
seals) in fishing nets has long been of concern to
naturalists for conservation reasons and to the fishing
industry for economic reasons. However, until recent-
ly this issue has been on the “back burner” compared
with more pressing and widespread environmental
problems. The advent of intensified fishing efforts,
huge factory ships, and collapsing fish stocks have
elevated this bycatch into both a major international
environmental issue and a serious economic problem.
This book, essentially the proceedings of a sympo-
sium, presents a recent update on the extent of the
problem in marine waters, world-wide, evaluations
of several proposed solutions as they apply to specific
fisheries and problems that have yet to be overcome.
The editors begin the book with a short preface that
outlines the history and extent of the problem, espe-
cially since it was identified as a major conservation
issue in the early 1970s. The first full chapter is a syn-
thesis, also by the editors, of a symposium organized
by the Pacific Seabird Group in Blaine, Washington,
in 1999. The synthesis summarizes the complexity of
the problem, “roadblocks” in the way of solving it and
guidelines to possible solutions. The remainder of the
book consists of nine peer-reviewed, scientific papers
(eight of which were presented at the symposium)
and seven abstracts. Two of the papers were reprinted
from recent (1999 and 2000) scientific journals. One
paper, by John Cooper, John Croxall and Kim Rivera
outlines the complexities of international efforts to re-
duce bycatch through research, local and international
regulations and cooperation among scientists, the fish-
ing industry and conservation groups. An afterword by
Craig Harrison graphically illustrates the complexity
of the problem by outlining the political and practical
difficulties of coordinating efforts to reduce bycatch
in the sockeye salmon fishery in the “shared waters”
of British Columbia and Washington, where two fed-
eral, one provincial and one state government share
jurisdiction with “21 Native American tribes” [a total
that applies only to Washington and omits the first
nations of British Columbia].
The rest of the papers and abstracts document the
extent of the bycatch in specific fisheries, results of
various experiments to reduce bycatch, and attempts
to measure the impact of specific fisheries on specific
populations of birds. As some seabirds spend non-
breeding times thousands of kilometers from their
breeding sites, measuring the effects of a specific fish-
ery on a particular breeding population is very diffi-
cult, especially as many seabirds are long-lived and
don’t breed every year. Moreover, fishing in a given
area may affect some species much more profoundly
than their close relatives (for example, effects of by-
catch on Black-footed Albatross populations are much
more significant than on Laysan Albatrosses) and may
affect different age groups differently (for example,
juvenile Black-footed Albatrosses are caught at a high-
er rate than adults). Research presented in this vol-
ume from the Atlantic, Pacific and Southern (Antarc-
286
tic) oceans shows that modifications to fishing gear
(weights, design, visual and acoustic alerts), timing
of fishing (daily and seasonally) and other techniques
can reduce bycatch substantially without substantially
reducing the take of target species, but that these mod-
ifications have different effects on the rate of bycatch
of different species and sometimes of a given species
in different areas, different times of the day or different
seasons. Banding continues to be helpful in sorting
out the origins of birds caught in specific fisheries,
while higher tech tracking devices and research on
genetic markers are also starting to improve our knowl-
edge of the complexities of movements by these highly
mobile species. Albatrosses receive the greatest amount
of attention, but data on various other “tubenoses,”
alcids, larids and some marine mammals are also pre-
sented.
Canadian content figures prominently in this book.
A 1972 paper by Canadian C. Eric Tull and co-authors
on the magnitude of Thick-billed Murre mortality in
Greenland fisheries is credited (page v) in drawing
attention to the significance of fisheries in seabird
population declines, and international legal efforts to
reduce bycatch in longlines stem from a resolution at
a 1996 meeting in Montreal of the World Conserva-
tion Congress of the World Conservation Union (page
11). Data from British Columbia are included in a
genetics (DNA) study of the breeding locations of
Common Murres entangled in fishing nets in Wash-
ington’s San Juan Islands and Puget Sound (pages
125-127) and in an abstract (pages 191-192) on sea-
bird avoidance experiments in northern Pacific waters.
Other papers and abstracts on observations and re-
search in Alaskan and Washington waters involve
populations of birds that spend portions of their lives
in British Columbian waters. Research from Atlantic
coast provinces and British Columbia are cited fre-
The Life of Mammals
By David Attenborough. 2002. Princeton University Press,
New Jersey. 320 pages, U.S.$29.95.
As the latest edition in the BBC “Life” series com-
bining television and print media, the book on mam-
mals is nicely illustrated with a good selection of
colour photographs that closely follows the engaging
text by David Attenborough as he presents interesting
stories on these fascinating animals. The first chapter,
“A Winning Design’, starts off with the ability of
mammals to adapt to different environments on earth,
including the harsh arctic conditions where lemmings
live year round. After describing some basic charac-
ters of mammals, such as hair and the production of
milk, there is a general introduction to the origin and
evolution of this group of warm-blooded organisms.
The chapter finishes off with two early mammalian
radiations that cover the egg-laying monotremes and
THE CANADIAN FIELD-NATURALIST
Vol. 118
quently.
This book provides a useful compilation of recent
developments on a complex issue, with plenty of in-
formation on legal (national and international)/poli-
tical aspects, recent research on seabird movements,
recent research on genetics of seabird populations, and
practical tests of various techniques under a variety of
conditions in a variety of waters. The literature cited
sections provide numerous additional references for
those requiring further information. The book should
be on the library shelves of any researchers, govern-
ment agencies and non-government conservation and
scientific organizations studying seabird biology and/
or the conservation of seabirds. Errors appear to be
few — the reference to Wilson et al. (1985) cited on
page 116 is not listed in that chapter’s literature cited
section, which includes two references that don’t appear
to have been cited. However, since most of tne chapters
are written as scientific papers, some may be too tech-
nical for some readers. The review by Cooper et al.
of legal and quasilegal aspects of the issue provides a
valuable reference compendium, but is so riddled with
acronyms that I found myself wishing for a glossary.
I also hope that the seven abstracts at the end of the
book are expanded into full papers somewhere. As
valuable a contribution as the book is in itself, this
volume will undoubtedly also stimulate more research
that will require another update before long. Such an
update could usefully also include papers or chapters
on aquatic bird bycatch of fisheries on inland waters,
such as those of the Great Lakes, several large prairie
province lakes and similar lakes on other continents.
MARTIN K. MCNICHOLL
4735 Canada Way, Burnaby, British Columbia V5G 1L3
Canada
the marsupials, which give birth to under-developed
young.
The remaining nine chapters deal with the placen-
tal eutherian mammals but instead of continuing to
describe them by scientific groups the format switches
to artificial categories such as diet and habitat. This
unnatural classification seems awkward at times with
bats, which people can readily identify with, split into
two separate chapters, “Insect Hunters” (curiously
including vampire bats) and “Life in the Trees” (al-
though some insect-eating bats also live in trees). There
was a missed opportunity to educate readers in scien-
tific classification and evolution while still entertaining
them with a plethora of amazing natural history stories.
Primates get star billing in the book with the last two
and a half chapters devoted to this charismatic order
of mammals. Although the higher-level taxonomy (or
common names employed) is not current, it begins
2004
_ with prosimians as an early branch of the primates.
The latest view is that this is not a natural group be-
cause, for example, tarsiers are more closely related
_to monkeys and apes, as alluded to but nonetheless
still included in the chapter with lemurs. The other
primates are grouped to cover the new and old world
_ monkeys, and ending with the gibbons and great apes,
including a branch for humans. The last half chapter
concentrates on both physical and social anthropology
from the first evidence of bipedal locomotion to cul-
tivation and civilization.
The book is definitely aimed at a general but knowl-
_ edgeable audience with an interest in nature and mam-
_mals. I am sure, however, that practising biologists
will still find a few facts new to them in their non-
specialist group because the background research is
_ relatively good. It was nice to see some recent scien-
tific hypotheses on mammalian evolution making it
into the book such as the close relationship between
BOOK REVIEWS
whales and hippopotamuses. But some other emerging
ideas based primarily on molecular data did not, in-
cluding the association of bats with carnivores, ungu-
lates and whales, as opposed to insectivores, or tree
shrews, flying lemurs and primates.
My criticisms are mostly biologically oriented be-
cause the book is attractively presented with most
photographs of good quality and information well writ-
ten. But there should be more books that combine
current scientific research with an explanation of the
deeper implications or processes involved for wider
distribution to the general public looking for mean-
ingful substance beyond the usual cursory facts.
BurRTON K. Lim
Centre for Biodiversity and Conservation Biology, Royal
Ontario Museum, 100 Queen’s Park, Toronto, Ontario M5S
2C6 Canada
_ Geographic Variation in Size and Shape of Savannah Sparrows (Passerculus sandwichensis)
_ By James D. Rising. 2001. Studies in Avian Biology Number
23. Cooper Ornithological Society, Camarillo, California.
65 pages. U.S.$7.
The newer field guides, such as The Sibley Guide to
Birds, occasionally describe and illustrate subspecies
of birds, usually based on differences in plumage or
_ soft parts. The “bander’s bible”, Peter Pyle’s Identi-
_ fication Guide to North American Birds, includes
wing and tail measurements to help banders identify
birds to the subspecies level — for example, he dis-
cusses 14 subspecies of the Savannah Sparrow. But
have you ever wondered why these differences exist
in the natural world?
Rising does and asks two questions in this regard:
Why do features such as body size, wing length, or bill
size and shape differ across a species’ range? and, if
these differences reflect adaptations to the different
environments to which the species is exposed, what
are the selective factors that have caused them?
One of the classic explanations for geographic vari-
ation in size is Bergmann’s Rule, which holds that
individuals of a species (vertebrates only) from colder
areas are generally larger-bodied than individuals from
warmer areas. Allen’s Rule takes this one step fur-
ther, stating that within such species, individuals from
colder areas will have smaller appendages relative to
their body size than individuals from warmer areas.
Rising asked his questions of the Savannah Spar-
row, which is one of the most wide-spread songbirds
in North America. He describes and quantifies geogra-
phic variation in the species throughout its breeding
range, from Alaska to the Maritimes to central Mexico,
and relates trends in phenotypic variation to environ-
mental variation.
He found some clinal variation in size of Savannah
Sparrows, with birds from the northeast being slightly
larger than those from the west, and birds in cool,
moist areas were larger than those where it is hot and
dry. But the species overall did not seem to follow
Bergmann’s Rule; rather, measures of summer tem-
perature and precipitation explained well the patterns
of size variation. His more significant find, though,
was that birds were larger on islands than on main-
land sites, whether in the Aleutian Islands, Alaska, or
on Sable Island, Nova Scotia. He speculates that the
long, cool, moist summers on these islands results in
a predictable and fairly rich food supply. This, com-
bined with the rather long breeding season, allows
multiple broods and perhaps enhanced competition
for high quality territories. This competition for either
food or territories might select for larger body size.
Rising ends with some taxonomic comments, com-
ing out on the side of the “lumpers’’. He sees no virtue
in naming subspecies where the only way they can be
reliably separated is by locality. He suggests recog-
nizing only two subspecies of non-saltmarsh Savannah
Sparrows, P. s. sandwichensis (large size) and P. s.
princeps (large and pallid), whereas the nine saltmarsh
subspecies seem to be clearly separable by morpho-
logical characters. This is in contrast to the 17 sub-
species currently recognized by the American Orni-
thologists’ Union.
Rising’s work relies on Principal Components and
Discriminant Functions analyses, which, although I
found it a little heavy going, was well presented sequen-
tially and a good example of the use of these techniques
for morphometric comparisons.
It will be interesting to watch in the coming years
how Rising’s thorough morphological studies interact
with genetic analyses in assessing variation and the sub-
species of Savannah Sparrows.
CyNnbDI M. SMITH
Box 5, Waterton Park, Alberta TOK 2MO Canada
288
THE CANADIAN FIELD-NATURALIST
Vol. 118
Warblers of the Great Lakes and Eastern North America
By Chris Early. 2003. Firefly Books Ltd., 3680 Victoria
Park Avenue, Toronto, Ontario, M2H 3K1. 131 + pages.
Cloth $24.95: paper $16.95
Sparrows and Finches of the Great Lakes and Eastern North America
By Chris Early. 2003. Firefly Books Ltd., 3680 Victoria
Park Avenue, Toronto, Ontario, M2H 3K1. 128 + pages.
Cloth $24.95: paper $.16.95
These books are an expansion and revision of two
earlier books by Chris Early (Warblers of Ontario and
Sparrows and Finches of Ontario). They both follow
the successful format of the earlier books. Each spe-
cies is shown in two to five photographs (Warblers)
or two to seven photographs (Sparrows). The actual
number of photographs for each species depends on
how variable the bird’s plumage can be. A short intro-
ductory note is followed by descriptions of the key
plumage characteristics and other relevant details. A
5 x 3 cm map of America shows the summer and
winter ranges.
“Warblers” covers 37 species plus one hybrid in
some detail. An additional seven vagrant species and
one race (the Yellow-rumped “Audubon’s” Warbler)
are covered by brief comments and a single accom-
panying photograph.
“Sparrows” includes 25 species covered in full and
20 vagrant species. In addition to the North American
sparrows (buntings) this volume includes longspurs,
finches, grosbeaks, crossbills, snow bunting and house
sparrow.
There are two features used by this author that will
make this book particularly valuable to beginners.
The first is called a cheat sheet and lists all the birds
in groups according to a key characteristic — such as
an unstreaked breast. The birds are further grouped
by a second characteristic such as a breast spot. The
second, and even better innovation, is a series of com-
Birds of the Yukon Territory
Edited by P. H. Sinclair, W. A. Nixon, C. D. Eckert and N.
L. Hughes. University of British Columbia Press, Van-
couver, British Columbia.
My appetite for a long-overdue return trip to the
Yukon has been incredibly whetted! This book is not
just an atlas, but also a coffee table book, a very use-
ful bird reference, and a source necessary for a
planning a trip to the Yukon. This book has stunning
photographs throughout, and not just of birds, but of
dramatic scenery (i.e., habitat shots) that will make
birders and non-birders alike think, “I must go there.”
Prior to the species accounts, there are chapters
covering the environment, aboriginal use of birds,
conservation, history and a month-by-month overview
of birdlife. There is also a short chapter outlining the
parison tables. These consist of a set of photographs
with birds in similar poses. The page is arranged to
show the most similar birds close together. For example,
there are three Common Redpoll photographs imme-
diately above three equivalent Hoary Redpoll photo-
graphs. Similarly, all the rufous-capped sparrows are
on one page. I think the arrangement of the warbler
comparison table is very clever. Here the Mourning
Warbler photograph is adjacent to a Connecticut War-
bler photograph. In turn, the Connecticut is above a
photograph of a Nashville Warbler, which in turn is
above a Northern Parula. All four birds share similar
combinations of colour and cause confusion to the
novice. This arrangement allows for easy compari-
son, either up and down or across the rows. For the
warblers there are tables showing the spring and fall
plumages. These features are on fold-out sheets at the
end of the book, making them quickly available in the
field. At the front of the book is a seasonal distribution
list for Point Pelee National Park. Using line thickness
the author also indicates the abundance of each species.
I find such distribution lists to be extremely useful.
These then are two small, portable books that deal
with birds that many find difficult to identify. The text
is well written. The photographs are both beautiful and
illustrative. Any one who needs help with the species
covered will find these books a tremendous help. Per-
haps we can encourage the author to write a third
book on shorebirds.
Roy JOHN
2193 Emard Crescent, Ontario, K1J 6K5 Canada
data management for the more than 160 000 records
that were used.
Each species account spans one to three pages. All
species are illustrated by a line drawing and at least
one, sometimes several, colour photographs; frequent-
ly, there is a very good habitat shot as well. Each
account also has a distribution map, and a histogram
outlining the number of database records for each
week of the year. The base layers of the maps show
major roads and rivers as well as ecozones; I would
have liked to see the dominant population centers
marked as well though.
The text is thorough and reads well. All the expect-
ed sections are there (distribution, nesting, habitat...),
and, where appropriate, a section on aboriginal use of
2004
the bird is included. Several appendices and a 600+
reference list end the book.
The items that bothered me were few, and mostly
minor. Noteworthy was the absence of birding essays,
a feature I first saw in Birds of Delaware, and thought
added spark to the thick reference book. Page numbers
were located in the most irritating choice possible,
along the inner margin of each page, thus not permit-
ting a rapid flip-through while searching through this
600 page book. The final, and dare I say incompre-
hensible feature of the book was the uninteresting and
out of focus (soft focus?) cover shot of the Territorial
bird, the Common Raven. People do judge a book by
BOTANY
BooK REVIEWS
289
its cover, rightly or wrongly, and in a book with hun-
dreds of stellar shots, I remain baffled as to why that
particular shot was chosen to be most people’s first
impression of the book.
Overall though, this is a very, very good book, and
a must-have for people interested in the birdlife of
the North.
RANDY LAUFF
Department of Biology, St. Francis Xavier University, Anti-
gonish, Nova Scotia B2G 2W5
Literature Cited
Hess, G. K., R. L. West, M. V. Barnhill I, and L. M. Fleming, 1999,
Birds of Delaware. University of Pittsburgh Press. 635 pages.
Wild Flowers of the Yukon, Alaska & Northwestern Canada, 2™ Edition
By John G. Trelawny. 2003. Harbour Publishing Co. Ltd.,
P.O. Box 219, Madeira Park, British Columbia VON 2HO
Canada. 224 pages. $24.95.
The first edition of this wild flower book was pub-
lished in 1983 and I reviewed it in 1984. The layout
in this new volume is much better. The type is larger
and more spaced on a purely white paper and is
wrapped around the absolutely beautiful colour pho-
tographs.
Many of the pictures of the 332 species treated are
the same as those in the first edition but the more
modern reproductions and paper have made them
shine. The descriptive text for each species has been
only slightly revised. The surrounding text includes
Acknowledgments, an easy-to-read map, an Introduc-
tion, an Illustrated Glossary, a Key to Species using
Flower Colour and Shape, Photo Credits, Bibliogra-
phy, an Index, and a list of Additional Field Guides
from Harbour Publishing. This is a most interesting
and delightful book for anyone living in, visiting or
planning to visit this wonderful area.
WILLIAM J. Coby
Biodiversity, Program on Environmental Health, Agriculture
and Agri-Food Canada, Wm. Saunders Building, Central
Experimental Farm, Ottawa, Ontario K1A 0C6 Canada.
Wild Flowers of Field & Slope in the Pacific Northwest
By Lewis J. Clark. 2002. Harbour Publishing, P.O. Box
219, Madeira Park, British Columbia VON 2HO. $9.95.
Wild Flowers of Forest & Woodland in the Pacific Northwest
By Lewis J. Clark. 2003. Harbour Publishing, P.O. Box
219, Madeira Park, British Columbia VON 2H0. $12.95
Wild Flowers of the Mountains in the Pacific Northwest
By Lewis J. Clark. 2003. Harbour Publishing, P.O. Box
219, Madeira Park, British Columbia VON 2HO0. $12.95.
These three books contain absolutely beautiful col-
our photographs. The photographs are numbered
sequentially and each one has a marker [x0.5] to in-
dicate its size. Each is accompanied by a printed para-
graph with the common and scientific names, a de-
tailed description, together with the habitat and range,
and a number to indicate its sequence in the book.
There are 108 in the first book, 100 in the second and
106 in the third.
There is a four- or five-page interesting introduction
at the front of each book and an index, glossary and a
list of Additional Field Guides available from Har-
bour Publishing at the end. There are most interest-
ing pictures on the front covers of each book. On the
back covers there is a note about the author, Dr. Lewis
J. Clark, together with a map of the Pacific Northwest
on which there are shaded areas depicting where the
wild flowers can be found. All are elegant.
WILLIAM J. Copy
Biodiversity, Program on Environmental Health, Agriculture
and Agri-Food Canada, Wm. Saunders Building, Central
Experimental Farm, Ottawa, Ontario K1A 0C6 Canada
290
MISCELLANEOUS
The Canoe: A Living Tradition
By John Jennings. Firefly Books, Toronto. 272 pages. $59.95.
There could hardly be a more poetic way to ex-
plore the natural world than by canoe. While not all
observers of natural history are canoeists, most canoe-
ists have respect for and curiosity about nature. In-
deed, a loon’s call or the slap of a beaver’s tail, accom-
panied by the quiet burbling of a canoe’s wake, has
served as an introduction to the contemplation of
nature for countless North Americans.
The Canoe: A Living Tradition is, in a sense, a nat-
ural history of traditional North American watercraft.
Included in this beautifully illustrated, coffee table-
sized book are chapters dedicated to the history and
construction of birch bark and dugout canoes, as well
as skin kayaks and umiaks (large, open vessels from
the Canadian Arctic). This book also discusses the
influence of canoes on the fur trade and the settlement
of northern North America, as well as the develop-
ment of recreational canoes and the preservation of
canoe history in more recent times. A respected expert
writes each chapter on the type of craft or historical
context being discussed. This makes for inconsistent
writing at times, but also gives the book an authority
that would not have been achieved by a single author.
I found that the technical details about the dimen-
sions (i.e., width and length, etc.) of canoes a bit repet-
itive. On the other hand, the documentation of these
measurements may be valuable in the future. As John
Jennings notes in the first chapter, the original canoe
designs of several First Nations in North America have
been erased without a trace, a poignant reminder of
the terrible loss of traditional knowledge that contin-
ues to this day.
While the book brilliantly covers the historical
context of canoeing and canoe building (over the
span of 230 pages), it pays scant attention to modern
uses of the canoe (2 pages). After all, as the title sug-
gests, canoeing and canoe building is a “living tradi-
THE CANADIAN FIELD-NATURALIST
Vol. 118
tion’. Canoeing is still one of the most elegant ways to
explore nature and there are many fine canoe builders
in North America currently manufacturing modern
and traditional canoes from a wide range of natural
and synthetic materials. It seems as though a chapter
could have been devoted to recent developments in
the design and construction of modern canoes.
The book gives a good overview of how birch bark
and dugout canoes are constructed, including useful
photographic illustrations; however, before you run
out and start assembling materials, take heed: the
information provided is insufficient for the “do it your-
self’ canoe builder. A noticeable shortcoming is the
omission of information about the many resources
available to those interested in building traditional
birch bark and dugout canoes, as well as skin kayaks.
For instance, while the book contains a photograph
of a canoe built by César Nawashish, it fails to refer-
ence the excellent 1971 National Film Board film
“César’s Bark Canoe”, which documents Nawashish’s
completion of a bark canoe with exquisite detail.
Other contemporary builders of traditional craft have
also produced thorough “how to” publications on
building birch bark canoes and skin kayaks including
David Gidmark, Robert Morris and Wolfgang Brink,
which have not been referenced in this book.
While Adney and Chapelle’s Bark Canoes and
Skin Boats of North America will remain the bible of
traditional canoe and kayak design, The Canoe: A
Living Tradition is broader (literally and figuratively),
more colourful and more accessible. It is simply irre-
sistible for the canoe enthusiast. Its shortcomings are
few and its design and production qualities are excel-
lent. In summary, it is a valuable addition to the annals
of canoe culture. Congratulations to John Jennings
and the Canadian Canoe Museum for their fine work.
PATRICK WILLISTON
41 Nielson Road, Smithers, British Columbia VOJ 2N2 Canada
A Passion for Wildlife: The History of the Canadian Wildlife Service
By J. A. Burnett. UBC Press, Vancouver, British Columbia.
Hardcover. 331 pages, $27.95 paper, $85.00 cloth.
Anyone who is prejudiced against “civil servants”
should read this book. The Canadian Wildlife Service,
from its inception, has contained a cadre of dedicated
scientists who work long hours, share their knowledge
widely, and on occasion risk their lives for the sake
of the environment. Burnett, an insider, tells the story
of this valuable and generally cost-effective organiza-
tion, beginning in 1916 with the five men who were
involved in drafting and implementing, from the
Canadian side, the Migratory Birds Convention Act.
In 1918, Hoyes Lloyd was appointed as Supervisor
of Wild Life Protection in Canada. Lloyd, in turn,
appointed three Federal Migratory Bird Officers. The
Dominion Wildlife Service (now the Canadian Wild-
life Service or CWS) was founded on | November
1947.
Burnett follows a roughly chronological sequence,
with 67 photographs. His writing skills introduce us
to many interesting scientists and their achievements,
without the inevitable plethora of names becoming
objectionable. The footnotes list the main publica-
tions that resulted from extensive research. He covers
objectively the lowest point in CWS history, the short
but destructive reign of Suzanne Blais-Grenier as
federal Minister of the Environment.
2004
This excellent history will be of interest to most
ornithologists, mammalogists and environmentalists,
and will be a useful reference in every major library.
However, I must admit to being flabbergasted by
the publication of this book by a reputable university
press, without any mention, let alone acknowledge-
ment, of the previous publication, with the identical
title, and with 99 per cent of the text which filled one
issue of The Canadian Field-Naturalist 113:1-214,
January-March 1999. Readers of this journal do not
need to buy the book; they already have a soft-cover
version on their shelves.
What does the new version offer as compared to
the unmentioned and unacknowledged version? An
appropriate foreword by Janet Foster and a few new
photographs have been added, but most are unchanged
except that their quality has been improved and some
have increased in size. Additions have been made to
the following sub-chapters: “Seabirds,” a paragraph
about Tony Gaston’s work on the Ancient Murrelet;
“Shorebirds,” two paragraphs on the Latin American
cooperation in shorebird banding and mention of the
Kees Vermeer Award now presented annually at Simon
Fraser University; “Habitat Management,’ a paragraph
on the purchase of Westham Island in the Fraser
River delta; “Consolidation,” two new paragraphs on
wildlife policy changes; “Peregrine Falcon,” Richard
Fyfe’s investiture into the Order of Canada on 26
April 2000; “Species Protection,’ a paragraph on the
delays and rocky road of Bill C-5, the Canada Species
at Risk Act, which finally passed on 11 June 2002;
“A Work in Progress,” four sentences of reminiscences
Birding on Borrowed Time
By Phoebe Snetsinger. 2003. ABA Inc. Box 6599, Colorado
Springs, Colorado. 307 pages. Paper US$19.19.
I never met Phoebe Snetsinger. In fact I have only a
vague recollection of hearing her name. I was sur-
prised at her sudden prominence after she died. Now
I have read her book and I understand.
I expected someone who saw over 8000 species to
be the typical “combat “ birder; a person who relishes
getting the tick on her checklist above everything
else. Phoebe Snetsinger was not a combat birder; she
was a true birdwatcher. She insisted on really seeing
and recording the birds she counted. She did not in-
clude those flits that zip into view for an instant and
are identified by the local guide. I have seen combat
birders joyfully tick off such birds on their list and
immediately move rapidly on in search of their next
“lifer.” Indeed the author did not seem to be truly
competitive until after her 7000" bird species and in
line for the Guinness Book of Records. She ceased
being competitive after achieving the world record at
her 8000" species of bird.
Her book is the account of her travels in accumu-
lating this incredible total, and the joy she had in see-
BOOK REVIEWS
29]
by Rob Butler. The title of Chapter 5 has been im-
proved from “Policy Implementation” to “Emergence
of Environment Canada.” A few small editorial im-
provements are evident, such as a change from “at the
same time that” to “even as.” Otherwise the two ver-
sions are almost word for word and paragraph for para-
graph in the text and word for word in the index. Sadly,
an opportunity to index each annual wildlife conference
was not seized.
What has been deleted? A short biography of the
author, Sandy Burnett; a short afterword by editor,
Francis Cook, explaining the contributions to editing
of the Canadian Field-Naturalist made by Harrison
F. Lewis, C. H. D. Clarke, and A. J. Erskine; and a
useful 31-page bibliography of major publications by
CWS personnel, compiled by Erskine.
The Canadian Field-Naturalist exists to record
and spread information of value, and contains a clear
statement that copyright for this particular paper re-
sides with “Her Majesty the Queen in Right of Canada”
as stated in 113(1). However, I remain surprised that
the author and the publisher appear, consciously or
unconsciously, to have chosen to withhold information
about this material having previously appeared in the
very scientific journal: in which this review is now
appearing.
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N OJ8
Canada 3
Copies of CFN 113(1) are available for $10.00 from the
Business Manager.
ing all of these birds. She was a focused, energetic and
hardworking individual who took her birdwatching
extremely seriously. She studied her target species long
before trying to see them. She kept copious notes on
what she saw. I agree with this approach and try to
use it myself. I do not understand why people pay so
much money and effort to go to a prime nature locale,
yet do not do their homework.
Spurred into action by the threat of cancer and the
potential to die young, Phoebe Snetsinger began a life
of traveling for birds. In the process she made numer-
ous friends in over 60 countries. I estimate she did ten
to a dozen trips a year and spent about U.S.$50 000/
year in today’s currency. Overall, she must have made
hundreds of trips.
A neat bonus is the group of 29 black-and-white
and 16 colour illustrations by Douglas Pratt. They por-
tray the key milestone birds of Phoebe’s impressive
odyssey. They are well done and make a nice coun-
terpoint to the text.
This is certainly a book for all birders. However, it
is not simply a long list of birds seen, but a rampag-
ing account of Phoebe’s obsession. This lady survived
297
gang rape, robbery, accidents, family crises, mechani-
cal breakdowns, bad service and bad food against a
background threat of cancer. Nothing seemed to slow
her down. It is a tale of the fortitude of the human
spirit. Indeed, I think a revision of this with the birding-
related material severely edited (after all, which non-
birder will realize the importance of a Red-shouldered
Vanga — a small, House Sparrow-sized grey, black-
and-white bird with bright chestnut shoulders — and
New TITLES
Zoology
+The American Bison. By D. Lott. 2004. University of
California Press. 229 pages, $40 U.S. Paper.
+ Annotated Bibliography of the Quaternary Vertebrates
of Northern North America. 2003. Edited by C. R. Harring-
ton. University of Toronto Press. xxii plus 539 pages, not
illustrated. $150 Cloth, $75. Paper.
Annotated Checklist of the Birds of Chile. By Manuel
Marin. Lynx Edicions, Barcelona, Spain. US$15.75.
Behavior and Ecology of Pacific Salmon and Trout. By
T. Quinn. UBC Press, 2029 West Mall, Vancouver, British
Columbia V6T 1Z2 Canada. 400 pages, $85.
Big Cat Diary: Leopard. By Jonathan Scott and Angela
Scott. Harper Collins. 128 pages, $42.
* The Bird Almanac. By D. Bird. 2004. Key Porter Books,
70 The Esplanade, Toronto, Ontario, Canada. xvii + 460
pages, not illustrated, $24.95. Paper.
Birding in Venezuela. By Mary Lou Goodwin. Lynx Edi-
cions, Barcelona, Spain. US$ 5.60.
Birds of South Asia: The Ripley Guide. Volumes I and II.
By Pamela C. Rasmussen and John C. Anderton. Lynx Edi-
cions, Barcelona, Spain. US$95.
Bowerbirds — Ptilonorhychidae. Edited by Clifford Frith.
Oxford University Press, 70 Wynford Drive, Don Mills,
Ontario M3C 1J9 Canada. 416 pages. $209 Cloth.
+ British Columbia - A Natural History. By R. and S.
Cannings. 2004. Greystone Books, Douglas and McIntyre,
Vancouver, British Columbia, Canada. ix + 341 pages.
$39.95 Paper.
+ The Buffalo Wolf. 2003. By Lu Carbyn. Smithsonian
books, Washington, D.C., USA. 248 pages. Paper.
Curassows and Related Birds. By Jean Delacour and Dean
Amadon. Update Chapter by Josep del Hoyo and Anna
Motis. Illustrated by Albert Earl Gilbert. Lynx Edicions,
Barcelona, Spain. US$75.
7 Ecology and Conservation of Birds in the Salton Sink:
an Endangered Ecosystem. By W. David Shuford and Kathy
C. Molina. 2004. Studies in Avian Biology Number 27.
Cooper Ornithological Society.
THE CANADIAN FIELD-NATURALIST
Vol. 118
its ilk?) would make it ideal for one of those inspira-
tional stories we find in Reader’s Digest. Having final-
ly seen a Red-shouldered Vanga, Phoebe was asleep in
the tour bus when the bus crashed and she was killed.
So she did not die of cancer, but binoculars in hand,
on a birding trip. I never did meet this lady — pity!
Roy JOHN
2193 Emard Crescent, Ottawa, Ontario K1J 6K5 Canada
* A Field Guide to the Bird’s Nests and Eggs of Alaska
Coastal Tundra. By T. Bowman. 2004. Alaska Sea Grant
College Program.
+ A Guide to Hawk Watching in NA. By D. Heintzleman.
2004. The Globe Pequot Press.
+ Mammal Tracks and Signs. By Mark Elbroch. 2004.
Stackpole Books.
+ Key Marine Habitat Sites for Migratory Birds in Nuna-
vut and the Northwest Territories. 2004. By M. Mallory
and A. Fontaine. 2004. Canadian Wildlife Service, Ottawa,
Ontario K1A OH3. Paper.
7 Orca — Visions of the Killer Whale. By P. Knudtson.
2004. Greystone Books, Vancouver, British Columbia. xvii
+110 pages. $19.95. Paper.
Readers Digest Birds of Canada. Edited by R. Greenberg
et al. 2004. Dorling Kindersly India Ltd., c/o Tourmaline
Editions, 662 King Street West, Suite 304, Toronto, Ontario
MSV 1M7.
Reptiles and Amphibians of the Amazon: An Ecotourist’s
Guide. By R. D. Bartlett and P. Bartlett Florida University
Presses, USA. 291 pages. $57 Canadian. Paper.
Wild Down Under: The Natural History of Australasia.
By Neil Nightingale, Jeni Clevers, Neil Pearson and Mary
Summerill. BBC Video. 240 pages, $50 Canadian. Cloth.
Botany
The Wild Flowers of Britain and Ireland — The Complete
Guide to the British and Irish Flora. By Marjorie Blamey,
Richard Fitter and Alastair Fitter. A & C Black. 512 pages,
$42 Canadian. Paper.
Environment
*Bull’s Eye — Unraveling the medical mystery of Lyme
Disease. By Jonathon Edlow. 2004. Yale University Press,
Box 209040, New Haven, Connecticut.
+ Canoeing, Kayaking & Hiking Temagami. By Hap Wil-
son. 2004. The Boston Mills Press (Firefly Books), 132 Main
Street, Erin, Ontario. 112 pages, $24.95.
+ Chicken Soup for the Fisherman’s Soul. By J. Canfield,
M. Hansen, K. & Dahlynn McKowen. 2004. Health Com-
munications Inc. Paper.
2004
Dictionary of Ecology. By Michael Allaby. 2004. Oxford
University Press, 70 Wynford Drive, Don Mills, Ontario
M3C 1J9. 448 pages, $29.95.
+ The Importance of Species. Edited by P. Karliva and S.
Levin. 2004. Princeton University Press, 41 William Street,
Princeton, New Jersey. xvi + 427 pages, not illustrated, Paper.
+ Lewis and Clarke on the Great Plains. By Paul Johns-
gard. 2003. University of Nebraska Press. xiv + 143 pages,
$14.95 U.S.
+ Missinaibi. By Hap Wilson. 2004. The Boston Mills Press
(Firefly Books), 132 Main Street, Erin, Ontario. 134 pages,
$24.95.
+ A place between the tides: A naturalist’s reflections on
the salt marsh. By Harry Thurston. 2004. Greystone Books.
Paper. $22.95 CAAD, $15.00 U.S.
+ Politics of the Wild - Canada & Endangered Species.
Edited by K. Beazley and R. Boardman. 2004. Oxford Uni-
versity Press, 70 Wynford Drive, Don Mills, Ontario. x +
254 pages, not illustrated, $29.95 Paper.
Population Ecology: First Principles. By John H. Vander-
meer and Deborah E. Goldberg. Princeton UP, USA. 280
pages, $123 Cdn, Cloth.
A Primer of Ecological Genetics. By J. Conner and D. Hartt.
2004. Sinauer Associates, Box 407, Sunderland, Massachu-
setts. 207 pages, $34.95 U.S., Paper.
BOOK REVIEWS
293
* Resource and Environmental Management in Canada.
Edited by B. Mitchell. 2004. Oxford University Press, 70
Wynford Drive, Don Mills, Ontario. x + 600 pages, $29.95
Paper.
+ Rivers of the Upper Ottawa Valley. By Hap Wilson. 2004.
The Boston Mills Press (Firefly Books), 132 Main Street,
Erin, Ontario. 112 pages, $24.95.
+ The Selbourne Pioneer. By T. Dodswell. 2004. Ashgate
Publising Company, Suite 420, 101 Cherry St., Burlington,
Vermont, USA. xvii + 238 pages, not illustrated. Paper.
+ Shaped by the West Wind — Nature and History in
Georgian Bay. By C. Campbell. 2004. UBC Press, 2029
West Mall, Vancouver, British Columbia, V6T 172 Canada.
256 pages, $85 Cdn.
The Smithsonian Atlas of the Amazon. By Michael Gould-
ing, Ronaldo Barthem and Efrem Ferreira. Smithsonian
Books, Washington, D.C., USA. 255 pages, $75 Cdn. Cloth.
+ Teaching in Eden. 2003. By J. Janovy Jr. Routledge, 29
West 35th St., New York, New York 10001 USA. 187 pages,
not illustrated, $22.95 U.S., Paper.
+ Wilderness Rivers of Manitoba. By Hap Wilson and S.
Aykroyd. 2004. The Boston Mills Press (Firefly Books),
132 Main Street, Erin, Ontario, Canada. 112 pages, $24.95.
+ Available
* Assigned
News and Comment
Update on Quebec Amphibian and Reptile Atlas Project: Rana-Saura 6(2)
The newsletter Rana-Saura resumes with Volume 6, Num-
ber 2 issued for April 2004. The previous issue was published
in March 2000. Due to translation expense no English ver-
sion is currently available of the new issue (of 383 participants,
only 23 are anglophones). Contents are: Et ¢a continue! —
Atlas des amphibiens et des reptiles du Québec — Suivi des
populations d’amphibiens du Québec — La présence de la Rai-
nette faux-grillon boreale [Pseudarcris maculata] enfin con-
firmée [Jean-Francois Desroches] — Un nouvelle reptile pour
Québec! [Jean-Fran¢ois Desroches] — Le tout nouveau guide
d’identification des amphibiens et des reptiles du Québec!
Rana-Saura is edited by David Rodrigue, for the Atlas of
amphibians and reptiles of Quebec (continuing in 2004 in its
17" year; since 2002 the entries have increased from 22 000
to nearly 45 000) and the Survey of populations of amphibians
of Quebec (in 2004 there will be 45 participants conducting
42 road surveys). These projects are coordinated by the Eco-
musuem of the St. Lawrence Valley Natural History Society
and financially aided by La Sociéte de la Faune et des Parcs
du Québec.
It is distributed by St. Lawrence Valley Natural History
Society, 21-125 chemin Sainte-Marie, Sainte-Anne-de-Belle-
vue, Quebec H9X 3Y7 Canada. Phone (514) 457-9449,
extension 105: Fax (514) 457-0769; e-mail: ecomus @total.net.
Froglog: Newsletter of the Declining Amphibian Populations Task Force (62)
Number 62, April 2004. Contents: Southern African Frog
Atlas Project completed! (Marius Burger and J. A. Harrison)
— Mark Twain’s frog not croaked after all! (Robert Stack) —
Decline of the Kihansi Spray Toad, Nectophrynoides asper-
ginis from the Udzungwa Mountains, Tanzania (Che Weldon
& Louis H. du Preez) — The Amphibian Fauna of Nagaland,
India: Species and Habitats (Meren Ao & Sabitry Bordoloi)
— Seed Grant News — Froglog Shorts.
Froglog is the bi-monthly newsletter of the Declining Am-
phibian Populations Task Force of The World Conservation
Union (IUCN)/Species Survival Commission (SSC) and is
supported by The Open University, The World Congress of
Herpetology, and Arizona State University. The newsletter
is edited by John W. Wilkinson, Department of Biological
Sciences, The Open University, Walton Hall, Milton Keynes,
MK7 6AA, United Kingdom; e-mail: daptf@open.ac.uk.
Funding for Froglog is underwritten by the Detroit Zoo-
logical Institute, P. O. Box 39, Royal Oak, Michigan 48068-
0039, USA. Publication of issue 62 was also supported by
Peace Frogs www.peacefrogs.com and by RANA and the U.S.
National Science Foundation grant DEB-0130273.
Amphipacifica: Journal of Aquatic Systematic Biology 3(4)
Volume 3, Number 4, dated 30 March 2004, is 113 pages
and contains the talitroidean amphipod family Najnidae in
the North Pacific region: systematics and distributional ecol-
ogy (E. L. Bousfield and Pierre Marcoux) and The amphi-
pod family Pleustidae (mainly subfamilies Mesopleustinae.
Neopleustinae, and Stenopleustinae) from the Pacific coast
of North America: systematics and distributional ecology
Marine Turtle Newsletter (104)
April 2004. 36 pages: ARTICLES: Nesting of Hawksbill
Turtles in Paraiba-Brazil: Avoiding Light Pollution Effects
— Stranding of Small Juvenile Leatherback Turtle in West-
ern Australia — Post-nesting Movements of Green Turtles
Tagged in the Turtle Islands, Tawi-Tawi, Philippines — Notes
from Preliminary Market Surveys in Morocco — NOTES:
Recoveries of Two Post-hatching Loggerhead Turtles in the
Northern Adriatic Sea — Green Turtle Nesting on the Gulf of
Oman Coastline of the Islamic Republic of Iran — Confirmed
Nesting of the Loggerhead Turtle in Corsica — Marine Tur-
tles in Iran: Results from 2002 — Sightings of the Leatherback
Turtle off the Southern Coast of Rio de Janeiro, Brazil —
(E. A. Hendrycks and E. L. Bousfield).
Amphipacifica (ISSN 1189-9905) is published quarterly by
Amphipacifica Research Publications, Edward L. Bousfield,
Managing Editor, 1710-1275 Richmond Road, Ottawa, On-
tario K2B 8E3 Canada. Annual subscription rates are $40.00
US or $50.00 Canadian funds. Back numbers are available
at $10 each.
MEETING REPORTS — IUCN/SSC MTSG News — BOOK REVIEWS
— ANNOUNCEMENTS NEWS & LEGAL BRIEFS — RECENT PUBLI-
CATIONS.
The Marine Turtle Newsletter is edited by Brendan J.
Godley and Annette C. Broderick, Marine Turtle Research
Group, School of Biological Sciences, University of Exeter,
Exeter EX4 4PS United Kingdom; e-mail MTN @seaturtle.
org; Fax +44 1392 263700. Subscriptions and donations to-
wards the production of both the MTN and its Spanish edi-
tion NTM [Noticiero de Tortugas Marinas] should be made
online at www.seaturtle.org/mtn or c/o SEATURTLE.ORG
11400 Classical Lane, Silver Spring, Maryland 20901 USA.
294
2004 THE CANADIAN FIELD-NATURALIST 295
Erratum 118(1): 80
Sloan, N. A., and P. M. Garier. 2004. Introduced marine species in the Haida Gwaii (Queen Charlotte Islands) Region, British
Columbia. Canadian Field-Naturalist 118(1): 77-84.
Langara Island
7 Parry Passage
Cryptosula pallasiana He Rose
Limnodrilus monothecus | Masset Spit
/ Delkatla
/ ;
/ ® Pelonaia corrugata
/ Inlet
Heh Ve
~ Trechus obtusus
Limnodrilus monothecus
om
Cryptosula pallasiana . a a x
\
xe Kumdis Bay
\ Yakoun Bay
Graham
Rennell Sound o Island
: Hecate
Skidegate he
Inlet
A
Moresby
‘ Island
Cartwright
Sound
Tasu
Sound
Bowerbankia gracilis
Hotspring
Ciona intestinalis Island
Legend STUNG a
a Sargassum muticum
Dolomite "Burnaby"
Narrows
O Mya arenaria
Qo oe
A
Harriet
© Ampithoe vallida
@ Other invertebrate sightings as noted B Harbour
pl ceeeen eels
at
5a
Bowerbankia gracilis ~~ —
nt Houston Stewart
Channel
Schizoporella unicornis ®
Tubularia crocea/
131°W
FicureE |. Map of Haida Gwaii showing locations mentioned in the text and collection sites of introduced marine plant and
invertebrate species, based on data from Sloan and Bartier (2000) and Sloan et al. (2001).
Editor’s Report for Volume 117 (2003)
Mailing dates for issues in volume 117 were: (1)
30 September 2003, (2) 23 March 2004, (3) 12 July
2004, (4) 16 September 2004.
A summary of membership and subscriber totals
2003 is given in Table 1. The number of articles and
notes in volume 117 is summarized in Table 2 by topic;
totals for Book Reviews and New Titles are given in
Table 3, and the distribution of content by page totals
per issue in Table 4. Council continued contribution of
40% of membership dues for publication. All of sub-
scriptions (both individual and institutional) also go
toward publication. As well, the Council allocated 80%
of the annual interest from the Manning Fund and
other capital funds to The Canadian Field-Naturalist.
The Manning fund portion is specifically to offset the
publication cost of northern papers where author and
institutional contributions were insufficient to cover
page charges.
Emil Holst arranged setting and printing at St. Joseph
Print Group, Ottawa, for 117(1), with special thanks due
Cameron Fraser and Willy Silfwerbrand, and at Gilmore
Printers, Ottawa, for 117 (2,3,4) with special thanks to
Wendy Cotie and Ally Reckzin. Leslie Cody prepared
the Index, Elizabeth Morton read the galleys. Bill
Cody as Business Manager handled all reprint requests
and charges and oversaw and proofed the compilation
of the Index. Wilson Eedy continued as Book-Review
Editor until his death in June, and Roy John replaced
him in August 2004.
Manuscripts (excluding book reviews, notices, and
reports) submitted to The Canadian Field-Naturalist
totalled 84 in 2003, down 16 from 100 in 2002. The
following reviewed for papers submitted in 2003: Asso-
ciate Editors: (number of manuscripts reviewed in par-
entheses): R. Anderson, Canadian Museum of Nature,
Ottawa (5): C. D. Bird, Erskine, Alberta (14); B. W.
TABLE 2. Number of articles and notes published in The Cana-
dian Field-Naturalist Volume 117 (2003) by major field of
study.
Subject Articles Notes Total
Mammals 19 * 14 33
Birds Lie 6 23
Amphibians + reptiles 4 1 BD)
Fish 3 D. 5
Invertebrates 6 1 6
Plants** 16 3 19
Tributes 2 0 2
Totals 67 27 93
*one article counted twice, one in each group: **includes one
feature article.
Coad, Canadian Museum of Nature, Ottawa (10); R.
R. Campbell, St. Albert, Ontario (6); P. M. Catling,
Agriculture and Agri-food Canada, Ottawa (11); A. J.
Erskine, CWS, Sackville, New Brunswick (13); D. F.
McAlpine, New Brunswick Museum, Saint John, N.B.
(8); D. W. Nagorsen, Victoria, British Columbia (11);
W. O. Pruitt, Jr., University of Manitoba, Winnipeg (21);
Others: (one review each except as marked): P. Achuff,
Waterton National Park, Alberta; Y. Alarie, Laurentian
University, Sudbury, Ontario; N. Alfonso, Canadian
Museum of Nature, Ottawa, Ontario; J. F Bain, Uni-
versity of Lethbridge, Alberta; R. Bird, Cascadia Re-
search, Olympia, Washington; K. Bellamy, OMNR,
Peterborough; J. R. Bider, Ecomuseum, Ste-Anne-de-
Bellevue, Quebec (3); E. L. Bousfield, Ottawa, On-
tario; J. P. Bogart, University of Guelph, Ontario; I.
Brodo, Canadian Museum of Nature, Ottawa, Ontario
(2); R. J. Brooks, University of Guelph, Ontario; J.
Calambokidis, Cascadia Research, Olympia, Washing-
ton; S. E. Campana, Bedford Institute of Oceanography,
TABLE |. The 2003 circulation of The Canadian Field-Naturalist (2002 in parenthesis). Totals compiled by W. J. Cody. Forty
percent of membership dues and 100% of subscriptions go to publication of The Canadian Field-Naturalist. Members vote
on Club affairs, subscribers and institutions do not.
Canada USA Other Totals
Memberships
Family & individual E, (OMI) 36) G2) 7 (8) 838 (951)
Subscriptions
Individuals 163 (164) 60 (65) 6 (5) 229° (234)
Institutions lesa — is(GuZAl)) 241 (252) 307762) 428 (455)
Totals 1005 (1246) 337 (349) 43 (45) 1495 (1640)
Note: 22 countries are included under “Other” (outside Canada and United States): Austria, Belgium, Brazil, Denmark (2),
United Kingdom (9: including | to Scotland), Finland (2), France (3: including | to St. Pierre & Miquelon), Germany (2),
Iceland, Ireland, Japan, Mexico, Netherlands (3), New Zealand, Norway (4), Poland, Russia, South Africa, Spain (3),
Sweden (2), Switzerland (2), Trinidad and Tobago.
296
2003
TABLE 3. Number of reviews and new titles published in Book
Review section of The Canadian Field-Naturalist Volume
117 by topic.
Reviews New Titles
Zoology 40 30
Botany 11 23
Environment 22 4]
Miscellaneous 12 18
Young Naturalists 0 18
Totals 85 130
Dartmouth, Nova Scotia; L. Carbyn, Canadian Wild-
life Service, Edmonton, Alberta (4); A. Ceska, Victoria,
British Columbia; A. H. Clarke, Jr., Portland, Texas;
W. J. Cody, Agriculture and Agri-food Canada, Ottawa;
V. Craig, EcoLogic Research, Gabriola Island, British
Columbia; M. Crete, Ministere de 1’ Environnement et
de la Faune, Quebec; E. J. Crossman, Royal Ontario
Museum, Toronto, Ontario; S. J. Darbyshire, Agriculture
and Agri-food Canada, Ottawa; R. Day, Canadian
Museum of Nature, Ottawa; C. Ely, U. S. Fish and
Wildlife Service, Anchorage, Alaska; M. Engstrom,
Royal Ontario Museum, Toronto; B. Erickson, Salon.
Ohio; M. Fairbarns, Conservation Data Centre, B. C.
Government, Victoria; M. Gosselin, Canadian Museum
of Nature, Ottawa; T. Goward, Clearwater, British
Columbia; W. A. Fuller, Athabasca University, Alberta;
D. Galbraith, Royal Botanical Gardens, Hamilton,
Ontario; Marco Festa-Bianchet, University of Sher-
brooke, Quebec; P. T. Gregory, University of Victoria,
British Columbia (2); D. Gummer, Provincial Museum
of Alberta, Edmonton (2); E. Haber, National Botani-
cal Services, Ottawa; F. Harrington, Mt. St. Vincent
University, Halifax, Nova Scotia; R. Harrington, Cana-
dian Museum of Nature, Ottawa; D. Henry. Parks
Canada, Haines Junction, Yukon Territory; S. Herrero,
University of Calgary, Alberta; G. V. Hilderbrand,
Alaska Department of Fish and Game, Anchorage; R.
P. Hodge, Gig Harbor, Washington; C. S. Houston,
Saskatoon, Saskatchewan (2); E. Holm, Royal Ontario
Museum, Toronto; G. Jarrell, University of Alaska
Museum, Fairbanks, Alaska; D. Johnson, Canadian
Forest Service, Edmonton, Alberta; N. Jotham, NRJ
Technical Services, Trade & Animal Welfare, Ottawa:
R. B. King, Northern Illinois University, DeKalb, Illi-
nois; J. L. Koprowski, Wildlife and Fisheries Resources,
University of Arizona, Tucson; S. Lariviere, Delta
Waterfowl Foundation, Portage La Prairie, Manitoba;
D. Larson, Memorial University of Newfoundland,
St. John’s; L. E. Licht, York University, North York,
Ontario; J. Lien, Memorial University of Newfound-
land, St. John’s; S. Lindgren, University of Northern
British Columbia, Prince George; G. L. Mackie, Uni-
versity of Guelph, Ontario; F. F. Mallory, Laurentian
University, Sudbury, Ontario; A. Martel, Canadian
EDITOR’S REPORT
297
TABLE 4. Number of pages per section published in The
Canadian Field-Naturalist Volume 117 (2003) by issue.
(1) (2) (3) (4) Total
Articles WAI SB) 109 119 490
Notes 12 16 15 17 60
Tributes 1] 0 16 (0) Dil,
Book Reviews’ 13 25 26 18 82
CFN/OFNC Reports x 0 2 8 212.
News and Comment 3 2 | 2 8
Index 0) 0 0 30 30
Advice to Contributors 0 0 | 0 |
Totals 166 180 176 188 710
*Total pages for book review section include both reviews
and new titles listings.
**Includes CFN Editors reports (issue 2), OFNC Annual
Business Meeting (3) and OFNC Awards (4).
Museum of Nature, Ottawa; John Maunder, New-
foundland Museum, St. John’s, Newfoundland; M. K.
McNicholl, Burnaby, British Columbia; G. R. Miche-
ner, University of Lethbridge, Alberta; G. Mulligan,
Agriculture and Agri-food Canada, Ottawa; E. Nol,
Trent University, Peterbourgh; P. Paquet, Meacham,
Saskatchewan; K. Prior, Canadian Wildlife Service,
Ottawa; G. Proulx, Alpha Research & Management
Ltd., Sherwood Park, Alberta; C. Renaud, Canadian
Museum of Nature, Ottawa, Ontario; B. Riddell, Paci-
fic Biological Station, Nainimo, British Columbia; R.
A. Ring, University of Victoria, British Columbia;
James Schaefer, Trent University. Peterborough, On-
tario; W. B. Schofield, University of British Columbia,
Vancouver; F. W. Schueler, Oxford Station, Ontario;
B. Slough, Whitehorse, Yukon Territory; I. Stirling,
Canadian Wildlife Service, Edmonton, Alberta (2); J.
Straley, University of Alaska Southeast, Sitka, Alaska;
D. Strickland, Dwight, Ontario; E. S. Telfer, Edmon-
ton, Alberta; I. Thompson, Canadian Forest Service,
Sault Ste. Marie, Ontario; C. Traynor, Ottawa, Ontario;
N. Vachon, Sociéte de la faune et des parcs du Québec,
Longueuil; P. Weigl, Wake Forest University, Winston-
Salem, North Carolina; G. Wobeser, Western College
Veterinary Medicine, University of Saskatchewan, Sas-
katoon; J. N. Womble, University of Alaska-Fairbanks,
Juneau, Alaska; P. M. Youngman, Ottawa, Ontario (2).
I am also indebted to the President of the Ottawa
Field-Naturalists’ Club Gary McNulty and the Club
Council for continuing support of the journal; Chair-
man Ron Bedford and the Publications Committee of
the OFNC for editorial encouragement and support, to
the Canadian Museum of Nature for access to its library
and the facilities at the Natural Heritage Building,
1740 Pink Road, Aylmer, Quebec, and to Joyce for
everything else.
FRANCIS R. COOK
Editor
Advice for Contributors to The Canadian Field-Naturalist
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RR 3 North Augusta, Ontario KOG TRO Canada |
298
TABLE OF CONTENTS (concluded) Volume 118 Number 2
Notes
Observations of-above surface littoral foraging in two sea ducks, Barrow’s Goldeneye,
Bucephala islandica, and Surf Scoter, Melanitta perspicillata, in coastal southwestern
British Columbia DEBORAH L. LACROIX, KENNETH G. WRIGHT, and DANIEL KEN1
New records of Cyperaceae and Juncaceae from the Yukon Territory
STUART A. HARRIS and PETER W. BALL
“Ashkui”, vernal ice-cover phenomena and their ecological role in southern Labrador
SHAUNA M. BAILLIE, CORINNE D. WILKERSON, and TINA L. NEWBURY
Sea Otter, Enydra lutris, sightings off Haida Gwaii/Queen Charlotte Islands, Canada, 1972-2002
KIMBERLY RAUM-SURYAN, KENNETH PITCHER, and RICHARD LAMY
iFirst record of a Barred Owl, Strix varia, in Labrador ISABELLE SCHMELZER and FRANK PHILLIPS
Forked Three-awned Grass, Aristida basiramea Engelm. ex Vasey: a new addition to the
flora of Quebec JACQUES BRISSON
Evidence for the use of vocalization to coordinate the killing of a White-tailed Deer, Odocoileus
virginianus, by Coyotes, Canis latrans ERICH M. MUNTZ and BRENT R. PATTERSON
Book Reviews
ZOoLoGy: Fish of Alberta — Sharks — In Search of the Golden Frog — Conversations with an Eagle —
North American Owls, Biology and Natural History, Second Edition — The Mountain White-Crowned
Sparrow: Migration and Reproduction at High Altitude — Seabird Bycatch: Trends, Roadblocks, and
Solutions — The Life of Mammals — Geographic Variation in Size and Shape of Savannah Sparrows
(Passerculus sandwichensis) — Warblers of the Great Lakes and Eastern North America — Sparrows
and Finches of the Great Lakes and Eastern North America — Birds of the Yukon Territory
Botany: Wild Flowers of the Yukon, Alaska & Northwestern Canada, 2™ edition — Wild Flowers of Field
| & Slope in the Pacific Northwest — Wild Flowers of Forest & Woodland in the Pacific Northwest —
Wild Flowers of the Mountains in the Pacific Northwest
MISCELLANEOUS: The Canoe: A Living Tradition — A Passion for Wildlife: The History of the Canadian
Wildlife Service — Birding on Borrowed Time
New TITLES
News and Comment
Update on Quebec Amphibian and Reptile Atlas Project: Rana-Saura 6(2) — Froglog: Newsletter of the
Declining Amphibian Populations Task Force (62) — Amphipacifica: Journal of Aquatic Systematic
Biology 3(4) — Marine Turtle Newsletter (104) — Erratum: Sloan and Bartiers 118(1): 80
| Editor’s Report Volume 117 (2003) FRANCIS R. COOK
| Advice for Contributors
Mailing date of the previous issue 118(1): 15 December 2004
2004
264
266
THE CANADIAN FIELD-NATURALIST Volume 118 Number 2 2004
Articles
Morphology and population characteristics of Vancouver Island Cougars,
Puma concolor vancouverensis STEVEN F. WILSON, APRYL HAHN, AARON GLADDERS, |
KAREN M. L. Gou, and Davip M. SHACKLETON 159
Conservation evaluation of Lemmon’s Holy Fern, Polystichum lemmonii, a threatened
fern in Canada GEORGE W. DOUGLAS 164
Conservation evaluation of the Pacific population of Tall Woolly-heads, Psilocarphus elatior,
an endangered herb in Canada GEORGE W. DOUGLAS and JEANNE M. ILLINGWORTH 169
Conservation evaluation of Howell’s Triteleia, Triteleia howellii, an endangered lily
in Canada GEORGE W. DOUGLAS and JENIFER L. PENNY 174
Conservation evaluation of Small-flowered Lipocarpha, Lipocarpha micrantha (Cyperaceae),
in Canada TYLER W. SMITH, GEORGE W. DOUGLAS, and ALLAN G. HARRIS 175)
Immobilizatin of clover-trapped White-tailed Deer, Odocoileus virginianus, with medetomidine
and ketamine, and antagonism with atipamezole JOSHUA J. MILLSPAUGH,
BRIAN E. WASHBURN, TAMARA M. MEYER, JEFF BERINGER, and LONNIE P. HANSEN 185
Predation on two Mule Deer, Odocoileus hemionus, by a Canada Lynx, Lynx canadensis, in the southern
Canadian Rocky Mountains DorTE PosziG, CLAYTON D. Apps, and ALAN DIBB 191
Effect of fire intensity and depth of burn on Lowbush Blueberry, Vaccinium angustifolium, and
Velvet Leaf Blueberry, Vaccinium myrtilloides, production in eastern Ontario
Luc C. DUCHESNE and SUSANNE WETZEL 195
Spring dispersal patterns of Red-winged Blackbirds, Agelaius phoeniceus, staging in eastern
South Dakota H. J. HomMaAN, G. M. Linz, R. M. ENGEMAN, and L. B. PENRY 201 1f
Changes in loon (Gavia spp.) and Red-necked Grebe (Podiceps grisegena) populations in the Lower
Matanuska-Susita Valley, Alaska TAMARA K. MILLS and BRAD A. ANDRES 210
The Barred Owl, Strix varia, in Alberta: distribution and status LisA TAKATS PRIESTLEY 215
Use of Eelgrass, Zostera marina, wrack by three species of ladybird beetles (Coleoptera:
Coccinellidae) in Prince Edward Island DaviD J. GARBARY, SARAH FRASER,
CARRIE FERGUSON, and RANDOLPH F. LAUFF 225
Predicting the effects of Cerulean Warbler, Dendroica cerulea, management on eastern Ontario
bird species JASON JONES, WILLIAM J. MCLEISH, and RALEIGH J. ROBERTSON Ds
Parasite prevalence in Dark-eyed Juncos, Junco hyemalis, breeding at different elevations i
HEATHER BEARS 235 iF
Movements of subadult male Grizzly Bears, Ursus arctos, in the central Canadian Arctic
ROBERT J. GAU, PHILIP D. MCLOUGHLIN, RAY CASE, H. DEAN CLUFF,
ROBERT MULDERS, and FRANCOIS MESSIER 239
Severe chronic neck injury caused by a snare in a Coyote, Canis latrans
PIERRE- Y VES DaAousT and PETER H. NICHOLSON 243
Interactions of Brown Bears, Ursus arctos, and Gray Wolves, Canis lupus, at Katmai National Park and
Preserve, Alaska Tom S. SMITH, STEVEN T. PARTRIDGE, and JOHN W. SCHOEN 247
Wild Turkey, Meleagris gallopavo silvestris, behavior in central Ontario during winter
LINH P. NGUYEN, JOSEPH HAMR, and GLENN H. PARKER 25
(continued on inside back cover,
ISSN 0008-3550
| The CANADIAN
— FIELD-NATURALIST
Published by THE OTTAWA FIELD-NATURALISTS’ CLUB, Ottawa, Canada
Volume 118, Number 3 July-September 2004
The Ottawa Field-Naturalists’ Club
FOUNDED IN 1879
Patrons
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The Canadian Field-Naturalist
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journal do not necessarily reflect those of The Ottawa Field-Naturalists’ Club or any other agency.
We acknowledge the financial support of the Government of Canada toward our mailing cost through the Publication Assistance
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Agreement number 40012317. Return Postage Guaranteed. Date of this issue: July-September 2004 (September 2005).
Cover: International zone on rugged rock headland of the Queen Charlotte Islands, British Columbia, each dominant species cre-
ating a distinct zone. The white lichen is mainly Coccotrema maritimum and the black one is almost entirely Verru cana
maura. Below the Verru cana is a zone bare of both lichens and marine algae, and, still lower, the algae take over. Figure
64 (page 77). Lichens of North America. By I. M. Brodo, S. D. Sharnoff, and S. Sharnoff. 2001. Yale University Press, New
Haven, Connecticutt. See article by Brodo and Sloan on lichen zonatum pages 405-424.
|
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| Volume 118, Number 3
The Canadian Field-Naturalist vA.
July—September 2004
Population Dynamics of Deer Mice, Peromyscus maniculatus, and
Yellow-pine Chipmunks, Tamias amoenus, in Old Field and Orchard
Habitats
THOMAS P. SULLIVAN!, DRUSCILLA S. SULLIVAN?, and EUGENE J. HOGUE?
'Agroecology Program, Faculty of Land and Food Systems, University of British Columbia, Vancouver, British Columbia
V6T 1Z4 Canada (corresponding author).
? Applied Mammal Research Institute, 11010 Mitchell Avenue, Summerland, British Columbia VOH 1Z8 Canada
3 Pacific Agri-Food Research Centre, Agriculture and Agri-Food Canada, 4200 Highway 97, Summerland, British Columbia
V1X 7S3 Canada
Sullivan, Thomas P., Druscilla S. Sullivan, and Eugene J. Hogue. 2004. Population dynamics of Deer Mice, Peromyscus mani-
culatus, and Yellow-pine Chipmunks, Tamias amoenus, in old field and orchard habitats. Canadian Field-Naturalist
118(3): 299-308.
There are often several rodent species included in the small mammal communities in orchard agro-ecosystems. This study was
designed to test the hypothesis that the population levels of Deer Mice (Peromyscus maniculatus) and Yellow-pine Chipmunks
(Tamias amoenus) would be enhanced in old field compared with orchard habitats. Rodent populations were intensively live-
trapped in replicate old field and orchard sites over a four-year period at Summerland, British Columbia, Canada. Deer Mouse
populations were, on average, significantly higher (2.5 — 3.4 times) in the old field than orchard sites in summer and winter
periods. Mean numbers/ha of Deer Mice ranged from 12.1 to 60.4 in old field sites and from 3.3 to 19.9 in orchard sites.
Breeding seasons in orchards were significantly longer than those in old field sites, in terms of proportion of reproductive
male Deer Mice. Recruitment of new animals and early juvenile survival of Deer Mice were similar in orchard and old field
sites. Populations of Yellow-pine Chipmunks ranged in mean abundance/ha from 5.6 — 19.0 in old field sites and from 1.9 —
17.5 on one orchard site, with no difference in mean abundance in 2 of 4 years of the study. Recruitment and mean survival
of Yellow-pine Chipmunks also followed this pattern. This study is the first detailed comparison of the population dynamics
of these rodent species in old field and orchard habitats. These species should be able to maintain their population levels and
help contribute to a diversity of small mammals in this agrarian landscape.
Key Words: Deer Mouse, Peromyscus maniculatus, Yellow-pine Chipmunk, Tamias amoenus, abundance, demography, old
field, orchard, population dynamics, recruitment, reproduction, British Columbia.
Voles of the genus Microtus are often the major
rodent species in perennial grasslands and agro-eco-
systems. In addition to grasses and herbs, these micro-
tines feed on vascular tissues of tree and other crop
plants primarily during winter months (Byers 1985;
Lewis and O’Brien 1990). Other major rodent species
include the Deer Mouse (Peromyscus maniculatus)
and Yellow-pine Chipmunk (TZamias amoenus), which
may occur in tree fruit orchards and adjacent habitats
in the inland regions of the Pacific Northwest of
North America. Neither of these associated species is
known to damage orchard trees by their feeding activity
as they are granivorous or insectivorous in their feeding
habits (Baker 1968; Webster and Jones 1982; Sutton
1992).
Deer Mice or White-footed Mice (P. leucopus) com-
monly occur with Microtus in old fields and other
perennial grassland habitats (Tamarin 1977; Krebs
1979; Dueser et al. 1981; Sullivan and Krebs 1981;
Schweiger et al. 2000; Manson et al. 2001; Pearson et
al. 2001) and in orchard agro-ecosystems (Sullivan et
al. 1998). Few studies of voles in orchards have report-
ed on the population dynamics of other species in the
small mammal community. Sullivan et al. (1998) dis-
cussed the population responses of all species to vege-
tation management in apple (Malus domestica) orchards
and Sullivan et al. (2000) reported changes in species
diversity of these communities in orchards and old fields.
Orchard habitats usually have frequent mowing and
vegetation management treatments during summer
months, and hence conditions for small mammals are
more changeable than in old fields. Thus, this study
was designed to test the hypothesis that the popula-
tion dynamics of Deer Mice and Yellow-pine Chip-
munks would be enhanced in old field compared with
orchard habitats. To evaluate this hypothesis, we pro-
vide a detailed analysis of the population dynamics of
these species in the two habitats.
299
300
Materials and Methods
Study area and experimental design
This study was conducted at the Pacific Agri-Food
Research Centre in the Okanagan Valley, Summerland,
British Columbia, Canada. The experimental design
consisted of two replicate “old field” and two repli-
cate orchard habitats. The old field habitats were
abandoned (225 years) hay fields composed of Crest-
ed Wheatgrass (Agropyron cristatum), Quack Grass
(Agropyron repens), Downy Brome (Bromus tecto-
rum), Diffuse Knapweed (Centaurea diffusa), with
some minor herbaceous species such as Yellow Salsify
(Tragopogon dubius), Great Mullein (Verbascum
thapsus), American Vetch (Vicia americana), Prickly
Lettuce (Lactuca serriola), and Tall Tumble-mustard
(Sisymbrium altissimum). These old field sites were
each 2 to 3 ha in area within a mosaic of sagebrush
(Artemisia tridentata), Ponderosa Pine (Pinus pon-
derosa) forest, and orchard habitats. These old fields
had resident populations of Deer Mice and Yellow-
pine Chipmunks. Other species included the Montane
Vole (Microtus montanus), Great Basin Pocket Mouse
(Perognathus parvus), Western Harvest Mouse (Reith-
rodontomys megalotis), and a few Long-tailed Voles
(M. longicaudus).
The orchards were: (A) a five-year-old apple orchard
unit, and (B) a 10-year-old apple orchard combined
with a 15-year-old pear (Pyrus sp.) orchard as one
unit. Both 1.2-ha orchards were located within a 90-
ha mosaic of tree fruits and vineyards. Thus, our ex-
perimental design had two true replicates of old field
sites and two replicates of orchard sites. Each pair of
old field and orchard sites was spatially segregated to
enhance statistical independence (Hurlbert 1984). A
third replicate pair would have strengthened the study
but was not possible within the operational setting of
the Research Centre.
Common grass species on the orchard sites included
Orchard Grass (Dactylis glomerata), Quack Grass,
bluegrass (Poa spp.), Smooth Brome (Bromus inermis),
and Crested Wheatgrass. These orchards were mowed
five or six times each summer. Rodenticides were
applied 3-4 times each winter in poison-bait feeder
stations (Radvanyi 1974) for voles (Mouse Bait IT® —
zinc phosphide and Ramik Brown® — diphacinone).
Rodenticides were not present in the old field sites.
Deer Mouse and Yellow-pine Chipmunk populations
All animals were live-trapped on 1-ha grids with
49 (7 x 7) trap stations located at 14.3-m intervals
with one or two Longworth live-traps at each station.
One of the old-field grids was an irregular shaped
rectangle of 1 ha with the same 49 stations. The four
grids (2 orchard and 2 old field) were live-trapped at
3-week (spring, summer, and fall) and at 4- to 6-week
(winter) intervals from June 1982 to April 1986.
Traps were baited with whole oats, peanut butter,
and carrot; coarse brown cotton was supplied as bed-
THE CANADIAN FIELD-NATURALIST
Vol. 118
ding. Traps were set on day 1, checked on the morning
and afternoon of day 2 and morning of day 3, and then
locked open between trapping periods. All animals
captured were ear-tagged with serially numbered tags,
breeding condition noted, weighed on Pesola spring
balances, and point of capture recorded. The duration
of the breeding season was noted by palpation of male
testes and the condition of mammaries of the females
(Krebs et al. 1969). A pregnancy was considered suc-
cessful if a female was lactating during the period
following the estimated time of birth of a litter. Ani-
mals were released on the grids immediately after
processing.
Seasons were defined as summer (April to Septem-
ber) and winter (October to March) periods. Thus,
there were four summer and four winter periods from
1982 to 1986. We used mass at sexual maturity to
infer age classes of animals. Body mass was used as
an index of age. The percentage of sexually mature
animals was used to determine the mass limitations
for juveniles and adults assuming that juveniles were
seldom, if ever, sexually mature, and that at least 50%
of the adults were sexually mature in their lowest
mass class. Deer Mice (juvenile = 1 — 20 g, adult > 21 g)
and Yellow-pine Chipmunks (juvenile = 1 — 44 g, adult
2 45 g) were classified as juvenile or adult by body
mass. Juveniles were considered to be young animals
recruited during the study. Recruits were defined as
new animals that entered the population through repro-
duction and immigration. All handling of animals was
in accordance with the principles of the Animal Care
Committee, University of British Columbia.
Demographic parameters
Population densities were estimated by the Jolly-
Seber model for reasons indicated by Jolly and Dick-
son (1983). The Jolly-Seber (J-S) model provides the
best.estimates of population size for mark and recap-
ture data when trappability values are generally < 70%
(Hilborn et al. 1976). However, when population size
falls very low and no marked animals are recaptured,
the J-S estimate becomes unreliable and impossible to
calculate (Krebs et al. 1986). For these sample weeks,
a minimum number of animals known to be alive
(MNA) (Krebs 1966) value was substituted for a bio-
logically unreasonable J-S estimate.
Measurements of recruitment, number of lactating
females, and early juvenile survival were derived from
the sample of animals captured in each trapping ses-
sion and then summed for summer periods. Early juve-
nile survival is an index relating recruitment of young
into the trappable population to the number of lactat-
ing females (Krebs 1966). A modified version of this
index is number of juvenile animals at week ft divided
by the number of lactating females caught in week
t — 3. Mean survival rates (28-day) for summer and
winter periods were estimated from the Jolly-Seber
model. Mean body mass of combined males and females
2004
SULLIVAN, SULLIVAN, AND HOGUE: POPULATION DYNAMICS OF DEER MICE AND CHIPMUNKS 30]
Peromyscus maniculatus
Number of animals/na
NO (Se) A on oO)
(eo) (ep) (ep) (oe) (=)
=
(eo)
--Old field 1 Old field 2
Orchard 1 Orchard 2
J SNJIMMJSNJIMMJISNJIMM JSNJIMM
1982 1983
1984 1985 1986
FiGurRE |. Population densities (Jolly-Seber) per ha of Deer Mice in replicate old field and orchard sites during the study.
Shaded bars indicate winter periods. Months of year are represented by J = July; S = September; N = November; J
January; M = March; M = May.
was used as an index of condition within populations
of Deer Mice and Yellow-pine Chipmunks during sum-
mer and winter periods.
Statistical analysis
Mean trappability, mean abundance, mean number
of recruits, mean Jolly-Seber survival rates, and mean
body mass were evaluated by 95% confidence inter-
vals (CI) for Deer Mice and Yellow-pine Chipmunks
in old field and orchard sites during summer and winter
periods, as per the recommendations of Gerard et al.
(1998) and Johnson (1999). Proportion of adult males
and adult females breeding was analyzed by a Chi-
square 2 x 2 contingency table (Zar 1984) for each of
the four summer periods. These datasets of proportion
of animals breeding often include animals captured
more than once, and hence they are not completely
independent. Thus, the Chi-square analyses provide
only an indication of the degree of difference between
datasets. In all analyses, the level of significance was
E1053
Results
Deer Mouse populations
Totals of 751 and 459 individual Deer Mice were
captured on the two old field and two orchard sites,
respectively. Mean J-S trappability estimates for Deer
Mice ranged from 62.6% to 73.8% in summer and
from 46.6% to 76.6% in winter in the old field sites.
These estimates in the orchard sites ranged from 48.0%
to 81.7% in summer and from 39.0% to 80.8% in
winter.
Deer Mouse populations were, on average, general-
ly higher (2.5 — 3.4 times) in the old field than orchard
sites in summer and winter periods (Figure 1). There
were some exceptions to this pattern in summers 1982
and 1985 and winter 1985-1986 when mean abun-
dance of Deer Mice was similar, at least in one old
field—orchard site comparison (Table 1). Numbers
of Deer Mice reached annual autumn peaks ranging
from 30.8 to 69.3 animals/ha in the old field-1 site and
from 57.2 to 67.5 animals/ha in the old field-2 site.
302 THE CANADIAN FIELD-NATURALIST Vol. 118
TABLE |. Mean abundance per ha + 95% confidence intervals for Deer Mice during summer and winter periods in replicate
old field and orchard sites. Sample size (n = number of trapping periods) in parentheses.
Old field Orchard
Period 1 2 1 2
Summer 1982 ye LES BikD 15.2 12.6
(7) 95% CI 11.2 — 23.8 22, 7.7 —22.7 9.3 — 16.0
Winter 1982-83 NG 25.8 49.0 16.8 6.0
(5) 95% CI 21.9 — 29.7 43.0 —55.] 10.6 — 23.0 2.6 —9.4
Summer 1983 Ve 41.9 55.6 15:5 19.9
(9) 95% CI 36.2 — 47.6 50.1 — 61.2 8.3 — 22.8 14.4 — 25.4
Winter 1983-84 xr 45.7 B92 10.6 9.0
(8) 95% CI 39.8 — 51.6 29.5 — 48.8 8.7 — 12.5 2.3 — 15.7
Summer 1984 1 ba 60.4 33.8 19.7 aL
(8) 95% Cl 54.5 — 66.3 24.0 — 43.6 16.1 — 23.3 14.3 —21.0
Winter 1984-85 x2 34.3 SES ite 333
(6) 95% CI 22.4 — 46.1 5.1-21.8 4.7-17.5 2.2-4.4
Summer 1985 V2 36.3 12.1 125 6.9
(9) 95% Cl 31.9 — 40.7 7.9 — 16.2 5.4 — 19.6 3.7— 10.1
Winter 1985-86 yf 41.1 22:2 19.6 4.4
(7) 95% CI 36.9 — 45.3 6.2 — 38.2 10.5 — 28.7 1.8—7.0
These old field populations also had increased recruit- In terms of mean abundance, Deer Mouse numbers
ment in early summer (April — May) in some years _ in old field sites ranged from a low of 12.1/ha to a high
which was likely related to the decline in breeding — of 60.4/ha during the four-year study (Table 1). Mean
activity by mid-summer (see Figure 2). abundance of Deer Mice on the two orchard sites
Peromyscus maniculatus
Old field 1 +2
80
fe))
oO
&
jo)
NO
fo)
Percentage of adult males breeding
!
JSNJIMMJISNJIMMJISNJIMMJISNJIMM
1982 1984 1985 1986
FiGurE 2. Percentage of adult males in reproductive condition for Deer Mice for pooled data in old field and orchard sites
during breeding seasons each year. Shaded bars indicate winter periods. Months of year are represented by J = July:
S = September; N = November; J = January; M = March; M = May.
2004
ranged from a low density of 3.3/ha to a high of 19.9/ha.
Orchard Deer Mice had annual increases in recruitment
in early summer with generally higher populations
(1.5 times) in summer than winter (Figure 1, Table 1).
Demographic parameters
Adult male Deer Mice commenced breeding in
January-February each year and continued up to July
in the old field sites and through the summer and
autumn months in the orchard sites (Figure 2). This
longer breeding season in orchard than old field sites
was significantly different in terms of proportion of
reproductive males in 3 of 4 years (Table 2). Propor-
tion of breeding female Deer Mice tended to follow
this pattern but there was a significant difference
between sites in 1984 only (Table 2).
The pattern of recruitment in terms of mean num-
bers of new Deer Mice was generally similar in old
field and orchard sites in both summer and winter
periods (Table 3). There was only one period (summer
SULLIVAN, SULLIVAN, AND HOGUE: POPULATION DYNAMICS OF DEER MICE AND CHIPMUNKS
303
1985) when an old field — orchard comparison of mean
values did not have overlapping 95% CI (Table 3).
Thus, productivity within orchard populations of Deer
Mice appeared to approach that of old field popula-
tions, at least with respect to breeding potential and
production of young.
Over the four breeding seasons, early juvenile sur-
vival was similar with overall mean values of 3.64 and
2.12 young Deer Mice captured per lactating female
in old field and orchard sites, respectively. Mean total
survival of Deer Mice was consistently higher in the
two old field sites and orchard-1 site than in the orch-
ard-2 site, except in summer 1983 when survival of
Deer Mice was significantly lower in the orchard
than old field sites (Figure 3).
Mean body mass of Deer Mice was the same or
higher in orchard than old field sites during summer
and winter periods (Figure 4). Only during winter
1983-1984 did body mass of mice in orchard-2 appear
lower than that in the old field sites.
TABLE 2. Proportion of adult male and female Deer Mice in reproductive condition during breeding seasons each year for
pooled data in replicate old field and orchard sites and results of Chi-square (y)analysis. Sample size (number of mice) in
parentheses. Significant P in bold face.
Old field Orchard Analysis
Year ve PB.
Males
1982 0.62 (84) 0.79 (28) 2.60 0.11
1983 0.67 (367) 0.95 (114) 34.87 <0.01
1984 0.67 (253) 0.81 (86) 6.58 0.01
1985 0.79 (150) 0.97 (39) qo <0.01
Females
1982 0.26 (69) 0.38 (42) eg 0.19
1983 0.30 (209) 0.30 (106) 0.00 1.00
1984 0.40 (182) 0.64 (96) 13.82 <0.01
1985 0.47 (103) 0.61 (49) 2.84 0.09
TABLE 3. Mean number of recruits (X) + 95% confidence intervals for Deer Mice during summer and winter periods in
replicate old field and orchard sites. Sample size (n = number of trapping periods) in parentheses.
Old field Orchard
Period 1 2 1 2
Summer 1982 X Syl Sel 4.6 5.6
(7) 95% Cl 2.6 —7.7 6.2 — 20.1 1:27 8:0 2.2 -8.9
Winter 1982-1983 X 4.0 6.6 2.8 2)
(5) 95% CI 1.7-6.3 2.6 — 10.6 0.0 —5.6 1.2—3.2
Summer 1983 X 6.7 10.0 49 5.6
(9) 95% CI 2.0— 11.3 SO llsy(9) DAVIS) 2.2 —-8.9
Winter 1983-1984 x BS) 3.5 1.9 3.8
(8) 95% CI 1.5-9.5 169-4 0.8 — 2.9 1.9-5.6
Summer 1984 X 9.9 SS) DS) 5.8
(8) 95% CI 7.3 —12.4 2.5 —8.5 2.5—8.5 3.2 — 8.3
Winter 1984-1985 X 3d 1S De), 0.7
(6) 95% CI 0.6 — 6.7 -0.6 — 3.6 -1.0 —5.3 One?
Summer 1985 X 7.8 3.4 3.9 2.0
(9) 95% Cl 4.3—11.2 2.1-—4.8 1.9-—5.9 1.1-—2.9
Winter 1985-1986 X 8.6 3.9 7.0 Dal
(7) 95% CI 1.5 — 15.6 0.5 -— 7.3 eS P27/ 0.2 —4.1
304 THE CANADIAN FIELD-NATURALIST Vol. 118
F @ i O Orchard 1
Peromyscus maniculatus orice” mn
@ Old field 2 O Orchard 2
|
O
2
c LJ
2 06 "
©
ne)
1)
of
>
= 04 if ?
2
S
14)
oO
=>
0.2
0
Summer Winter Summer Winter Summer Winter Summer Winter
1982 1982-83 1983 1983-84 1984 1984-85 1985 1985-86
FiGurE 3. Mean Jolly-Seber survival (per 28 days) + 95% confidence intervals for Deer Mice in replicate old field and
orchard sites during summer and winter periods in the study.
Yellow-pine Chipmunk populations
Totals of 137 and 79 individual Yellow-pine Chip-
munks were captured in the two old field and two
orchard sites, respectively. Only three individual chip-
munks were captured in the orchard-2 site during the
study. Mean J-S trappability estimates ranged from
30.8% to 63.8% in the old field sites, and from 37.1%
to 58.3% in the orchard sites.
Populations of Yellow-pine Chipmunks ranged in
mean abundance/ha from 5.6 to 19.0 in old field sites
and from 1.9 to 17.5 in the orchard-1 site (Table 4).
Mean abundance of Yellow-pine Chipmunks was sig-
nificantly (non-overlapping 95% confidence intervals)
lower in the orchard-1 than old field sites in 1982 and
1985 (Table 4). In terms of population changes over
the study, Yellow-pine Chipmunk abundance/ha ranged
from 1.0 — 27.0 in old field sites and from 1.0 — 46.3
in the orchard-1 site (Figure 5).
Mean number of Yellow-pine Chipmunk recruits
was similar between the old field and orchard-1 sites
(Table 4). Mean (+ SE) Jolly-Seber survival rates
averaged 0.78 + 0.05 (summer) and 0.96 + 0.02 (win-
ter) in the old field-1 site and 0.71 + 0.05 (summer)
and 0.91 + 0.06 (winter) in the orchard-1 site.
Discussion
Deer Mouse and Yellow-pine Chipmunk populations
The pattern of abundance of Deer Mice in our old
field sites was somewhat different from that recorded
in other old field and perennial grassland studies of
Peromyscus and Microtus. Grant (1972) and Baker
(1968) suggested that the Deer Mouse suffers from
competition from microtine rodents in perennial grass-
lands, and is forced to live in woodlands. However,
Deer Mouse densities in our studies reached annual
peaks ranging from 30.8 to 69.3 animals/ha in the pres-
ence of relatively high numbers of Montane Voles
(Sullivan et al. 2003). Experimental studies by Grant
(1971) and Redfield et al. (1977) concluded that Micro-
tus Outcompete Peromyscus in grassland habitats; how-
ever, explanations for this process were not given.
Conversely, other studies concluded that competitive
interactions among microtine rodents and Deer Mice
were unimportant (Gilbert and Krebs 1984; Galindo
2004 SULLIVAN, SULLIVAN, AND HOGUE: POPULATION DYNAMICS OF DEER MICE AND CHIPMUNKS 305
® Old field 1 O Orchard 1
Old field 2 O Orchard 2
Peromyscus maniculatus
30
35
43
S 86
21
my CD oA 57
a 97 141} J 169 ,, 13 68 478
= t 10440) ze
44 36
> mA 96 90
3 72 158
2 + ' 220
87
= if 355 ;
= {
= 2)
15
Summer Winter Summer Winter Summer Winter Summer Winter
1982 1982-83 1983 1983-84 1984 1984-85 1985 1985-86
FiGuRE 4. Mean body mass (g) + 95% confidence intervals for Deer Mice in replicate old field and orchard sites during
summer and winter periods in the study.
TABLE 4. Mean abundance (X) and mean number of recruits per ha (X) (+ 95% confidence intervals) for Yellow-pine
Chipmunks during non-hibernation periods in replicate old field and orchard sites. Sample size (x = number of trapping
periods) in parentheses.
Attribute and Old field Orchard
period 1 2 1 2
Abundance
1982 X 5.6 7.9 1.9 -
(7) 95% CI 3.6 — 7.7 3.8 — 12:0 0.7 — 3.0 -
1983 X 8.1 11.8 9.3 0.1
(13) 95% Cl 5.3 — 10.9 9.8 — 13.8 2.2 — 16.4 =
1984 X 19.0 8.9 TES) 0.2
(11) 95% CI 15.2 — 22.9 6.2 — 11.6 8.7 — 26.2 -
1985 X 14.5 9.8 3.6 -
(10) 95% Cl 12.1 — 16.9 6.2 — 13.4 1.9-—5.4 —
Recruits
1982 X 1.1 Da 0.6 -
(7) 95% CI 0.5 — 1.8 0.1-—5.3 -0.2 — 1.3 —
1983 X eS) 12 2.3 0.1
(13) 95% Cl 0.1 — 3.0 0.0 — 2.4 0.3 — 4.3 -
1984 x De) 0.7 3.4 0.2
(11) 95% CI E2339 -0.1-1.5 0.6 —6.1 ~
1985 X 1S 2.1 0.4 -
(10) 95% CI 0.7 — 2.3 0.5 — 3.7 -0.3-1.1 =
306
THE CANADIAN FIELD-NATURALIST
Vol. 118
Tamias amoenus
50
N () as
(o) (~) oO
Number of animals/ha
=x
oO
--Old field 1
-# Old field 2
< Orchard 1
J S NJ MM:J SON JOM.M J°S.N JOM Mod -S NLS MiGM
1982 1983
1984 1985 1986
FiGuRE 5. Population densities (Jolly-Seber) per ha of Yellow-pine Chipmunks in two old field sites and one orchard site
during the study. Shaded bars indicate winter periods. Months of year are represented by J = July; S = September; N
= November; J = January; M = March; M = May.
and Krebs 1985). Sullivan and Krebs (1981) reported
persistence of Deer Mice with Microtus spp. in a grass-
land habitat. Our densities of Deer Mice were as high
as reported in other studies of perennial grassland hab-
itats and orchards (Sullivan and Krebs 1981; Sullivan
et al. 1998).
This study is the first detailed investigation of the
population dynamics of non-target rodent species in
orchards treated with rodenticides for vole control.
Populations of Deer Mice in orchard sites showed con-
sistent annual changes in abundance averaging 15.0
animals/ha in summer and 10.1 animals/ha in winter
periods. These values were similar to those reported
for Montane Voles in these same orchards at 16.5 ani-
mals/ha in summer and 21.1 animals/ha in winter (Sul-
livan et al. 2003). Clearly, Deer Mice seemed produc-
tive in the orchard environment, having longer breed-
ing seasons than in the old field sites, and comparable
survival of young animals. Winter breeding in Deer
Mice has been reported, particularly after substantial
mast crops in forests (Wolff 1996) or in supplemental
food studies (Taitt 1981). Food resources appeared
sufficient to support breeding mice during winter peri-
ods and at body masses comparable to old field popu-
lations during most periods. These orchards received
regular inputs of fertilizer and irrigation, and hence
likely produced relatively “rich” habitats in terms of
plant production and invertebrate biomass. Mean
overall survival of Deer Mice in orchards was poor, in
at least one of the sites, relative to old field populations.
A lack of vegetative cover may have contributed to
greater predation by raptors, weasels (Mustela spp.),
and Coyotes (Canis latrans).
Our orchards were situated in a mosaic of different
varieties and age classes of orchards and vineyards
with adjacent natural habitats of sagebrush and Pon-
derosa Pine (Pinus ponderosa). As discussed by Sul-
livan et al. (1998) for their study in this same mosaic,
it was possible that our relatively high numbers of
Deer Mice (and Yellow-pine Chipmunks) in orchards
may have represented transients or animals who lived
in nearby sage-pine areas. However, a comprehensive
analysis of transient and resident animals suggested
strongly that these rodents very likely lived in the actual
2004
orchard units (Sullivan et al. 1998). There was no rea-
son to assume that our animal populations behaved
differently, and hence our population estimates were
considered accurate.
The prediction of the hypothesis that population
dynamics of Deer Mice and Yellow-pine Chipmunks
would be enhanced in old field compared with orch-
ard habitats is partially accepted. Abundance, recruit-
ment, and overall survival of Deer Mice were higher
in old field than orchard sites. However, proportion
of breeding animals and length of breeding seasons
were greater in the orchard sites. Early juvenile sur-
vival and body mass were similar between sites for
Deer Mice. Similarly, the general lack of differences
in abundance (except in 1982 and 1985) and recruits
for Yellow-pine Chipmunks between sites (albeit for
one replicate only) also contradicted our prediction.
These rodent species should be able to maintain
their population levels in association with Microtus
in these habitats. Traditional methods of vole control
(rodenticides) seem to have had little effect on these
two non-target species in the orchard sites. The higher
abundance of Deer Mice, and sometimes Yellow-pine
Chipmunks, in the old field than orchard sites was
more likely a function of habitat quality than expo-
sure to rodenticides. Consequently, Deer Mice and
Yellow-pine Chipmunks may assist integrated pest
management in orchards because both species per-
sisted in this managed habitat and their consumption
of seeds and invertebrates could provide some degree
of assistance in reducing weed and insect pests. In
addition, as prey species, they may attract a greater
number of predators to these sites. A total of six small
mammal species was recorded in these orchards,
which suggests that these agro-ecosystems and adja-
cent natural lands help contribute to a diversity of
habitats in this agrarian landscape.
Acknowledgments
We thank the Research Branch of Agriculture Can-
ada and the Applied Mammal Research Institute for
financial support; the study area and facilities provided
by the Summerland Research Station; and field assis-
tants W. Kaiser, J. Gareau, B. Jones, J. Krebs, and C.
Robinson.
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Received 11 August 2002
Accepted 24 December 2004
Density and Survival of Lady Beetles (Coccinellidae) in Overwintering
Sites in Manitoba*
W. J. TURNOCK and I. L. WISE
Cereal Research Centre, Agriculture and Agri-Food Canada, 195 Dafoe Road, Winnipeg, Manitoba, Canada R3T 2M9
Turnock, W. J., and I. L. Wise. 2004. Density and survival of Lady Beetles (Coccinellidae) in overwintering sites in Manitoba.
Canadian Field-Naturalist 118(3): 309-317.
The densities of lady beetles, Coccinellidae, overwintering as adults (adults per m7) in leaf litter collected in late October for
two years in a beach-ridge forest on the south shore of Lake Manitoba were 56.4 for the Thirteen-spotted Lady Beetle,
Hippodamia tredecimpunctata (Say), 38.3 for the Seven-spotted Lady Beetle, Coccinella septempunctata (L.), 7.7 for the
Transverse Lady Beetle, Coccinella transversoguttata richardsonii Brown, 1.6 for the Convergent Lady Beetle, Hippodamia
convergens Guerin, and 0.6 for the Parenthesis Lady Beetle, Hippodamia parenthesis (Say). The mean overwintering survival
for these species was 0.254, 0.036, 0.023, 0.0, and 0.0, respectively. The density of overwintering coccinellids was highest
near the margins of the forest, particularly on the beach side, where beetles from shore appear to have entered the forest. The
mean density over 3 years (2.9 per m7) of all coccinellid species in November in the litter under a remnant grove of riverbank
forest in Winnipeg, was lower than in the beach-ridge forest (104.8 per m?), but their survival (0.460) was higher than in the
beach-ridge forest (0.154). More species of coccinellids were found in the samples from the riverbank forest than from the
beach-ridge forest.
Key Words: Lady Beetles, Coccinellidae, leaf litter, beach-ridge forest, overwintering sites, Lake Manitoba, Red River.
The overwintering sites of north-temperate zone coc-
cinellids include leaf litter, grass tufts, bark crevices,
stone piles, and rock clefts (Hodek and Honék 1996).
Adults of some species migrate long distances to hiber-
nate at high elevations, and even those which move
only locally seem to be attracted to even slightly higher
elevations and vertical silhouettes. In Bohemia and
Moravia, Coccinella septempunctata L. (C7) prefers
elevated places, but also hibernates in refuges among
cultivated areas and does not migrate long distances
(Hodek 1960). In southern Manitoba, where much of
the land is flat and cultivated, it is generally believed
that lady beetles overwinter in the leaf litter under trees
in field shelterbelts, farmsteads and urban plantings,
along the shores of streams and lakes, and in “bluffs”
(groves of trees on uncultivated land). The species oc-
currence, density, and survival of coccinellids in most
of these overwintering sites have not been studied.
Large numbers of pre-hibernating coccinellids are
washed ashore in some years on Manitoba lakes, usu-
ally in late August to early October (Lee 1980; Turnock
et al. 2003). These beetles usually fly away soon after,
to complete their search for hibernating sites, and do
not often walk into the adjacent beach-ridge forest.
Once, on 1 November 1978, beetles (mainly H. con-
vergens) were washed ashore, but subsequent cold
weather forced them to remain near the beach, where
few survived the winter (Turnock and Turnock 1979).
In this paper, the density, distribution, species com-
position, and overwintering survival of coccinellids in
the litter under a beach-ridge forest are compared with
the density and survival of coccinellids in the litter
under a riverbank forest.
Methods
Beach-Ridge Forest. The abundance and species
composition of coccinellids overwintering in the sur-
face litter and soil under a beach-ridge forest on the
south shore of Lake Manitoba at the Delta Marsh Field
Station (University of Manitoba), 50°11'N, 98°23'W,
about 120 km WNW of Winnipeg, were recorded. The
shore is a sand beach with a forested barrier-beach
ridge formed by the reworking of alluvial sand depos-
its. This beach ridge, about 60 m wide, supports a
mature deciduous forest of Manitoba Maple (Acer
negundo L.), Green Ash (Fraxinus pennsylvanica
Marsh.), Plains Cottonwood (Populus deltoides Marsh.),
and Peachleaf Willow (Salix amagdaloides Anderss.)
(Kenkel 1986). The ridge has its highest elevation 5-
10 m from the top of the foreshore and slopes down
about 50 m to the marsh. A road about 10 m wide along
the south edge of the beach ridge separates the forest
from the marsh. Samples were taken along five tran-
sects, 20 m apart, perpendicular to the beach. Six sam-
ples were taken along each transect at 1, 6, 11, 21, 31,
and 41 m from the top of the foreshore, where the
beach ended and the beach-ridge forest began. A
sample of the leaf litter and soil above the sandy par-
ent material, 0.25 m? and 5-10 cm deep, was collect-
ed at each of the 30 locations. Samples were collected
after beetle flight had ceased, on 22 October 1992 and
27 October 1993. Each sample was bagged, sorted by
*Contribution Number 1832 from the Cereal Research Centre, Agriculture and Agri-Food Canada, 195 Dafoe Road, Winnipeg, Manitoba,
Canada R3T 2M9.
309
310
hand to remove the beetles, and the species and num-
ber of coccinellids were recorded.
The numbers and species of coccinellids emerging
in the spring were determined from cone traps, each
covering a surface area of 0.1028 m* (Turnock et al.
1987). One trap was set into the litter at each of the
30 locations, near the place where a litter sample had
been collected the previous autumn. The traps were
set out at each location in late April or May, depend-
ing on the disappearance of snow, in 1993, 1994, and
1995. The traps at the apex of the cones were emptied
at regular intervals, and the coccinellids identified to
species and counted.
Riverbank Forest. The overwintering of coccinellids
in a remnant grove of riverbank forest along the Red
River at the University of Manitoba, Winnipeg, Mani-
toba, was determined from records of the insects found
in litter samples and emergence traps used to study
the overwintering of flea beetles (Chrysomelidae) (Tur-
nock et al. 1987). The grove of trees, about 1.3 ha in
area, included Bur Oak (Quercus macrocarpa Michx.),
American Elm (Ul/mus americana), Manitoba Maple,
Green Ash, Black Ash (Fraxinus nigra Marsh.), and
Basswood (Tilia americana L.). In this grove, 50 litter
samples, each 0.25 m7, <10 cm deep, were collected in
the autumn of the years 1980-1982, and in the springs
of 1980, 1981, and 1983. The samples were taken at
10 m intervals along five transects running north to
south through the grove. Spring emergence was sam-
pled by 100 cone traps, each covering 0.1028 m/, in
1980 and 1981. Two traps were located at 10 m inter-
vals along each transect, one on each side of the site
of a litter sample, as described by Turnock et al. (1987).
For coccinellids, only the total number collected in
each sampling period was recorded, except in the litter
samples of 3 November 1982, where the species were
identified but their numbers were not recorded.
Results
Beach-Ridge Forest. The dominant species in all
collections were H. tredecimpunctata, C. septempunc-
tata, and Coccinella transversoguttata. In the autumn
litter samples in 1992 (n = 653) and 1993 (n = 918)
coccinellid relative abundances were: 0.54/0.54 (H.
tredecimpunctata); 0.36/0.37 (C. septempunctata); 0.08/
0.07 (C. transversoguttata); 0.01/0.02 H. convergens;
and 0.004/0.001 H. parenthesis (Say). In the spring
emergence samples, the relative abundances of each
species in 1993/94/95 were: H. tredecimpunctata —
0.95/0.78/0.92; C. septempunctata — 0.04/0.19/0.06;
and C. transversoguttata — 0.02/0/0. Neither H. conver-
gens nor H. parenthesis were found in the spring sam-
ples. The distribution of numbers per sample of H.
tredecimpunctata and C. septempunctata was skewed
in both the autumn litter samples and the spring emer-
gence samples, with most samples containing 0, 1, or
2 beetles (Figure 1).
THE CANADIAN FIELD-NATURALIST
Vol. 118
The mean density per m* of coccinellids in the
autumn was 87.1 in 1992 and 122.4 in 1993, and 8.5
and 11.7 in the following springs. The density of coc-
cinellids in the autumn was generally higher on the
margins of the forest, but it varied among species
(Figure 2). The numbers of H. tredecimpunctata were
highest near the beach margin in 1993, but they were
higher near the marsh margin in 1992. The density of
both C. septempunctata and C. transversoguttata was
higher near the beach margin in both years, with only a
slight increase along the marsh margin. These patterns
suggest that most of the C. septempunctata and C.
transversoguttata found in the litter near the beach were
from aggregations that had washed ashore (Turnock et
al. 2003). Hippodamia tredecimpunctata seems mainly
to have come from the beach in 1993, but in 1992
more appeared to have come across the marsh to the
edge of the forest.
The proportion of living beetles in the autumn litter
samples differed little between years, 81.3% in 1992
(n = 653) and 81.4 % (n= 913) in 1993 (Table 1). The
mean proportion of living beetles, by species for both
years, was: H. tredecimpunctata = 0.963 (n = 847);
C. septempunctata = 0.729 (n = 575); C. transversogut-
tata = 0.250 (n = 116); H. convergens = 0.458 (n = 24);
and H. parenthesis = 0.500 (n = 4). Survival of all spe-
cies was lowest adjacent to the beach and increased
toward the edge of the marsh (Figure 3). The decreased
survival in the forest edge near the beach was prob-
ably caused by the burial of overwintering beetles by
sand blown off the beach by strong winds.
Coccinellids emerged from the leaf litter during May
and early June in traps throughout the beach-ridge.
Most of the beetles (98%, n = 187) were of two spe-
cies, H. tredecimpunctata and C. septempunctata. The
mean density per m? of emerging coccinellids in 1993
to 1995 was: 17.5, 9.1, 27.9 for H. tredecimpunctata;
0.65, 2.3, 1.9 for C. septempunctata; and 0.32, 0, 0 for
C. transversoguttata. The pattern of higher densities
near the margins of the forest was less prominent in
the spring than in the autumn (Figures 2 and 4). The
density of emerging beetles was <20 per m? except at
distances from the beach of | m in 1995, 31 m in 1994,
and 41 m in 1993.
The mean overwintering survival (density spring/
density autumn) in the beach-ridge forest for H. tre-
decimpunctata was 0.370 in the winter of 1992-1993,
and 0.139 for 1993-1994 (Table 1). The survival ratios
over the same two winters for C. septempunctata
were (0.021 and 0.051, and for all coccinellids, 0.212
and 0.096. The survival of H. tredecimpunctata was
quite variable with position within the forest (Figure 5).
Overwintering survival of all species was very low at
1 m from the beach margin of the forest, where drifting
sand often covered the leaf litter. However, the over-
wintering survival did not significantly differ among
years, density of coccinellids in the autumn, or distance
2004 TURNOCK and WISE: DENSITY AND SURVIVAL OF LADY BEETLES 31]
Coccinella septempunctata
Mmm 1992
Gas%] 1993
Frequency
60 80 100
Hippodamia tredecimpunctata
Frequency
100
Coccinella transversoguttata
Frequency
80 100
0 20 40 60
Beetles per sample
FIGURE 1. Frequency distribution of numbers of coccinellids, Hippodamia tredecimpunctata, Coccinella septempunctata,
and Coccinella transversoguttata, per sample of litter (0.25 m? x 5-10 cm deep) from the floor of the beach-ridge
forest at the Delta Marsh Field Station, Manitoba, in late October of 1992 and 1993. n = 60 for each species.
SH
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 1. The mean numbers (N) per m? in autumn litter samples and spring emergence samples, the proportion of living
beetles in the autumn samples, and the overwintering survival (density spring emergents/density in autumn), for Coccinella
septempunctata (C7), Hippodamia tredecimpunctata (H13),
C. transversoguttata (CT), H. convergens (HC), and H.
parenthesis (HP), and all coccinellids in the beach-ridge forest at the Delta Marsh Field Station.
Species 1992 1993
Autumn Spring
H13 N/m? 47.3 IES
Survival 0.95 0.37
N 355 54
(Oy N/m? Si1k3 0.65
Survival 0.72 0.02
N 235 2
CT N/m? 6.9 0.32
Survival 0.37 0.05
N 52 1
HC N/m2 101 0
Survival 0.38 0
N 8 0
HP N/m? 0.4 0
Survival 0.67 0
N 3 0
All N/m? 87.1 18.5
Survival 0.81 0.21
N 653 57
1993 1994 1995
Autumn Spring Spring
65.6 9.1 27.9
0.97 0.14 ~
492 28 86
45.3 ep) 129
0.73 0.05 -
340 q 6
8.5 0 0
0.16 0 -
64 0 0
25k 0 0
0.5 0 -
16 0 0
0.13 0 0
1 0 -
0 0
122.4 11.7 30.5
0.81 0.1 —
913 36* 94%
*Includes one specimen of Anistosticta bitriangularis in 1994 and two specimens of Calvia quatuordecimguttata in 1995.
from the beach (analysis of variance, proc glm, SAS
Inst. Inc. <www.sas.com>). The high survival of H. tre-
decimpunctata at several locations likely reflects the
placing of the emergence traps over local aggrega-
tions of beetles in the litter, as does a single record of
high survival of C. septempunctata.
Riverbank Forest. The litter samples collected on 3
November 1982 contained nine species of coccinel-
lids: Stethorus punctum (LeConte), Scymnus (Pullus)
brullei Muls., Hyperaspis benedetti (Say), Chilocorus
stigma Say, H. tredecimpunctata, Anatis labiculata
(Say), Adalia bipunctata L., C. transversoguttata, and
Psyllobora virginimaculata (Say). The mean density
of all coccinellid species in the autumn litter collec-
tions of 1980-1982 (n = 110) was 2.9 per m? (2.0-
4.3), vs. 4.4 (1.5- 10.4) in the spring litter collections
(n = 172) of 1980, 1981, and 1983. Overwintering
survival, calculated by dividing the number of living
beetles in the spring litter samples by the total num-
ber of beetles in the autumn samples, was 76% for the
winter of 1980-1981 and 43% for the winter of 1982-
1983. Survival during the winter of 1980-1981 was
lower, 49%, when the spring density, 0.97 per m*, was
based on captures in the emergence traps (n = 10).
Discussion and Conclusions
The studies of coccinellid density and survival in
three overwintering sites in southern Manitoba differ
in location, years, and sampling design. However, the
results of some comparisons may be helpful to future
investigators of site selection and survival by overwin-
tering coccinellids. In the autumn, more overwintering
lady beetles were found in a beach-ridge forest on
the shores of Lake Manitoba in 1992 and 1993 than in
a riverbank forest in Winnipeg in 1980 to 1981. The
difference in the density between the two sites may
have been related to differences in the populations of
lady beetles in the years sampled. Another factor could
be the availability of overwintering sites in the two areas.
The beach-ridge forest was located in an intensively-
farmed area with few treed areas, whereas the river-
bank forest was near suburban Winnipeg, where trees
were more abundant. Beetles washed ashore on the
beach contributed to the number overwintering in the
beach-ridge forest in 1993, but in 1992 more beetles
seem to have entered the forest from the side away
from the beach.
The beach-ridge forest, despite higher initial den-
sities, had fewer species and fewer beetles emerging
in the spring than in the riverbank forest, because of
lower overwintering survival. Overwintering survival
by beetles may be related to their need for moisture
(Hodek and Honék 1996). The litter under the river-
bank forest was thicker and lay upon a clay soil, thus
providing a moister environment than the thinner litter
on a sandy soil under the beach-ridge forest.
The limited sampling by Turnock and Turnock
(1979) on the shores of Lake Manitoba, following a
very late flight (1 November) and aggregation of
beetles, indicated few beetles survived the winter (2%
of 1002 per m? trapped in the beach debris). Even this
level of survival is surprising, because beach debris
usually is pounded and buried by high water, large
2004 TURNOCK and WISE: DENSITY AND SURVIVAL OF LADY BEETLES
Beetles per m?
Beetles per m?
Beetles per m?
30 40 50
0 10 20
Distance from forest edge (m)
FiGurE 2. Mean density per m? of Hippodamia tredecimpunctata, Coccinella septempunctata, Coccinella transversoguttata,
and all coccinellids, in forest litter samples collected at various distances from the forest edge next to the beach in
late October 1992 and 1993 at the Delta Marsh Field Station.
314 THE CANADIAN FIELD-NATURALIST Vol. 118
Proportion alive
Proportion alive
All species
Proportion alive
0 10 20 30 40 50
Distance from forest edge (m)
FicuRE 3. Proportion of live individuals of Hippodamia tredecimpunctata (H13), Coccinella septempunctata ( (C7).
Coccinella transversoguttata (CT), and all coccinellids, in litter samples taken at different distances from forest edge
next to the beach in late October of 1992 and 1993.
TURNOCK and WISE: DENSITY AND SURVIVAL OF LADY BEETLES
2004
—e— H13
-O::- C7
N —-w— All species
= —.
=
(oy
[ou
0)
a)
x)
®
faa)
N
E
=
(or)
Q.
o
v
zr)
®
a
N
i=
=
®
a
72)
&
©
®
a
Distance from forest edge (m)
FiGure 4. Mean density per m? of Hippodamia tredecimpunctata (H13), Coccinella septempunctata (C7), and all coccinel-
lids, in emergence trap samples collected at different distances from the forest edge next to the beach. The samples
were collected from emergence cones placed over the litter in May of 1993, 1994, and 1995.
316
Survival
THE CANADIAN FIELD-NATURALIST
Vol. 118
H13-1992/3
H13-1993/4
C7-1992/3
C7-1993/4
Distance from forest edge (m)
FiGurE 5. Mean overwintering survival ratios for Hippodamia tredecimpunctata (H13), and Coccinella septempunctata (C7),
for the winters of 1992-1993 and 1993-1994 in forest litter on the beach ridge at different distances from the forest
edge next to the beach at the Delta Marsh Field Station.
waves, and ice chunks from violent autumn and spring
storms. In this study the top of the foreshore, where a
covering of aspen leaves had accumulated on the sand,
had 74 beetles per m* and overwintering survival was
53%. This location is not likely to be a suitable over-
wintering site in most years because of high water
and waves. The grassy backshore, with little litter, had
28 beetles per m’, of which 18% survived the winter.
The foreshore of the sandy beaches and even the shal-
low litter in the sparse beach-ridge forest of Trembling
Aspen, Populus tremuloides Michx., do not appear to
be selected by coccinellids for overwintering. Excep-
tions can occur when beetles washed ashore after un-
usually late autumn flights aggregate on the beach when
subsequent temperatures are too cool to allow flight,
but warm enough to allow limited walking up the beach
to the backshore. In these cases the beach-ridge forest,
even if unsuitable, is mainly a “last-chance” overwin-
tering site for these beetles.
Four species of coccinellids, H. tredecimpunctata,
C. septempunctata, C. transversoguttata, and H. con-
vergens (in order of relative abundance) were found
in both years in autumn litter samples in the beach-
ridge forest, but only the first two species were found
in the spring emergence samples in all three years.
More H. tredecimpunctata (14 and 38%) survived over
winter than C. septempunctata (3 and 5%) or C. trans-
versoguttata (5 and 0%). This level of survival of C.
septempunctata is much lower than the 97% survival
of C. septempunctata that had been covered with litter
in experimental cages at Edmonton, Alberta (Ryan and
Acorn 1999).
Although in Europe C. septempunctata does not
migrate long distances to hibernate (Hodek 1960), large
flights of this species occur in both autumn and spring,
as shown by the numbers of this species that are found
in the aggregations washed ashore on the shores of
the lakes (Turnock et al. 2003).
Southern Manitoba is mostly cultivated and has a
flat terrain, so potential overwintering sites are limited
to leaf litter under trees. These habitats probably are
both attractive and suitable for the hibernation of coc-
cinellids, but without information on the preferred over-
wintering sites in this area, the true level of overwinter-
ing survival by native and introduced species cannot
be compared.
2004
Acknowledgments
The statistical advice by S. Woods, technical assis-
tance of R. J. Bilodeau, and the help given by the staff
of the Delta Marsh Field Station (University of Mani-
toba) in providing facilities is gratefully acknowledged.
This is Publication Number 305 from the Delta Marsh
Field Station (University of Manitoba).
Literature Cited
Hodek, I. 1960. Hibernation-bionomics in Coccinellidae.
Acta Societis Entomolicae Cechosloveniae 57(1): 14-17.
[In Czech with English “Discussion and Conclusions” }.
Hodek, I., and A. Honék. 1996. Ecology of Coccinellidae.
Series Entomological. Volume 54. Kluwer Academic Pub-
lishers. Dordrecht. 464 pages.
Kenkel, N. C. 1986. Vegetation structure and dynamics of the
barrier-beach ridge at Delta, Lake Manitoba. Annual Report
of the University of Manitoba Delta Marsh Field Station
21: 61-83.
TURNOCK and WISE: DENSITY AND SURVIVAL OF LADY BEETLES 317
Lee, R. E. 1980. Aggregations of lady beetles on the shores
of lakes. American Midland Naturalist 104; 295-304.
Ryan, S. E., and J. H. Acorn. 1999. Overwintering survival
of the seven-spot ladybug (Coccinella septempunctata) in
Edmonton. Blue Jay 57: 97-100.
Turnock, W. J., and R. W. Turnock. 1979. Aggregations of
lady beetles (Coleoptera: Coccinellidae) on the shores of
Lake Manitoba. Manitoba Entomologist 13: 21-22.
Turnock, W. J., R. J. Lamb, and R. J. Bilodeau. 1987. Abun-
dance, winter survival, and spring emergence of flea beetles
(Coleoptera: Chrysomelidae) in a Manitoba grove. The
Canadian Entomologist 119: 419-426.
Turnock, W. J., I. L. Wise, and F. O. Matheson. 2003. Abun-
dance of native coccinellines (Coleoptera: Coccinellidae)
before and after the appearance of Coccinella septem-
punctata. The Canadian Entomologist 135: 391-404.
Received 9 August 2002
Accepted 24 December 2004
Description of Age-O0 Round Goby, Neogobius melanostomus Pallas
(Gobiidae), and Ecotone Utilisation in St. Clair Lowland Waters,
Ontario
JOHN K. LESLIE and CHARLES A. TIMMINS
Great Lakes Laboratory for Fisheries and Aquatic Sciences, Department of Fisheries and Oceans, 867 Lakeshore Road, Burling-
ton, Ontario L7R 4A6 Canada
Leslie, John K., and Charles A. Timmins. 2004. Description of age-O Round Goby, Neogobius melanostomus Pallas (Gobiidae),
and ecotone utilisation in St. Clair lowland waters, Ontario. Canadian Field-Naturalist 118(3): 318-325.
Early developmental stages and ecotone utilisation of the non-indigenous Round Goby, Neogobius melanostomus (Pallas, 1811),
are described and illustrated. Fish (5-40 mm) were collected in coarse gravel, rocks and debris in the St. Clair River/Lake
system, Ontario, in 1994-2000. The Round Goby hatches at about 5 mm with black eyes, flexed urostyle, and developed fins
and digestive system. Distinguishing characters include large head, dorsolateral eyes, large fan-shaped pectoral fins, two dorsal
fins, fused thoracic pelvic fins and a distinct black spot on the posterior of the spinous dorsal fin. Modal counts for preanal,
postanal, and total myomeres were 12, 19, and 31, respectively.
Key Words: Round Goby, Neogobius melanostomus, St. Clair aquatic ecosystem, age-0, morphometry, habitat, Ontario.
Gobiidae, the largest family of marine fishes, has
been found in fresh waters of all continents (Nelson
1984) except Antarctica. None of 68 species endemic
to North America is native to the Great Lakes, where
two introduced species, the Round Goby, Neogobius
melanostomus (Pallas, 1811) and the Tubenose Goby,
Proterorhinus marmoratus (Pallas, 1811), recently be-
came established. These fishes originate in the Ponto-
Caspian region (Caspian, Azov and Black seas and Sea
of Marmara). International ships’ ballast was assumed
the most probable means by which Round Goby eggs
and/or postembryonic stages were transferred from
the Black Sea to the Great Lakes (Crossman et al.
1992; Jude et al. 1992). Since its arrival in the mid-
late 1980s the relatively innocuous Tubenose Goby
has not proliferated beyond the St. Clair-western
Lake Erie ecosystem (Leslie et al. 2002). In contrast,
the aggressive, eurytopic Round Goby has diffused
extensively and is now one of the most abundant fish
in the Great Lakes basin. Apparently, repetitive spawn-
ing and habitat requirements of this fish conflict with
our native species (Dubs and Corkum 1996), some of
which they may supplant.
The Round Goby is a guarding cavity spawner with
a life span of 4-5 years (Miller 1986). Spawning sea-
son is typically from spring to late summer. Rocks,
gravel, solid objects with crevices and submersed plants
are used for egg deposition (Miller 1986; Skora 1997*).
Whereas literature abounds on the ecology of adults,
information on postembryonic fish is rare. Eggs and
early developmental stages in southern Russia and
Ukraine have been described by Moskal’kova (1967),
Kalinina (1976), and Koblickaja (1981). This report
presents information on aspects of taxonomy and eco-
tone utilisation of age-O0 Round Gobies in the Great
Lakes and considers possible effects the species may
have on the aquatic community in general and native
fishes in particular.
Study Area
Eggs and age-0 fish were collected at numerous
locations at the shore of the St. Clair River, Ontario,
various sites along the southeastern shore of Lake St.
Clair, and in Duck Creek (42°17'N, 82°35'W), a low
gradient stream tributary to Lake St. Clair (Figure 1).
Duck Creek is a disturbed system draining a small
area in one of the most highly cultivated agricultural
regions in Canada. It is approximately 9 km long and
10-15 m wide near its mouth, where most specimens
were collected. Mid-stream depth ranges from 1.2 to
1.6 m. In April to November 1995, mean conductivity
was 487 uS/cm and Secchi disc depth 0.3 + 0.1 m,
reflecting high suspended particulate load due to run-
off from cropland. Substrate at the sampling site is
mainly alluvium, with clay and scattered debris of
human origin at the base of 1-4 m high stream banks.
However, age-O Round Gobies were found only on a
small gravelled area at the base of a railway bridge.
Duck Creek has a large diverse, albeit transient, fish
assemblage of at least 41 species (Leslie and Timmins
1998) dominated by Gizzard Shad Dorosoma cepedi-
anum, Bluntnose Minnow Pimephales notatus, Spottail
Shiner Notropis hudsonius, and Bluegill Lepomis
macrochirus. Submersed plants near the collection site
include Pondweed Potamogeton spp., Eelgrass Vallis-
neria americana, Canada Waterweed Elodea cana-
densis, Eurasian Milfoil Myriophyllum spicatum, and
Curly Pondweed Potamogeton crispus. Arrowhead
Sagittaria sp., Sedge Carex sp., Cattail Typha spp., and
Bulrush Scirpus spp. were abundant emergent species.
318
2004
Michigan Lake Huron
ichig
20 kn
Lake St. Clair
© Duck Creek
FiGure 1. Main sites where age-O Neogobius melanostomus
were collected in the St. Clair River-Lake ecosystem
in 1994-2000: LGS (Lambton Generating Station) and
Duck Creek.
Round Goby eggs and age-0 developmental stages
as well as numerous co-occurring fishes were found
at various locations at the shore of the St. Clair River,
mainly in dilute condenser cooling water discharge
of Lambton Generating Station (LGS) (42°47'N,
82°22'W). Random fish collections took place at LGS
(Figure 1) each year between April and November
1994-2000 over a shoreline stabilised with debris,
limestone boulders and rocks 0.3-1.0 m in longest
dimension. This formation extends 4 m from shore on
a natural substrate of sand. Most common fish species
collected with age-O Round Gobies in the St. Clair
River include age-O0 White Sucker Catostomus com-
mersoni, Alewife Alosa pseudoharengus, Brook
Silverside Labidesthes sicculus, Rainbow Darter Ethe-
ostoma caeruleum, lowa Darter Etheostoma exile,
Johnny Darter Etheostoma nigrum, Spottail Shiner,
and Emerald Shiner Notropis atherinoides. Of these
species, guarding speleophils Rainbow Darter, Iowa
Darter, and Johnny Darter utilise common ecotones
and probably compete with gobies for food and shelter.
Methods
A bulging larval fish beach seine (4 m long, 1 m
wide, mesh 0.4 mm) was necessary for capture of
recently hatched gobies, which only emerged from pro-
tective crevices when the bottom of the seine dis-
LESLIE and TIMMINS: AGE-O ROUND GoBy IN ONTARIO
319
turbed the substrate. Two flat seines, 3 m long, | m
wide (3 mm mesh), and 6 m long, | m wide (6 mm
mesh) were used to sample young and adult gobies
and co-occurring species. All seine hauls took place
repeatedly in contact with gravel at the base of a rail-
way bridge over Duck Creek.
In the St. Clair River, clusters of eggs attached to
rocks or human artefacts such as discarded sewer
pipe were preserved intact with 5-10% formalin and
enumerated in the laboratory. Water temperature, spe-
cific conductivity, water transparency, substrate char-
acteristics, and co-occurring fishes were recorded at
all sampling locations except four that were devoid
of cover and fishes.
Fish were preserved in a 12:1 solution of 80%
ethanol and glycerin, respectively, and stored at room
temperature (22-25°C). A dissecting microscope
equipped with an ocular micrometer was used for mea-
surement and illustration of fish. Measurements <5 mm
were accurate to +0.1 mm, and larger characters to
+0.2 mm. Several specimens were cleared to determine
vertebra number. Fish used in this study are stored at
the Royal Ontario Museum, Toronto, Ontario.
In general, terms used to describe fishes follow
Trautman (1981). Base length of median fins is defined
as the distance from the anterior margin of the first
spine or soft ray to the posterior margin at the base of
the last spine or ray. Snout length is the distance from
the anterior margin of the premaxillary to the-anterior
margin of the eye. Interorbital width is the least dis-
tance between orbits. Body depth factor (BDF) and
caudal depth factor (CDF) indicate general body
form and swimming ability (Webb and Weihs 1986).
Body depth factor is defined as mean TL/mean body
depth, whereas CDF = mean caudal peduncle depth/
mean body depth. A high BDF and CDF denotes an
elongate species whose depth is more or less the same
along its length; e.g., clupeid or osmerid. Low values
are found in centrarchids, where manoeuvrability is
enhanced by a deep body and large pectoral fins. Fish
volume, determined in each size class = mean total
length x (mean body depth)’.
Results
Reproductive and nursery habitat
Environmental conditions for fish reproduction and
rearing differed in Duck Creek and the St. Clair River
according to water quality and physical characteris-
tics. On most dates, water temperature at the shore of
the river was about 3°C lower and suspended particu-
late load always lower, than in Duck Creek. Whether
collected at 4° or 30°C, Round Gobies were recorded
in the same habitat from April to November. However,
their occurrence was contingent on availability of
cover. For example, gobies were not found at LGS in
May 1999 when low water level completely exposed
rock and rubble habitat. Recently hatched fish were
rarely found along featureless, sandy shores, where
320
za
Do OI
THE CANADIAN FIELD-NATURALIST
Vol. 118
SS ES
eee a ae
~ a] s
FIGURE 2. Neogobius melanostomus at 7.5 mm; upper: dorsal, middle: lateral, lower: ventral view. Length bar = 1 mm.
juvenile and adult gobies were occasionally caught.
Small boat launches with corrugated concrete ramps
were consistent sources of larger (>30 mm) specimens
of age-0 gobies.
Presence of small age-0 fish in late spring and early
autumn indicates a possible prolonged spawning peri-
od in Duck Creek, accommodated by water tempera-
ture >10°C from early May to mid-October. Earliest
evidence of recently hatched fish (5-13 mm TL) on 1
June 1995 suggests spawning takes place in April or
May. However, in early May 1998, ten gobies (22-28
mm) were caught near LGS at 10°C above ambient
(4°C). These fish may have hatched in late winter in
dilute heated power plant effluent. Since small gobies
(14-23 mm) were found each year in September,
spawning at LGS may extend to late summer.
In Duck Creek, Round Gobies endure continuous
turbid water, enriched conditions, occasional dense
blooms of blue-green algae (Anabeana sp; Cyanophy-
ta) and temperature at least 30°C. According to size
in autumn, gobies attain a mean length of about 33-
39 mm at the end of first year growth. For example,
in Duck Creek fish were 32.8 mm (28-36 mm) in early
October 1995, whereas at LGS, they were 37.6 mm
(range 31-49 mm) in November 1994 and 39.4 mm
(30-45 mm) in November 1995.
Reproduction
In mid-July 1999, numerous clusters of eggs were
found attached to the underside of rocks at a depth of
0.3 m in Duck Creek. A sample (N = 121) of eggs in
a cluster of roughly 200 on a rectangular patch of about
30 cm? averaged 3.0 mm long and 1.8 mm wide with
2004
LESLIE and TIMMINS: AGE-O ROUND GoBY IN ONTARIO 32]
FIGURE 3. Neogobius melanostomus at 25 mm. Length bar = 2 mm.
respective modal values of 3.1 mm and 1.8 mm (range:
2.6-3.3 mm and 1.6-2.0 mm). Eggs are oblong with
rounded base and blunt apex, with a fibre-like basal
pedestal or stalk 0.4-0.5 mm long. Yolk is light orange
and occupies nearly 75% of the capsule. These eggs
incubated in situ in turbid, almost lentic water at 28-
30°C. Similarly, egg clusters were found in early June
2000 at 14°C in the St. Clair River beneath limestone
rocks and human artefacts. A cluster of approximately
300 eggs formed an oval patch (estimated area =
40 cm?) under a rock at a depth of 0.2-0.3 m in slow
flowing water. Eggs (n = 78) were 3.5 mm long and
2.0 mm wide (modal values, 3.7 mm and 2.1 mm).
Morphology
Yolk, which is usually retained in the gut of fish
4.5 to 6.5 mm long, may persist to 11 mm. At 5-8
mm, minute teeth are present on the jaws. Origin of
D1 is at the fourth myomere or fifth vertebra, whereas
D2 originates at the seventh or eighth myomere (elev-
enth or twelfth vertebra). Scales first appear on mid-
caudal peduncle at approximately 8-9 mm and body
scalation may be complete at 12-15 mm.
The upper lip is protractile and jaw articulation is
below the anterior margin of the pupil. The anterior
tubular nostril protrudes, whilst the minute posterior
nostril is flush. At about 13 mm the cranium is de-
pressed, cheeks begin to enlarge, and sub-orbital canals
and papillae are barely visible. At all sizes, the head
is bluntly arrow-shaped in ventral profile (Figure 2).
All spines and fin rays are formed, although principal
rays are incomplete in the caudal fin. Pectoral fin rays
are joined distally by membrane. A small genital papilla
is first obvious at about 23 mm.
Origin of D2 is on a vertical line with the anus and
separated from D1 by a flap of tissue. Full complement
of branched caudal rays is attained at about 20 mm.
At 22-25 mm, the pectoral fins are slightly flared ven-
trally and depressed D2 and anal fins extend equally
to mid-peduncle (Figure 3). Two short, stout spines
support a transverse membrane on the pelvic fin, the
whole forming a suctorial disc.
Fish >30 mm have a moderately rounded snout
and large protruding dorsolateral eyes above bulging
cheeks. Sub-orbital papillae occur in transverse rows
(Figure 4). The tip of the large fleshy upper lip is
anterior to the lower, and the opening of the terminal
mouth lies below the ventral margin of the eye. The
centre of the pupil lies along a horizontal line with the
origin of the pectoral fin. Gill openings are narrow.
Ctenoid scales cover the body, whereas cycloid scales
occupy the anterior nape and gill covers. In outline,
Ficure 4. Lateral view of male Neogobius melanostomus at 38 mm. Length bar = 5 mm.
B22
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE |. Morphometrics for age 0 Neogobius melanostomus collected in the St. Clair ecosystem, Ontario. Lengths are
percentage (with range) of mean total length (TL) in each size class.
Size 5.0-8.9 9.0-12.9 13.0-16.9
class n= 20 m=9 n=2
Mean TL Ussies A 10.4 + 1.2 13301
Standard 79.0 79.3 78.1
73-86 78-83 77-719
Preanal 45.8 43.8 41.5
43-52 42-45 41-42
Predorsal 33.0 Silen 30.6
30-42 30-33 30-32
Prepelvic Pes A| PAE | 27.6
18-30 24-31 27-28
Body depth 17.8 16.8 1GS)59)
14-21 15-18 14-17
Peduncle US 8.0 8.3
6-9 7-9 0
Head 26.2 26.3 27.6
21-30 24-29 27-28
Eye? 30.6 Bilal 27.6
25-37 26-35 27-28
Volume (mm?*) 12.3 30.1 5i5).7/
BDF 5.6 6.1 6.5
CDF 0.42 0.49 0.54
Pectoral fin 18.6 19.7 D5
10-22 17-22 21-22
Pelvic fin 1525 Ne, 19.3
9-21 13-19 18-20
Dorsal | base 7.0 7.8 6.5
5-11 6-10 6-7
Dorsal 2 base 24.3 235 23.4
19-30 20-29 23-24
Anal base 20.5 19.7 18.5
18-24 16-23 17-20
*% head length
D1 is slightly rounded, D2 slopes slightly, and the
anal fin is uniform (Figure 4).
Morphometry
Relative changes in lengths are generally small as
fish grow (Table 1). Head length (24-28% TL) is 1.3
times its width and 1.4 times its depth. Snout length
increased from 15% HL at 7 mm to 20% HL at 35 mm.
Interorbital width, variable among and within size
classes, is 10-22% HL. Pectoral fin rays are 19-24%
TL whereas D2 base is 23-26% TL. Longest spines
and base of D1 are about equal but less than the
longest ray of D2. On fish >35 mm, the pectoral fin
base is approximately 55% greatest body depth. Body
depth and caudal depth factors are generally constant
(Table 1).
Meristics
Respective modal counts for preanal, postanal, and
total myomeres are 12 (range, 11-13), 19 (17-20), and
31 (29-32). Modal spine and fin ray complements are
D1: VI, D2: 1 15 (13-16), anal: I 13 (11-13), pectoral:
18 (16-19), pelvic(s): 1 5 (conjoined), principal caudal:
17.0-20.9 21.0-24.9 25.0-32.9 33.0-39.9
n=9 n= n=33 N23,
18.5+0.9 23.5+0.9 2837 = 21 35.3+ 1.8
80.3 79.8 79.5 80.3
79-83 78-83 77-81 79-82
44.0 44.7 44.0 43.4
43-46 41-48 42-51 39-46
30.1 29.7 29.2 28.2
29-32 28-32 27-31 24-29
DAs 27.0 26.6 26.6
26-28 24-32 25-29 25-34
gh) 16.9 17.6 ei
14-20 15-19 15-20 16-19
9.0 8.9 8.9 8.8
9-10 8-9 9-10 8-10
25.5 253 24.8 24.0
25-27 24-27 23-27 23-26
33.0 32.4 B22 30.3
31-35 28-35 28-35 26-35
189 35 ii 2 1401
5.8 6.0 Si 5.6
0.53 0.52 0.51 0.50
23.6 24.0 DES) 23.6
22-25 22-25 19-27 21-26
203 19.9 20.1 19.8
20-22 18-21 18-22 17-23
8.8 8.5 9.0 9.2
8-9 7-12 8-11 7-11
pip) 24.7 25.9 DS)
24-28 20-29 24-27 24-27
19.6 19.2 20.6 20.4
17-22 17-22 17-23 19-23
13 (11-13). There are 33 modal (32-33) vertebrae and
49 (48-52) ctenoid scales in mid-lateral series.
Pigmentation
On free embryos, pigmentation consists of black
eyes and several black spots on posterior spines of
D1. However, on many specimens <9 mm, the char-
acteristic black spot on D1 is absent. Speckled mel-
anophores on snout and dorsum of head, a dark crescent
on the occiput and a small patch on the cheek are
typical at 10-12 mm. Ventrally, an elongate stellate
melanophore is situated mid-gut. About five faint
dorsolateral clusters are expressed on the body. There
is a small group of stellate melanophores on frontal
and parietal areas, a ventral patch on the pectoral fin
base and a subcutaneous series on the intestine. Mel-
anophores develop at the base of each anal fin ray,
and a narrow mid-ventral series prevails from anal fin
base to caudal fin base (Figure 2). At 14 mm, striation
extends from maxilla to orbit and a black spot is
pronounced between fifth and sixth spines on D1.
Several faint mid-lateral blotches extend the length
of the body.
2004
LESLIE and TIMMINS: AGE-O ROUND GoByY IN ONTARIO 323
FiGuRE 5. Cottus bairdi at 10.5 mm. Length bar = | mm.
At 22-25 mm a large brown patch is obvious on
the dorsal peduncle of the pectoral fin. First four rays
of D1 are lightly pigmented, and patches appear on
the base of interradials. A faint stripe exists mid-fin on
D1 (Figure 3). Posterior margins of body scales are
darkly outlined and rays at the base of the caudal fin
are lightly pigmented. A small basicaudal spot persists
throughout development.
Fish >30 mm have a small stripe on the preopercle,
and about seven irregular patches of brown pigment
on the side of the body, mainly below the mid-line.
Otherwise, lips and dorsum of head are covered with
small round spots, whilst the throat is essentially de-
void of pigment. Pelvic and caudal fins are lightly
spotted, whereas D2 has two pale longitudinal stripes.
Pigmentation patterns are intensified over head, body,
and fins (Figure 4). Overall colouration on individuals
varies from dark brown to grey-brown.
Description of age-O Mottled Sculpin
Mottled Sculpin larvae (11.4 + 1.1 mm; n = 5)
have the following characters: preanal length 41%
TL, head 25%, eye 29% head length; head length and
width equal; predorsal length 29% TL, prepelvic length
24%. Branchiostegals 3,4. Except for pelvic fin sep-
aration, overall body characters are similar to gobies
(Figure 5). Pigmentation features black eyes and
approximately six lateral saddle marks on the body.
Melanophores are absent on the ventral body surface
and fins. Meristics for this, and superficially similar,
species are given in Table 2.
Discussion
The Round Goby is an eurythermal fish adapted to
slightly brackish environments in the Caspian and
Black seas (Miller 1986). In the Great Lakes basin it
is ubiquitous in the littoral zone, including ecotones
intolerable to many of our native fishes. Eggs incu-
bate in almost static water in Duck Creek, a stream
burdened with silt, and at times, blooms of blue-
green algae at high temperatures. Concurrently, eggs
may develop in the St. Clair River in water of high
quality and clarity at temperatures several degrees
lower than in small turbid streams in the same catch-
ment. The reproductive strategy includes parental
guarding of eggs and free embryos. In the St. Clair
aquatic ecosystem, age-O0 Round Gobies appear to
remain natal stream and shore habitats throughout
their first year of growth. Solid objects, unlike sand
and other unstable substrates, provide surfaces essential
for attachment and refuge for small gobies in flowing
water.
Reproduction is prolonged and extensive but varies
geographically. In their native range, gobies migrate
to spawning habitat at 9-26°C and reproduce from
April-September in intervals of 3 or 4 weeks (Charle-
bois et al. 1997). Similar data for the Great Lakes are
lacking, although MacInnis and Corkum (2000) suggest
a possible spawning period from April to November
in the upper Detroit River. In power plant cooling
water discharges, the reproductive period may extend
from winter to late summer or beyond, since the endo-
crine system is active all year (Charlebois et al. 1997)
and water temperatures are constantly >10°C.
TABLE 2. Comparison of meristics of several Great Lakes age-0 fishes superficially similar in appearance.
Species D1 D2 Pelvic Pectoral Anal Preanal _Postanal
fin fin fin fin myomeres myomeres References
Etheostoma exile VII-X LO=12 5 12-14 II, 7-8 Heufelder 1982
Etheostoma nigrum VIl-XI 10-14 5 11-12 EWVealO els Bil Heufelder 1982
Etheostoma caeruleum x 12 6 13 ind) 16-17 18-19 Cooper 1979
Cottus bairdi VIL-IX 16-19 I, 3-4 13-17 13-14 9-12 19-21 Heufelder 1982
VIL-VIN =15-17_ I, 3-4 13-15 13 9-10 19-21 This study
Cottus cognatus VII-IX 16-19 1, 3-4 12-16 10-14 9-12 19 Heufelder 1982
Proterorhinus marmoratus VI-VII 16-19 1,5 14-15 | is) 11 20 Leslie et al. 2002
Neogobius melanostomus VI 1S =1G) les 18 iatles} 12 19 This study
324
In the study area, batches of about 200-300 eggs
represent an absolute fecundity of 800-1200, assuming
four spawning episodes. MacInnis and Corkum (2000)
estimated an absolute fecundity of 252-1818 eggs based
on three spawning episodes from late May to the end
of July in the upper Detroit River. Miller (1986) report-
ed fecundity of gobies 7-13 cm long as 328-5221 in the
Black-Caspian-Azov seas, whilst Kuczyfiski (1995)
calculated 2700-3000 eggs in the Gulf of Gdansk. In
general, fecundity is lower and eggs slightly smaller
(3.7-3.9 mm long, 2.0-2.2 mm wide) than in the Black
and Baltic seas, possibly because the spawning popu-
lation is younger and fish are smaller (MacInnis and
Corkum 2000).
Moskal’kova (1967) reared embryos that emerged
from the egg at 5.5-5.7 mm and remained in the nest
4-9 days. Gobies do not have a true larval stage (Miller
1986) and hatch with most characteristics of juveniles.
However, in the present study, smallest gobies (4.5-
5.0 mm) feature a large yolk sac and incomplete com-
plement of fin rays. These fish may have extruded from
eggs during the collection process and perhaps are not
representative of free embryos. Otherwise, smallest
specimens found in coarse gravel were clearly un-
guarded, free-living fish.
The Round Goby is a cryptic, benthic fish, devoid
of air bladder and planktonic stage. As such, early
developmental stages are found in and among firm
structures. Gobies have smaller caudal and body depth
factors than larvae capable of high thrust and acceler-
ation, such as Anchovy (Eugraulidae), Alewife (Clu-
peidae) or percids (C. A. Timmins, unpublished, 2000).
The Round Goby may not be a strong or fast swimmer,
but its large head, robust body, and large pectoral fins
enhance its manoeuvrability.
Age-0 Round and Tubenose gobies did not co-occur
in any given habitat in the St. Clair ecosystem, al-
though they partitioned habitat in a small area near
the mouth of Duck Creek (Leslie and Timmins 1998).
Usually, small age-O Round and Tubenose gobies may
be separated on the basis of head and body pigmen-
tation, which is much lighter in the former. Whereas
the Round Goby has a conspicuous black spot on the
posterior spines of D1, the Tubenose Goby has an
oblique stripe on anterior spines. Further, tubular nos-
trils that extend beyond the upper lip are peculiar to
the Tubenose Goby. However, most mensural char-
acters overlap for these gobies. Thus, small (<6 mm)
unpigmented fish may not be separable.
Fishes with similar habitat requirements and mor-
phology, such as cottids, darters, and gobies sometimes
co-occur. Recently hatched Mottled Sculpins are pre-
cocious and appear similar to gobies (Figure 5).
However, all fins are developed in recently hatched
Round Gobies, whereas cottids (and darters) have a
complete fin fold and separate pelvic fins, which are
expressed some weeks post-hatch. In addition, pre-
anal and total myomere counts of cottids and darters
THE CANADIAN FIELD-NATURALIST
Vol. 118
do not overlap with those of gobies. Fin spine and ray
counts and pigmentation patterns also differ among
these taxa.
The Round Goby has survival advantage over many
competitors. It reproduces repeatedly from spring to
autumn, the critical life stage is not determined by
specific seasonal type or quantity of food, its embryos
hatch with almost all external structures elaborated,
the young are guarded in nests and it persists in natal
habitats. Certainly, few native fishes of the Great Lakes
basin are as morphologically and physiologically suit-
ed to thrive in comparable environmental conditions.
Therefore, geographic range expansion and prolifer-
ation of the species seems likely in the Great Lakes
Basin.
Acknowledgments
R. E. Dermott, Department of Fisheries and Oceans,
Burlington, Ontario, kindly provided specimens of
mottled sculpin. We thank two anonymous reviewers
for comments that improved the manuscript.
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Received 17 February 2003
Accepted 15 November 2004
A Systematic Analysis of the Alpine Saxifrage Complex (Saxifragaceae)
in the Canadian Arctic Islands Using Morphology and Chloroplast
DNA Data
CAROLINE HEALY! and LYNN J. GILLESPIE
Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada
' Present address: Department of Biology, University of Ottawa, P.O. Box 450, Station A, Ottawa, Ontario KIN 6N5 Canada
Healy, Caroline, and Lynn J. Gillespie. 2004. A systematic analysis of the alpine saxifrage complex (Saxifragaceae) in the
Canadian Arctic Islands using morphology and chloroplast DNA data. Canadian Field Naturalist 118(3): 326-340.
The Saxifraga nivalis complex displays significant ecological, morphological and cytological variation. Most European studies
suggest that the S$. nivalis complex comprises two distinct species: Saxifraga nivalis sensu stricto and Saxifraga tenuis.
However, the presence of intermediate morphotypes, inconsistencies in chromosomal counts and variability in morphological
keys and descriptions have led to different taxonomic interpretations of the complex in North America. This study investi-
gated the systematics of Canadian Arctic Island members of this complex from 157 specimens using 23 morphological
characters. Principal component analysis of the morphological data revealed two adjacent clusters, corresponding to the two
taxa and consistent with a close morphological similarity and the presence of hybrids. A preliminary restriction site analysis
of five non-coding regions of the chloroplast genome, trnH-trnK, trnT-trnF, trnF-trnV, trnV-rbcL and rbcL-ORF106, was
conducted using 21 restriction endonucleases. This analysis indicated a length difference between the trnT-tvnF region of S.
nivalis and that of S. tenuis, but no difference in restriction sites for any of the assayed regions. These results confirm that in the
Canadian Arctic, the S. nivalis complex consists of two closely related, largely sympatric species, with notable morphological
variability, and possible hybrids.
Key Words: Alpine Saxifrage, Saxifraga nivalis, Saxifraga tenuis, Canadian Arctic, systematics, morphology, chloroplast
DNA restriction site analysis.
Saxifraga L., the largest genus in the Saxifragaceae,
consists of nearly 400 herbaceous, mostly perennial
species (Webb 1993; Soltis et al. 1993, 1996). Saxi-
fraga nivalis L. sensu lato, commonly known as the
Alpine Saxifrage, inhabits arctic and alpine environ-
ments throughout the northern hemisphere. The S.
nivalis complex is dispersed throughout northern and
alpine Europe, Siberia, arctic and subarctic North
America and south in the alpine zone to Arizona and
the Gaspé, Quebec (Britton and Brown 1913; Krause
and Beamish 1973; Scoggan 1978; Webb 1993).
Members of the S. nivalis complex display notable
morphological, cytological and ecological variation,
which has led to different taxonomic interpretations
and classifications.
Linnaeus (1753) first described S. nivalis, a name
that means snow saxifrage, as these plants are often
found growing in snow patch plant communities (Brit-
ton and Brown 1913). Later, Wahlenberg (1812) recog-
nized S. nivalis var. tenuis Wahlenb. for plants with a
notably smaller stature, fewer flowers, smaller fruits
and recurved stigmas. Smith (in Lindman 1918) elevat-
ed Wahlenberg’s variety to Saxifraga tenuis (Wahlenb.)
Harry Sm. However, the taxonomy of the S. nivalis
complex remained problematic and the acceptance of
S. tenuis as a species was controversial. For instance,
Bocher (1938) recognized S. nivalis and S. tenuis as
distinct species, but also suspected the presence of races
and microspecies within the S. nivalis complex. Polunin
(1940) found the two taxa difficult to separate morpho-
logically with intermediates and suggested the need for
breeding and cytological studies before distinguishing
them at the species level. Although accepted as a dis-
tinct species in Scandinavia and Greenland, based on
samples from Alaska and the Yukon, Hultén (1945)
concurred at the time with Polunin in treating the
taxon as S. nivalis var. tenuis because of its minimal
phenotypic distinction from S. nivalis and its low fre-
quency of occurrence within the area of distribution of
S. nivalis. However, in the Canadian Arctic, Porsild
(1957, 1964) and Porsild and Cody (1980) recognized
S. nivalis and S. tenuis as distinct species. Upon fur-
ther examination of specimens from Alaska and neigh-
boring regions, Hultén (1968) also recognized the
two taxa at the species level. More recently Scoggan
(1978) and Aiken et al. (1998) treat the two taxa as
varieties of S. nivalis.
Taxonomic and nomenclatural ambiguity also
stemmed from the description of additional varieties and
microspecies, as well as the re-emergence of Haworth’s
(1812) suggestion to revise Linnaeus’ concept of the
genus Saxifraga (reviewed in Spongberg 1972). In
1905, Small divided the genus Saxifraga into 13 genera
in North America (in Small and Rydberg 1905;
reviewed in Soltis et al. 1996). Small treated S. nivalis
as Micranthes nivalis (L.) Small, S. nivalis var. tenuis
as Micranthes tenuis (Wahlenb.) Small, and distin-
guished an additional species in the Canadian eastern
Arctic, Micranthes kumlienii Small. However, subse-
quent authors did not recognize the genus Micranthes,
326
2004
and M. kumlienii was treated as belonging to S. nival-
is (Polunin 1940; Aiken et al. 2000*). Fernald (1917)
distinguished Saxifraga nivalis var. labradorica Fern.,
a variety localized in Labrador, and suggested that this
plant corresponded to Small’s concept of Micranthes
tenuis. Subsequently, this variety was treated as a syn-
onym of S. nivalis var. tenuis (Scoggan 1978) or as a
luxuriant form of the latter (Polunin 1940). In the Gaspé
Peninsula, Fernald (1917, 1950) identified another
member of the S. nivalis complex, Saxifraga gaspensis
Fern. Subsequently, this species was included under
S. nivalis var. tenuis (Scoggan 1950, 1978), treated as
S. nivalis var. gaspensis (Fern.) Boivin (Boivin 1966),
and then considered as small S. nivalis s.s. (Blondeau
1989a). Most recently, Gervais et al. (1995) followed
Fernald in treating the Gaspé population as a distinct
species. In Alaska, Hultén (1968) considered S. nivalis
as highly variable, recognizing S. nivalis var. tenuis,
and describing S. nivalis var. rufopilosa Hultén for
plants characterized by “densely pubescent, rufous-
haired leaves and red petals” (page 579) found in
Alaska and the Yukon. Porsild (1957, map page 188)
appeared to treat S. rufopilosa under S. tenuis ac-
cording to his map of that species (see also Porsild and
Cody 1980, map page 403; Cody 1996). Later, Porsild
(1975) recognized the latter as the distinct species, S.
rufopilosa (Hult.) A. E. Porsild, and suggested that it
was more closely related to S. tenuis than S. nivalis.
Cody (1996) also recognized S. rufopilosa as a distinct
species and considered S. tenuis as not present in the
Yukon. In 1978, Scoggan’s concept of S. nivalis var.
tenuis encompassed S. tenuis, S. gaspensis, S. nivalis
var. labradorica and S. nivalis var. rufopilosa.
Based on cytology and morphology, Love (1983)
and Webb (1964, 1993) discerned the species S. nivalis
(2n = 60) and S. tenuis (2n = 20) in Europe. The taxo-
nomic ambiguity regarding the S. nivalis complex in
North America (Aiken et al. 2000*) appears to stem
from the following factors: (1) several morphological
characters used to distinguish the species in Europe
do not hold up in North America; (2) taxa can be found
growing together; and (3) intermediate morphotypes,
as well as variation in chromosomal counts suggest
hybridization. Various cytological studies of material
from North America have demonstrated cytological
diversity within the S. nivalis complex with chromo-
somal counts of 2n = 20, 40, c. 56, 58, 60 or c. 60.
While most support the above European counts for S.
nivalis and S. tenuis (Mosquin and Hayley 1966; Hed-
berg 1967; Johnson and Packer 1968; Packer and
McPherson 1974; Love and Love 1975), several studies
found intermediate chromosome counts. Krause and
Beamish (1973) provide counts for plants of the S.
nivalis-tenuis complex from the Yukon (2n = 20, 40),
British Columbia (60) and Idaho (20), which they were
unable to identify to species. Intermediate chromosome
counts have also been found in the Russian Arctic in
a plant described as S. nivalis x S. tenuis (Devyatov et
HEALY AND GILLESPIE: ALPINE SAXIFRAGE COMPLEX 327
al. 1997). In the Gaspé Peninsula S. gaspensis is con-
sidered to be a putative endemic hybrid based on chro-
mosome number (2n = 40) and apparent intermediate
morphology (Gervais et al. 1995). Further confusion
results from the variance and discrepancies among the
morphological keys used in the identification of this
complex and related species, such as S. foliolosa R.
Br., which are occasionally misidentified as members
of the S. nivalis complex. Consequently, accurate and
consistent identification of North American plants
belonging to this complex can be problematic.
The aim of this study was to investigate the distinc-
tiveness of S. nivalis and S. tenuis in the Canadian
Arctic Islands based on morphological and molecular
differences, and to help reassess the taxonomic status
of S. tenuis.
Material and Methods
Morphological Analysis
Specimens
Representative specimens from the Canadian Arc-
tic were selected from the Canadian National Herb-
arium, Canadian Museum of Nature (CAN), and the
Agriculture and Agri-foods Canada Herbarium, Cen-
tral Experimental Farm, Ottawa (DAO). Morphological
data were gathered from observations and measure-
ments on 157 herbarium sheets (listed in Appendix
I), including two chromosome count vouchers (S.
nivalis, 2n = 60, Calder et al. DAO 24148: S.. tenuis,
2n = 20, Calder et al. DAO 24149). One plant per
sheet was sampled, except when sheets comprised
mixed collections or included DNA vouchers, and
then multiple plants per sheet were sampled. A total
of 200 plants were sampled, 122 S. nivalis and 78 S.
tenuis. More specimens of S. nivalis were available for
study than of S. tenuis. Where identifications of exam-
ined specimens were judged questionable, specimens
were re-identified based on a combination of published
keys and preliminary results. Additionally, identifica-
tions of many S. tenuis specimens at CAN were sub-
sequently confirmed for the Panarctic Flora Project
(E. Reidar, 2001, 2002).
Morphological characters
Characters used in descriptions and keys of the S.
nivalis complex (Simmons 1906; Polunin 1940; Porsild
1957; Love 1983; Blondeau 1989a, 1989b; Webb
1993; Aiken et al. 1998, 2000*) were reduced to a set
of 30 characters based on ease of observation or meas-
urement on dried specimens as well as their taxonom-
ic significance. Of these, 23 were selected for statis-
tical analysis (Table 1). Petal length was excluded
from all analyses due to difficulties in measuring petals
that were often folded and partly included within the
calyx. The qualitative characters, stem colour, petal
shape, prominence of leafy bract on stem, leaf blade
shape, leaf blade base shape and apex shape, were
excluded due to variation within a plant or difficulties
in determining discrete states.
328
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE |. Morphological characters used in analyses of the Saxifraga nivalis complex in the Canadian Arctic.
Quantitative characters:
Hair length on leaf lower surface (mm): UNDHRLGTH
Hair length along leaf margin (mm): MRGHRLGTH
SOC eE ES ON Calipers) Ei
Plant height (cm): HEIGHT; length from basal rosette to top of inflorescence
Stem width (mm): STWIDTH; measured midway along lower half of stem
Stem hair density (0, glabrous to 4, dense): STHRDENSITY
Stem hair length (mm): STHRLENGTH; measured midway along lower half of stem.
Leaf blade length (cm): LFLENGTH; measurement made on the largest leaf
Leaf blade width (em): LFWIDTH; measurement made on the largest leaf
Number of teeth on leaf: TEETH; count made on the largest leaf
10. Tooth width (mm): TTHWIDTH; measurement made on largest tooth on the largest leaf
11. Tooth length (mm): TTHLENGTH; measurement made on largest tooth on the largest leaf
12. Petal width (mm): PTWIDTH; measurement made on the largest petal
Qualitative characters:
Stem hair texture (short fine; long coarse)
Tooth apex shape (rounded; pointed)
Hair colour on leaf lower surface (rust; white)
Hair colour on leaf margin (rust; white)
Inflorescence density (open; tight cluster)
10. Style shape (curved; straight or essentially so)
SEN SION a eS
11. Petal colour (pink or essentially so; white or essentially so)
The software package DELTA (Dallwitz et al. 1993)
and the character set for the “Flora of the Canadian
Arctic Archipelago” (Aiken et al. 2002*) were used to
generate preliminary taxon descriptions. These descrip-
tions were then modified to read more easily, to ex-
clude irrelevant characters, and to include important
diagnostic characters not included in the Flora char-
acter set.
Statistical analysis
All statistical analyses were performed with SYSTAT
version 8.0. For each quantitative trait, the means for
S. tenuis and S. nivalis specimens were compared by
performing t-tests. Separate variance values were cal-
culated for each taxon. T-tests were conducted on both
raw and log-transformed data. A principal component
analysis (PCA) using the 12 quantitative characters in-
dicated in Table 1 was conducted to visualize possible
distinctiveness between S. nivalis and S. tenuis. The
character MRGHLGTH was excluded from some PCA
analyses due to a large amount of missing data in S.
tenuis, which sometimes lacked marginal hairs. The
PCA analysis excluded all specimens with missing
values. A discriminant function analysis was also per-
formed on the quantitative data. For the 11 selected
qualitative characters (Table 1) the percentages of spec-
imens having each character state was determined for
each taxon.
To determine if there was any geographical pattern
to the morphological variation in S. tenuis, principal
component analysis was performed only on the S.
tenuis quantitative data (excluding MRGHLGTH).
This analysis also included five specimens from Alas-
Stem hair colour (rust-coloured; mixed rust and white; white)
Regularity of teeth (even in size; variable in size smaller towards leaf blade apex)
Hair presence on leaf lower surface (moderate to dense; sparse; absent)
Hair presence on leaf margin (moderate to dense; sparse; absent)
ka (Calder 6107, 6511, 6249 DAO) and northern
British Colombia (Calder & Kukkonen 28151 DAO,
Taylor et al. 1204 DAO) not included in the larger
analysis. Individuals were coded as occurring in one
of three regions: high arctic (67), eastern arctic (11)
or western montane (5).
Chloroplast DNA analysis
Plant material and DNA extraction
A total of 15 plants, for which silica gel dried mate-
rial was available, were selected for molecular analysis:
seven individuals of S. nivalis (Gillespie 6165, 6675-1,
6826a-1, 6826a-2, 6977-2, 6984-5; Aiken 98-055-3),
seven S. tenuis (Gillespie 6728-1, 6807-1, 6807-3,
6825-2, 6870-2, 6877-1, 6881-3), and one S. foliolosa
(Gillespie 6841) (Appendix 1). The latter species was
selected to provide perspective on the chloroplast
DNA (cpDNA) data, based on its close phylogenetic
relationship to the S. nivalis complex (Soltis et al.
1996). DNA was extracted following Doyle and Doyle’s
(1990) CTAB total DNA extraction procedure as
modified by Gillespie et al. (1997).
Restriction site analysis
DNA extracts were PCR amplified using five pairs
of universal primers for non-coding regions of chloro-
plast DNA. The five regions are: tmmH-tmmK (Demesure
et al. 1995), trnT-trnF (Taberlet et al. 1991), trnF-trnV
(Dumoulin-Lapegue et al. 1997), trnV-rbcL (Dumou-
lin-Lapegue et al. 1997), and rbcL-ORF106 (Arnold
et al. 1991). Amplification reaction mix and programs
follow Gillespie and Boles (2001).
2004 HEALY AND GILLESPIE: ALPINE SAXIFRAGE COMPLEX 329
TABLE 2. Descriptive statistics and t-test comparing the means of S. nivalis and S. tenuis at the 95% confidence level for 12
quantitative morphological characters.
Range Difference
Character Taxon N Mean (+SD) Min Max in means t value df p
S. nivalis 122 OFZ) CE3'3i7) af AsO)
Plant height (cm) 4.66 13.68 176.2 0.000
S. tenuis 78 4.40 (+1.40) 1.8 8.5
S. nivalis 122 1.37 (+0.35) 0.7 DES
Stem width (mm) 0.82 23.06 178.6 0.000
S. tenuis 78 0.56 (+0.15) 0.3 1.0
S. nivalis 122 3.2 (+ 0.70) 1 4
Stem hair density 2.0 24.94 205.0 0.000
S. tenuis 78 1.2 (+ 0.36) 1 3}
S. nivalis 1:22 3.2 (+ 0.70) 1 4
Stem hair length (mm) 0.67 35.45 188.5 0.000
S. tenuis Tal 0.19 (+0.09) 0.1 0.5
S. nivalis 119 0.96 (+0.34) 0.4 Dil
Leaf blade width (cm) 0.51 14.81 161.2 0.000
S. tenuis 77-044 (+0.13) 0:25 570!8
S. nivalis 119 1.38 (+ 0.50) 0.6 3.6
Leaf blade length (cm) 0.69 13.51 166.5 0.000
S. tenuis TL 0.67 (+ 0.18) 0.4 IES
Hair length on lower S. nivalis 120 0.38 (+0.13) 0.2 12,
leaf surface (mm) 0.10 725) 97:08 70/000
S. tenuis 78 0.27 (+0.06) 0.1 0.5
Hair length on S. nivalis 121 0.19 (+ 0.07) 0.1 0.4
leaf margin (mm) 0.07 8.47 167.4 0.000
S. tenuis 55% 0.12 (+ 0.04) 0.1 0.2
Number of teeth S. nivalis 118 10.3 (+1.74) 7 14
on leaf blade 2.8 16.63 167.8 0.000
S. tenuis 78 7.5 (40.73) 6 9
S. nivalis 118 1.17 (+ 0.42) 0.5 3h)
Tooth width (mm) 0.37 7.86 195.6 0.000
S. tenuis 78 0.80 (+ 0.24) 0.5 1.6
S. nivalis 118 1.52 (+0.48) 0.8 B82.
Tooth length (mm) 0.62 11.84 190.5 0.000
S. tenuis 78 0.90 (+0.26) 0.4 1.8
S. nivalis 120 1.12 (+0.24) 0.7 1.8
Petal width (mm) 0.40 14.16 202.0 0.000
S. tenuis al 0.72 (+0.16) 0.5 il
* Marginal hair was not present in all S. tenuis
PCR products were single digested with twenty one Apal, BamHI, Bgil, BglII, Dral, EcoRI, EcoRV, Hincll,
restriction endonucleases according to manufacturer’s PstI, XhoI. To separate restriction fragments, 8 uL of
recommendations. These included nine 4-base pair the reaction mixture and 2 uL of buffer-dye mix were
(bp) cutting restriction enzymes: Alul, Haelll, Hhal, run on 1.1% agarose gels with ethidium bromide at
Mspl, Rsal, Ddel, Hinfl, Sau96], Taql; two 5bp cutting 38 V for 2-3hrs. The restriction fragment patterns were
restriction enzymes: BstOl, SinI; and ten 6bp enzymes: visualized and photographed under ultraviolet light.
330
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 3. Distribution of qualitative morphological character states in Saxifraga nivalis and S. tenuis in the Canadian Arctic.
Numbers represent percentage of individuals having a particular character state.
Character Character state
Stem hair colour rust
mixed
white
Stem hair texture short fine
long coarse
Tooth apex shape rounded
pointed
Regularity of teeth even-sized
variable
Hairs presence on leaf lower surface moderate-dense
sparse
absent
Hair colour on leaf lower surface rust
white
Hair presence on leaf margin moderate-dense
sparse
absent
Hair colour on leaf margin rust
white
Inflorescence density open
tight cluster
Style shape curved
straight
Petal colour pink
white
Lengths of total amplified product and restriction frag-
ments were estimated by comparison with known
100 bp ladder DNA markers.
Results
Morphological Analysis
To determine whether the means of the examined
quantitative characters were different between S. nivalis
and S. tenuis, t-tests were performed (Table 2). The
analysis revealed a significant difference in means be-
tween the two taxa for all characters examined. Overall,
plants belonging to S. nivalis are more robust than S.
tenuis as implied by higher means in both plant height
and stem width observed in S. nivalis. Similarly, leaves
of S. nivalis are on average longer, wider and have
longer, wider and more numerous marginal teeth than
S. tenuis. Also, hairs on the stems are longer and denser
and hairs on the lower surface and margin of leaves
are on average longer in S. nivalis. Petal width was sig-
nificantly greater in S. nivalis than in S. tenuis. How-
ever, the two taxa have notably different variances,
with S. nivalis having a higher variance than S. tenuis
for all quantitative characters examined. Considering
the very low probability values and the robustness of
t-tests for samples of this size, the differences in means
can be considered as meaningful. Analyses were also
performed on log-transformed data, with no significant
differences.
The frequency of occurrence of states of qualitative
characters differed considerably between the two taxa
S. nivalis S. tenuis
3} 74.4
0 25.6
98.7 0
1.6 100
98.4 0
DNS 100
97.5 0
18.3 87.2
81.7 12.8
91.7 84.6
es 15.4
0.8 0
40.0 79.5
60.0 20.5
91.7 10.3
8.3 60.3
0 29.5
20.7 60.0
79.3 40.0
1.8 97.1
98.2 2.9
25.9 84.7
74.1 15}3)
14.9 81.8
85.1 18.2
for most characters (Table 3). The characters, stem hair
colour and texture, tooth apex shape and inflorescence
density, differed significantly between the two taxa,
with less than a five percent overlap in states. Several
characters, regularity of teeth, petal colour and style
shape, exhibited an overlap in states of 10-26% between
the two taxa. In contrast, one character, hair presence
on lower leaf surface, displayed very similar frequen-
cies of states between S. nivalis and S. tenuis, with
hairs present in over 95% of the specimens examined
in both taxa, although density was sometimes more
sparse in S. tenuis. The remaining characters displayed
considerable overlap in states between the taxa.
The principal component analysis of quantitative
characters (excluding MRGHLGTH) revealed two
clusters, positioned adjacent to each other with little
overlap (Figure 1). Factor loading for the analysis was
STWIDTH, LFWIDTH, LFLENGTH, STHRLENGTH,
STHRDENSITY, HEIGHT, TEETH, PIWIDTH and
TTHLENGTH for factor 1, and TTHWIDTH and
UNDHRLGTH for factor 2, with 61% and 10% of total
variance explained by factors | and 2, respectively. As
noted above, there is considerable variation among S.
nivalis plants for most examined characters. This can
be observed on the graph through the large oblique
spread of S. nivalis compared to S. tenuis. The PCA
including the character MRGHLGTH produced very
similar results (although displayed fewer individuals).
The discriminant function analysis performed on the
same data distinguished between the two taxa 100%
2004
5
4
3
2) ORO
Q 1 On S Boo GS ‘OP
2 ©
O
<=
LL
9)
ES
-4
5
5 -1 0 { : :
FACTOR(1)
FIGURE |. Principal component analysis on the quantitative
morphological data set for the Saxifraga nivalis com-
plex in the Canadian Arctic. Circles represent individ-
uals of S. nivalis, crosses represent S. tenuis.
of the time, with one dimension accounting for the
variation.
The PCA analysis examining geographical patterns
to morphological variation in S. tenuis revealed very
little geographical structure, with eastern arctic and
high arctic plants almost completely overlapping.
HEALY AND GILLESPIE: ALPINE SAXIFRAGE COMPLEX 33]
Western montane plants separated from the majority
of arctic plants on a combination of both factors (with
LFWIDTH, LFLENGTH, and TEETH, loading high
on factor one, HEIGHT on factor two), but overlapped
considerably with several eastern arctic plants. A dis-
criminant function analysis performed on the three
geographic groups produced similar results (correctly
placing the western montane plants with 100% reli-
ability, high arctic plants with 86% reliability, and
eastern arctic plants with only 42% reliability).
Chloroplast DNA analysis
The trnH-trnK amplicons were estimated at 1600
base pairs (bp) for S. nivalis and S. tenuis and 1700 bp
for S. foliolosa. The three largest regions, trnF-trnV,
trnV-rbcL and rbcL-ORF106, were approximately
3000 bp in length in all three taxa. Interestingly, the
tnT-trnF region was estimated to be 1800 bp, 1850 bp
and 2000 bp in length for S. nivalis, S. tenuis and S.
foliolosa, respectively.
Sixteen out of 105 enzyme restriction assays showed
restriction site differences between S. foliolosa and
the S. nivalis complex, including three site differences
in the trnH-trnK region, three in the rbcL-ORF106
region, three in the trnV-rbcL region, five in the trnF-
trnV region and two in the trnT-trnF region (Table
4). No restriction site differences were detected bet-
ween S. nivalis and S. tenuis. However, digestion of
the trnT-trnF region with the restriction enzyme Alul
showed clearly the length difference between S.
nivalis and S. tenuis (Figure 2).
Table 4. Data matrix of restriction site characters for S. nivalis (N), S. tenuis (T) and S. foliolosa (F). “0” represents absence
of restriction site; “1” represents presence of restriction site.
trnH-trnK rbcL-ORF106
NTF INGE
Alu I eal ie 1b kl
Apal 000 000
BamHI 000 eeleall
Bell 000 000
Bel Il 000 Ave let
BstO I 001 Ethel
Dral 001 lO
EcoRI 000 Ikea
EcoR V 000 ae al
Hae It Hee al 001
Hha lI 000 000
Hinf I lbw eal
Msp I ha al hiked
j sO lal al
apna iL hal
000 000
000 Write al
Pal il ilies al
ie ihel oak il
000 001
000 000
trnT-trnF
NTF
trnF-trnV
INiglge
trnV-rbcL
NTE
DR RP eB RrP ORR RRP rR OOOO COOCCrF
ORB Re RP ROR RFP RRP rR OCOCOCOCOCCOOF
CORR RRB BS OR RP RB Re RO OrR KR OOF OF
eee Re RK Or Fer COOCOCcoocoocoorcoor
[St ee a) ees) (5) oa ea) (Fea) fos
OPER ROORHEH OHM OH COOCOOH
SPSS LOLS shore Oise SO oro Sc
See =O Ores Orr Ore SO Ora Ore SS
OororcjooroqooqococrreKScocorf
Oo
Oo
Nw
THE CANADIAN FIELD-NATURALIST
Vol. 118
MNNTTTTNNT F
FiGuRE 2. Digestion of the chloroplast DNA region trnT-trnF with restriction enzyme Alul for Saxifraga nivalis (N), S.
tenuis (T) and S. foliolosa (F). The first lane contains a 100 bp DNA size marker (M). Note absence of the upper band
on S. nivalis.
Discussion
The principal component analysis confirms that the
S. nivalis complex in the Canadian Arctic is represent-
ed by two principal morphotypes, appearing as adjacent
clusters on the PCA graph. The several plants occu-
pying an intermediate position between the two clus-
ters displayed a somewhat intermediate morphology,
but nevertheless could readily be assigned to one of
the two taxa. For example, several specimens of S.
nivalis from Prince Patrick Island (e.g., Gillespie &
Consaul 6869-4, 6926a-3) were very small with slender
flowering stems, characters typical of S. tenuis, but
otherwise had the morphological characteristics of S.
nivalis. Although character states or ranges overlapped
for the majority of characters examined, differences
between the two taxa were statistically significant for
all quantitative and for three qualitative characters.
Morphological variability
A significant amount of variance was observed for
most characters measured. Since the S. nivalis complex
is considered an environmental indicator (Aiken et
al. 1998, 2000*), the variability observed may be due
to phenotypic plasticity and variation in environment.
For instance, S. nivalis plants growing in harsher
habitats are usually shorter and less robust (e.g., the
very short plant shown in Figure 3) than those grow-
ing in more nourishing environments. Also plants of
S. nivalis may be taller with more slender stems in
shady microhabitats as a result of etiolation. Another
contributor to variance is the time of collection. Since
stems elongate in the fruiting stage, particularly in S.
nivalis, plants collected later in the season are more
likely to be taller than their younger counterparts.
However, most examined collections of S. nivalis and
S. tenuis made at the same time and site displayed
significant height differences on average between the
two taxa. Leaf characters, such as leaf size and teeth
number and size, showed much variation both within
and between the two taxa. Although S. tenuis is usu-
ally found in wetter habitats than S. nivalis, the latter
species in particular occupies a broad range of habitats
and the two species sometimes co-occur in mixed
populations. Some of the morphological variation in
the complex, particularly within S. nivalis, may reflect
this variation in habitat (Blondeau and Cayouette 2002;
Aiken et al. 2000*). Such high intraspecific variation
is apparently typical of Saxifrages, particularly in arctic
and alpine environments, and several studies have
demonstrated that such variation may not be of taxo-
nomic significance (Soltis et al. 1996; Brysting et al.
1996).
The coloration of petals also varied within each
taxon, but season and environment can be a large con-
HEALY AND GILLESPIE: ALPINE SAXIFRAGE COMPLEX
pws
ki,
y
~
FIGURE 3. Saxifraga nivalis complex in the Canadian Arctic. A. S. tenuis (Gillespie & Consaul 6978-2), habit. B. S. nivalis
(Gillespie and Consaul 6977-1), habit. C. Comparison of basal rosette of leaves of S. tenuis (on left, Gillespie &
Consaul 6978-2) and S. nivalis (on right, Gillespie and Consaul 6977-1). A and B are the same scale.
334
tributor to petal coloration. Plants growing in more
open, sunnier environments tend to have more pink
or dark red anthocyanin pigment throughout the plant,
including the petals. White petals may also sometimes
turn pinkish with age. In contrast, little variation was
observed within each taxon for the texture and color-
ation of stem hair, and these characters were signifi-
cantly different between taxa.
Among traits traditionally used for identification of
the S. nivalis complex, many displayed considerable
intrataxon variance, with ranges often overlapping be-
tween taxa. Our results also indicate a greater degree
of variability within S. nivalis than in S. tenuis in the
Canadian Arctic. This pattern of variation results in a
somewhat obscure morphological boundary between
the two species and has led to difficulties in construct-
ing good identification keys.
Characters and taxonomic identification
Despite the considerable intraspecific variation,
most commonly used identification characters were
significantly different between the two taxa. Indeed,
plants of S. nivalis were overall larger and more robust
than S. tenuis, and the latter often had a more reddish
tinge on the petals and stem hair, as previously found
by numerous authors (Simmons 1906; Polunin 1940;
Porsild 1957; Boécher et al. 1968; Léve 1983; Blon-
deau 1989a; Webb 1993).
Flowering stem width was an excellent identifica-
tion character apart from a few individuals, with S.
tenuis characterized by a width of 1 mm or less, con-
sistent with Webb’s (1993) use of it as a key character.
Consistently used by various botanists (e.g., Webb
1993), stem hair characters were among the most use-
ful for identification. Saxifraga nivalis usually has a
much more conspicuous, longer, denser, coarse crisped
white vestiture, while S. tenuis has a less conspicuous,
shorter, finer, usually glandular pubescence. Canadian
Arctic S. tenuis was found to always have stem hairs,
thus not conforming to descriptions of the taxon in
Greenland and Svalbard as having mostly glabrous
stems (Bécher et al. 1968, 1978; Ro@nning 1996).
Generally, S. nivalis plants were taller than S. tenuis,
but due to its variance, height was not useful for iden-
tification.
Saxifraga nivalis had more numerous teeth on the
leaves than S. tenuis, and the latter had rounder ob-
tuse teeth versus more pointed, as suggested in the
literature (e.g., B6cher et al. 1968), The width and
length of S. tenuis teeth were also found to be less
than those observed on S. nivalis, but, this is not sur-
prising considering that S. nivalis had on average
longer and wider leaves. Interestingly, S$. nivalis had
a notably less regular dentition than S. tenuis in regards
to the size of the teeth. The former generally had
small teeth at the base with teeth becoming larger
towards the apex, whereas S. tenuis had more evenly
sized teeth. Although size of the largest leaf differed
significantly between the two taxa, leaf size characters
THE CANADIAN FIELD-NATURALIST
Vol. 118
make poor diagnostic characters due to overlap and
age related variation. Also, leaf shape varied tremen-
dously and thus should not be considered a good
discriminating character. However, the leaf apices of
S. tenuis did tend to be more rounded than those of S.
nivalis.
Inflorescence compactness provides a useful identi-
fication character, with S. nivalis having one or more
compact head-like clusters and S. tenuis a more open
inflorescence (as described in Porsild 1957). Flower
pedicels, especially of the lowermost flowers, are longer
in S. tenuis than in S. nivalis. Since pedicels of the
latter may elongate somewhat in fruit, this difference
may be obscured later in the season. Although not con-
stant, petals tend to be whiter, wider and ovate in S.
nivalis and pink, narrower, more elongated and rounder
at the apex in S. tenuis. BOcher (1938), Bocher et al.
(1968), and more recently Love (1983) and Rgnning
(1996) state that S. nivalis has straight or slightly
spreading styles, while S. tenuis has styles that curve
strongly downwards. This was not always the case in
Canadian Arctic specimens we examined. The way
specimens were pressed and the time of collection
might be partly responsible for the variation in this
character within the two species.
Other characters showed variation that was not use-
ful in separating the two taxa. While S. nivalis usually
had hairs on leaf margins, this character was also
found to a lesser degree in S. tenuis. Most specimens
examined had a purplish or reddish stem, thus not
specific to S. tenuis. Also, the flowering stems of both
taxa had on occasion a reduced leaf (bract) or two near
the inflorescence, although usually more prominent
in S. tenuis.
The presence of rust-coloured hairs on the lower
surface of the leaves of S. tenuis has been commonly
used to distinguish it from S. nivalis in the Canadian
Arctic, and was used as a key character by several
authors (Porsild 1957; Scoggan 1978; Porsild and
Cody 1980). However, this study reveals that hairs
are present on the leaf undersurface in over 99% of the
plants examined of both species in the Canadian Arctic,
and that hairs may be rust-coloured in both species,
about 42% of S. nivalis plants examined and 74% of
S. tenuis plants. This error may have resulted from
Porsild’s inclusion of S. rufopilosa within his concept
of S. tenuis (distribution maps of S. tenuis in Porsild
(1957) and Porsild and Cody (1980) appear to have
included S. rufopilosa). Saxifraga rufopilosa, a species
now considered to be endemic to unglaciated areas of
the Yukon and Alaska, is characterized by a mat of long
crinkly rusty hairs on the leaf undersurface (Cody
1996), much longer and denser than in either S. tenuis
or S. nivalis. Whatever its origin, use of rust-coloured
hair presence as a key diagnostic character in identify-
ing Canadian Arctic material of the S. nivalis complex
resulted in many misidentified specimens and much
confusion as to the identity of S. tenuis.
2004. HEALY AND GILLESPIE: ALPINE SAXIFRAGE COMPLEX 335
Sy
e Specimen data (CAN, DAO)
‘\ == Adjacent species range from
S Porsild and Cody (1980)
we
e Specimen data (CAN, DAO)
-\se=, Adjacent species range from
OB Porsild and Cody (1980)
Ficure 4. Distribution of the Saxifraga nivalis complex in the Canadian Arctic. (above) S. nivalis. (below) S. tenuis.
Shading indicates approximate distribution outside of the Arctic Islands (from Porsild and Cody 1980, and CAN and
DAO herbarium records).
336
The many herbarium collections having both S.
nivalis and S. tenuis plants on the same sheet and under
the same number (e.g., Bruggeman 358, Savile 4562,
Macdonald 150, Calder et al. 24149) shows just how
problematic identification of this complex in the Cana-
dian Arctic has been. About 20% of herbarium speci-
mens identified as S. tenuis at both CAN and DAO
were in fact mixed collections including both S. tenuis
and S. nivalis plants, or less often including small plants
of S. foliolosa or S. hieracifolia Waldst. & Kit. Pre-
vious identification problems of the S. nivalis complex
in the Canadian Arctic may also have been due to
misinterpretation of key characters. For example, S.
nivalis with several flower heads could be keyed out
under lax (open) inflorescence.
Although S. nivalis and S. tenuis can be readily dis-
tinguished in the Canadian Arctic, a small percentage
of specimens had one or a few characteristics of the
other species. For example, some high arctic S. nivalis
had very slender stems or fruit with strongly recurved
styles. While this may be part of the natural variation
within S. nivalis, it may also suggest a low level of
hybridization. Some of the overlap in quantitative char-
acter states shown in our morphological analyses may
also be the result of hybridization. Recent cytological
studies have suggested the existence of S. nivalis-S.
tenuis hybrids (2n = 40) in regions of the Russian
Arctic and the Yukon where S. nivalis and S. tenuis are
found growing together (Krause and Beamish 1973;
Devyatov et al. 1997). The population in the Gaspé
Peninsula has the same intermediate chromosome num-
ber and may represent a stabilized relictual hybrid in
an area whether neither parent now occurs (Gervais et
al. 1995). In addition Polunin (1959) suggested that
hybridization may also occur between the S. nivalis
complex and other closely related species, such as S.
hieracifolia.
Geographical variation in Saxifraga tenuis
Savile (1961) proposed that North American S. tenuis
may be divided into three disjunct and morphologi-
cally distinct “populations.” The first is a high arctic
population composed of plants identical to material
from the north of Greenland and hypothesized to have
spread from there following the Pleistocene. The
second population is apparently found mostly along
Hudson Straight in southern Baffin Island, northern-
most Quebec and Southampton Island, but also
scattered northward to northeast Baffin Island. Savile
treated plants in the Gaspé Peninsula of Quebec, con-
sidered by some as a separate species S. gaspensis, as
part of this population. Plants of this population appar-
ently tend to be larger and less purplish in colour than
in the high arctic. The third highly variable population,
found in Alaska and the Yukon, is usually character-
ized by a highly purplish pigmentation and whitish
scape hairs, and was suggested to be intermediate
between S. nivalis and high arctic S. tenuis.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Our analysis indicates that eastern and high arctic
plants of S. tenuis cannot be distinguished based on
examined quantitative characters, while western mon-
tane plants (based on our small sample size) may be
differentiated from most arctic plants based on larger
size. Since Savile (1961) used mostly qualitative char-
acters to distinguish the three groups, further analyses
based on both qualitative and quantitative characters
and including more western montane and eastern arctic
specimens should be made to further test his hypoth-
esis.
Chloroplast DNA analysis
The five non-coding cpDNA regions of S. nivalis
and S. tenuis were identical for restriction sites as-
sayed. Considering the conservative nature of cpDNA
evolution, it is not surprising to observe such similar-
ity, with closely related species often having identical
cpDNA restriction site profiles (Olmstead and Palmer
1994). However, S. nivalis and S. tenuis displayed an
estimated 50 bp length difference in the trnT-trnF
region. This difference was observed both among plants
from the same site and from different locations. This
suggests that the size variation in the t7T-trnF region
is not background variation among populations or a
phenomenon limited to a particular population, but
represents a molecular difference between S. nivalis
and S. tenuis, either a deletion event in S. nivalis or
an insertion event in S. tenuis. Sequencing of the
tnT-trnF region would prove useful in specifying the
nature of this size difference. The RFLP analysis re-
vealed molecular differences for 16 of 105 restriction
enzyme assays between S. foliolosa and the other two
species. These results are similar to a study of Saxifraga
based on the cpDNA matK sequences (Soltis et al.
1996; plus sequences in Genbank), in which S. nivalis
and S. tenuis would appear to be more closely related
to each other than to S. foliolosa. Based on comparison
of the Genbank sequences, the single plant of S. fenuis
differed from S. nivalis in four nucleotide substitu-
tions, and from S. foliolosa in 79 substitutions.
Implications
Our results suggest that S. nivalis and S. tenuis
should be recognized as distinct taxa, and are most
appropriately recognized at the species level following
Porsild (1957), Porsild and Cody (1980), and Webb
(1993). The two taxa are distinguishable at both the
molecular and cytological level and have morpho-
logical differences that correspond to these differences.
Although no morphological characters give 100% sep-
aration, many quantitative and qualitative characters
show statistically significant differences between the
two taxa. The two taxa overlap in geographic distribu-
tion in the Canadian Arctic, with the range of the less
common S. tenuis included within that of S. nivalis.
Although ranges of habitat preferences differ, there is
considerable overlap, with the two taxa sometimes oc-
curring in mixed populations. Lack of geographical
2004
separation and considerable habitat overlap make
recognition at the subspecific level inappropriate, while
the morphological distinctiveness of the two taxa would
make recognition at the varietal level inappropriate.
Saxifraga nivalis complex in the Canadian Arctic:
key to species
A. Inflorescence one to several dense head-like clusters
of numerous flowers; petals white or essentially so
(sometimes becoming pink with age); flowering stem
(0.5-) 1-2.5 mm wide, moderately to densely hairy,
with conspicuous long coarse white hairs; plant usu-
ally robust in appearance S. nivalis
B. Inflorescence an open cyme of fewer flowers, flowers
on distinct pedicels; petals pink or less often white;
flowering stem 0.3-1 mm wide, usually sparsely hairy,
with short fine hairs that are usually inconspicuous;
plant delicate in appearance S. tenuis
Saxifraga nivalis L.
Plants perennial herbs, (2) 5—17 cm high, with a basal ros-
ette of leaves. Leaves simple, alternate, all basal in a rosette,
evergreen; petiole usually distinct, 0.2-2.5 mm long. Leaf
blade ovate, obovate, orbicular or spatulate, 6-36 mm long
(mean 14 mm), 4-21 mm wide (mean 10 mm), slightly leath-
ery; green above, green or reddish-purple beneath, base obtuse
and usually abruptly narrowed at petiole; apex obtuse, rounded
or rarely acute; appearing single-veined or with inconspic-
uous lateral veins; upper surface glabrous; lower surface
sparsely to densely hairy; hairs 0.2-1.2 mm long, rust-coloured,
whitish or translucent; margins coarsely serrate or crenate,
usually with rust-coloured or whitish hairs; teeth 7-14, usually
increasing in size towards blade apex, tips usually pointed.
Flowering stem erect, (0.5) 1-2.5 mm wide, green to purple,
moderately to densely hairy, with hairs conspicuous, (0.5)
0.7-1.2 mm long, crisped (crinkly and irregularly wavy), white
or translucent with tips and crosswalls white or sometimes
rust-coloured or purplish, the tips sometimes glandular, usually
leafless or occasionally with reduced leaves (bracts) close to
the inflorescence. Inflorescence a dense head-like cluster of
numerous flowers, sometimes with 1-2 smaller lateral clusters
on short to long peduncles; flowers on very short pedicels,
subtended by bracts. Flowers: sepals 5, free, green or purple,
glabrous; petals 5, ovate or elliptic, 0.7-1.8 mm wide, equal
to or longer than the sepals, white or cream-coloured, some-
times with reddish apex, mostly obtuse at apex; stamens 10;
gynoecium partly inferior; carpels 2, partly fused; styles 2,
free; placentation axile; ovules numerous. Fruit a capsule,
spherical in lower half, with straight or slightly divergent
free carpels above, 34 mm long, 4.5—5.5 mm wide, glabrous,
dry, dehiscent; styles straight or slightly divergent, persistent;
sepals persistent in fruit. Seeds numerous, 0.5—1 mm long,
yellowish brown, with surface verrucose. Figure 3b, c; map
4a.
Saxifraga tenuis (Wahlenb.) Harry Sm.
Plants perennial herbs, 2-9 cm high, with a basal rosette
of leaves. Leaves simple, alternate, all basal in a rosette, ever-
green; petiole usually indistinct, ~0.5—2.5 mm long. Leaf blade
narrowly ovate, obovate or spatulate, 4-15 mm long (mean
7 mm), 2-8 mm wide (mean 5 mm); slightly leathery, green
to reddish-purple above, reddish-purple beneath; base obtuse
or broadly attenuate and decurrent onto petiole; apex obtuse,
rounded or rarely acute; appearing single-veined or with
inconspicuous lateral veins; upper surface glabrous; lower
HEALY AND GILLESPIE: ALPINE SAXIFRAGE COMPLEX
337
surface usually sparsely hairy, with hairs 0.1-0.4 mm long,
rust-coloured, whitish or translucent; margins coarsely serrate
or crenate, with sparse rust-coloured or whitish hairs or some-
times glabrous; teeth 6-9, usually evenly sized, tips usually
rounded. Flowering stem erect, 0.3-1 mm wide, usually dark
purple, sparsely hairy, with hairs mostly inconspicuous, 0.1-
0.3 (0.5) mm long, fine, crinkled or straight, rust-coloured
to translucent, often with purplish crosswalls and tips, the
tips usually glandular; sometimes with a reduced leaf (bract)
on the upper part of the stem. Inflorescence an open head of
few flowers; flowers subtended by bracts; lower-most flowers
often long-pedicellate and each subtended by a conspicuous
bract. Flowers: sepals 5, free, green or purple, glabrous; petals
5, ovate or elliptic, 0.5-1.1 mm wide, equal to or longer than
the sepals, usually pink, sometimes white, often with reddish
apex, often rounded at apex; stamens 10; gynoecium partly
inferior; carpels 2, partly fused; styles 2, free; placentation
axile; ovules numerous. Fruit a capsule, spherical in lower half,
with diverging free carpels above, 3-4 mm long, 4.5—5.5 mm
wide, glabrous, dry, dehiscent; styles usually strongly re-curved
at maturity, persistent; sepals persistent in fruit. Seeds num-
erous, 0.5—1 mm long, yellowish brown, with surface verru-
cose. Figure 3a, c; map 4b.
Acknowledgments
We thank Kristina Makkay for assistance with the
Statistical analysis and figures; Laurie Consaul for sug-
gestions in statistical analysis and assistance with map-
ping; Michelle Leblanc for assistance with mapping:
Susan Aiken for interesting discussions; Gisele Mitrow
and William J. Cody for assistance at the DAO herb-
arium. Also, a special thank-you to Marcel Blondeau
from the Université Laval for sharing his knowledge
and insights on the Saxifraga nivalis complex. We
acknowledge and thank Polar Continental Shelf Project,
Nunavut Research Institute and Aurora Research
Institute for their logistic support in the field. This
paper is based on a fourth year honours thesis project
by C. H. submitted to the Biology Department, Uni-
versity of Ottawa.
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Accepted 7 December 2004
Appendix 1: Collections examined of the Saxifraga nivalis complex from the Canadian Arctic.
Saxifraga nivalis
NUNAVUT. Axel Heiberg Island: 79°28'N 87°40'W, Beschel 10979 (CAN); Bukken River, 80°31.57'N 92°21.83'W,
Gillespie et al. 6613 (CAN); Crusoe Glacier, 97°27'N 91°12'W, Kuc 476-3 (CAN); Crusoe River, 79°24'N 90°S0'W, Kuc
s.n. (CAN 331187); Diana Lake, 79°30°N 88°30’ W, Porsild 16699-2 (CAN); Expedition Fjord, 79°20'N 92°W, Kuc s.n.
(CAN 331189, CAN 331189); Mesa Brook, 79°37'N 95°W, Beschel 13129 (CAN); Mokka Fiord, 79°45'N 87°W, Parker
73061E (CAN). Baffin Island: 63°24'N 64°35'W, McLaren 91 (CAN); 66°40'N 70°W, Soper s.n. (CAN 65150); Admiralty
Inlet, 73°13'N 84°W, Malte 118993 (CAN); Apex, 63°43'N 68°27'W, Gillespie & Soreng 6785 (CAN); Beekman Peninsula,
63°24'N 64°35'W, McLaren 9] (CAN); Burwash Bay, 65°59'N 71°18'W, Jacobs & Maus s.n. (CAN 517697); Frobisher
Bay, 63°45'N 68°31'W, Gillett 19018 (CAN); Dorset Island, 64°12'N 76°32'W, Hainaud & Norman 5698 (CAN); Foxe
Peninsula, 66°23'N 83°13'W, Manning 265 (CAN); Foxe Peninsula, 69°52'N 76°54'W, Manning 231 (CAN); Frobisher Bay,
62°57'N 66°03'W, Aiken et al. 86-260 (CAN); Frobisher Bay, 63°44'N 68°27'W, Aiken et al. 86-493 (CAN); Frobisher Bay,
62°57'N 66°03'W, Calder et al. s.n. (DAO 24148); Frobisher Bay, 62°57'N 66°03'W, Wynne-Edwards 7353 (CAN); Pond
Inlet, 72°50'N 76°40'W, Dutilly 1224a (CAN); Stising Valley, Weber 94 (CAN); Taverner Bay, 67°12'N 72°25'W, Manning
44, 68, 77 (CAN). Bathurst Island: Polar Bear Pass, 75°43'N 98°23'W, Aiken & Maus 92-022 (CAN); Goodsir Inlet,
75°45'N 97°45'W, Lamothe 69-25 (CAN); Polar Bear Pass, 75°43.8'N 98°25.45'W, Gillespie & Consaul 6984 (CAN) [DNA
voucher, individuals 1-5 examined]. Bylot Island: 72°53'N 76°W, Wilcox 125631 (CAN). Cameron Island: 76°19.5'N
104.5°W, Aiken 92-039 (CAN). Cornwallis Island: Resolute, 74°40'N 94°50'W, Aiken & MacCormac 98-055 (CAN
581909, plants 1-5; CAN 582554); Resolute, 74°40'N 95°04'W, Aiken et al. 93-072 (CAN). Devon Island: Dundas
Harbour, 74°31.3'N 82°33.5'W, Gillespie et al. 6675-1 (CAN); Truelove Lowland, 75°40'N 84°40'W Kerik s.n. (CAN
409363). Digges Island: 62°32'N 77°45'W, Gaston 25, 29 (CAN); 62°35'N 77°50'W, Gaston 17 (CAN). Ellef Ringnes
Island: Isachsen, 78°47'N 103°50'W, Macdonald 242 (CAN). Ellesmere Island: 79°34'N 84°44'W, Edlund & Roncato-
Spencer 264 (CAN); Alexandra Fiord, 78°53'N 75°45'W, Gillespie & Vogel 6165 (CAN); Alexandra Fiord, 78°53'N
75°50'W, Gillett & Shchepanek 18108 (CAN); Craig Harbour, 76°20'N 81°30'W, Dutilly 1267 (CAN): Hazen, 68°30'N
72°45'W, Soper 8194 (CAN); Hazen, 81°49'N 71°20'W, Gillespie & Vogel 6238 (CAN); Sawtooth Range, 79°43.54'N
83°09.44'W, Gillespie et al. 6643 (CAN); Slidre Fjord, 80°N 86°15'W, Tener 95 (CAN): Tanquary, 78°53'N 75°45'W,
Gillespie & Vogel 5982 (CAN). King William Island: Gjoa Haven, Cooper 28 (CAN), 73 (CAN), 226 (CAN); Gjoa
Haven, 68°38'N 95°53'W, Larson 25 (CAN); Victory Point, Cooper 164 (CAN), 122 (CAN). Lougheed Island: 77°30'N
105°38'W, Edlund 2091 (CAN). Meighen Island: 79°55'N 99°30'W, Kuc (CAN 331171). Pelly Bay: 68°53'N 89°51'W,
Campbell s.n. (CAN 282778). Prince Charles Island: 67°10'N 76°43'W, Baldwin 1919 (CAN). Victoria Island: 68°53'N
105°W, Edlund & Argus 12730-1 (CAN).
NORTHWEST TERRITORIES. Banks Island: 73°N 117°W, Aiken 99-203 (CAN); 73°24'N 117°0'W, Porsild 17711
(CAN); 74°31'N 121°07'W, Manning & Macpherson 164 (CAN); Bernard River, 73°22'N 121°47'W, Maher & Maclean 75
(CAN); Egg River, 72°27'N 124°36'W, Lambert s.n. (CAN 535943); Lambton, 71°05'N 123°09'W, Porsild 17579 (CAN);
Shoran Lake, 71°51'N 113°23'W, MaclInnes s.n. (CAN 535570, 535598, 535733). Fitzwilliam Owen Island: 77°07'N
113°47'W, Kuc s.n. (CAN 331114). Melville Island: 75°56'N 114°48'W, Edlund & Aiken 148 (CAN); Canrobert Hills
75°47.30'N 115°56'W, Edlund 179 (CAN); Ibbett Bay, 75°54'N 114°30'W, Edlund 43 (CAN); Kitson River, 76°02'N
113°05'W, Edlund 18 (CAN); Marie Bay 76°12'N 114°55'W, Edlund 305 (CAN); McCormick Inlet, 75°46.2'N
112°31.64'W, Gillespie & Consaul 6977 (CAN, plants 1, 2), 6964a (CAN); Shellabear Point, 71°51'N 113°23'W, Edlund
115 (CAN); Sherard Bay, 76°08'N 108°07'W, Dugal s.n. (CAN 535598); Winter Harbour, 74°17'N 110°42'W, Kuc s.n.
(CAN 400104); Winter Harbour, 74°17'N 110°42'W, Tener & Harington 149 (CAN). Prince Patrick Island: Green Bay.
76°33.67'N 118°53.09'W, Gillespie & Consaul 6869 (CAN, plants 1-6); Intrepid Inlet, 76°22.01'N 118°35.45'W, Gillespie
340 THE CANADIAN FIELD-NATURALIST Vol. 118
& Consaul 6876 (CAN); Mould Bay 76°12N 119°25'W, MacDonald 146 (CAN); Mould Bay, 76°14.50'N 119°21'W,
Gillespie & Consaul 6806 (CAN, plants 1-5); Mould Bay, 76°14'N 118°57'W, Gillespie & Consaul 6827 (CAN, plants 1,
2), 6826 (CAN, plants al-a5); Mould Bay, 76°21.50'N 119°30.50'W, Gillespie & Consaul 6884 (CAN, plants 1, 2), 6984
(CAN, plants 1-5), 6806 (CAN, plants 1-5). Victoria Island: Minto, 71°34'N 115°21'W, Edlund 594 (CAN).
Saxifraga tenuis
NUNAVUT. Axel Heiberg Island: Bastion Ridge, 79°21'N 90°48'W, Beschel 12920 (CAN); Mesa Brook, 79°35'N
95°30'W, Beschel 13129 (CAN 295548): 80°17'N 88°27'W, Scotter & Zoltai 45133 (DAO), 4518/1 (DAO). Baffin Island:
Resolution Island, 61°20'N 64°55'W, Wynne-Edwards 7225 (CAN); Erik Harbour, 72°40'N 76°30'W, Calder s.n. (DAO
30869, 30871); Ogac Lake, 62°51.7'N 67°21'W, McLaren s.n. (CAN 274125); Frobisher Bay, 63°45'N, 68°32'W, Senn 3658
(DAO); Blackhead Island, 64°59'N 66°19'W, Soper s.n. (CAN 125598); Savage Islands, 61°49.15'N 65°42.62'W, Gillespie
et al. 6728 (CAN), 6732 (CAN); Inugsuin Fjord, 69°50'N 69°08'W, Beschel 3649A (CAN). Bathurst Island: 76°36'N
100°04'W, Blake 24a (DAO). Bylot Island: 73.03'N 80.07'W, Scotter & Zoltai 6751A (DAO). Ellef Ringnes Island:
Isachsen, 78°49'N 103°37'W, Savile 4275 (DAO), 4219 (DAO), 4224 (DAO), 4285 (DAO), 4355 (DAO), 4293 (DAO);
Isachsen, 78°47'N 103°30'W, MacDonald 251 (CAN), 252 (CAN); Christopher Peninsula, 78°59'N 101°35'W, Savile 4194
(DAO); 78°45'N 102°50'W, Savile 4148 (DAO). Ellesmere Island: Eureka, 79°59'N 85°50'W, Scotter & Zoltai 45294-B
(DAO); Eureka, 80°10'N, 85°39'W, Bruggemann S05 (DAO); Fosheim Peninsula, 79°34'N 84°44'W, Edlund & Roncato-
Spencer 262 (CAN 535348, 533280); Fosheim Peninsula, 79°58'N 84°26'W, Edlund & Roncato-Spencer 275 (CAN);
Hazen, 81°49'N 71°21'W, Savile 4485 (DAO), 4752 (DAO), 4655 (DAO); Hazen, 81°45'N 68°30'W, Powell 338 (CAN);
Hazen, 82°N 70°W, Soper 8273 (CAN); Makinsen Inlet, 76°41'N 81°37'W, Blake 7 (DAO); Mount Pullen, 82°25'N
62°17'W, MacDonald 46 (CAN); 81°45'N 62°11'W, Powell 520 (CAN); Mt. Pullen, 82°26'N 62°11'W, Bruggemann 215
(DAO); Tanquary Fjord, 79°12'N 83°29'W, Brassard 3306 (CAN); Van Hauen Pass, 81°07'N 86°55'W, Brassard 3047
(CAN); Vesle Fjord, 79°12'N 83°29'W, Edlund & Roncato-Spencer 282 (CAN). Somerset Island: 72°56'N 94°57'W, Zoltai
741044 (DAO).
NORTHWEST TERRITORIES. Melville Island: 74°58'N 115°02'W, Parker 44f (DAO); Bailey Point, 74°58'N,115°02'W,
Parker 48b (DAO); McCormick Inlet, 75°46.2'N 112°31.64'W, Gillespie & Consaul 6978 (CAN, plants 1, 2), 6964b
(CAN). Prince Patrick Island: Green Bay, 76°33.67'N 118°53.09'W, Gillespie & Consaul 6870 (CAN, plant 1); Intrepid
Inlet, 75°46.9'N 112°22.09'W, Gillespie & Consaul 6877 (CAN, plant 1); Mould Bay, 76°21.5'N 119°30.5'W, Gillespie &
Consaul 6881 (CAN, plants 1-6); Mould Bay, 76°14'N 118°57'W, Gillespie & Consaul 6825 (CAN, plants 1-3); Mould
Bay, 76°14.5'N 119°21'W, Gillespie & Consaul 6807 (CAN, plants 1-5). Victoria Island: Ulusartok Peninsula, 70°44'N
117°44'W, Edlund 875 (CAN).
ALASKA. Kenai Peninsula. 60°49'N 149°33'W, Calder 6511, 6249, 6107 (DAO).
BRITISH COLUMBIA. Haines Junction, Calder & Kukkonen 28151 (DAO); Haines, Taylor et al. 1204 (DAO).
Mixed collections - Saxifraga tenuis and Saxifraga nivalis on same sheet
NUNAVUT. Baffin Island: Apex, 63°43'N 68°27'W, Calder et al. s.n. (DAO 24149); Home Bay, 68°45'N 67°10'W, Smith
VP-53-61 (CAN). Ellesmere Island: Tanquary Fjord, 79°12'N 83°29'W, Brassard 3317 (CAN); Hazen, 81°49'N 71°21'W,
Savile 4562 (DAO).
NORTHWEST TERRITORIES. Victoria Island: near Holman, 70°43'N 117°43'W, Edlund 719 (CAN). Prince Patrick
Island: Mould Bay, 76°12'N 119°25'W, MacDonald 150 (CAN, S. tenuis: 1, 3, 4, 7, 8, 9; S. nivalis: 2, 5, 6, 10).
_ The Influence of Prey Availability and Vegetation Characteristics on
| Scent Station Visitation Rates of Coyotes, Canis latrans, in a
Heterogeneous Environment
LynpDA A. RANDA! and JOHN A. YUNGER2
Department of Biological Sciences, Northern [Illinois University, DeKalb, Illinois 60115 USA
'Present address: Natural and Applied Sciences Division, College of DuPage, 425 Fawell Boulevard, Glen Ellyn, Illinois
60137 USA
Present address: Environmental Biology Program, Governors State University, University Park, Illinois 60466 USA
Randa, Lynda A., and John A. Yunger. 2004. The influence of prey availability and vegetation characteristics on scent station
visitation rates of Coyotes, Canis latrans, in a heterogeneous environment. Canadian Field-Naturalist 118(3): 341-353.
We investigated the effects of local prey fluctuations and habitat variables on the scent station visitation rates of the Coyote
(Canis latrans) in northern Illinois within a heterogeneous environment. Availability of small mammalian prey was assessed
by monthly mark-recapture sampling and visual counts conducted along three, 192-m transects in each of seven habitats that
ranged from grassland to wooded sites. Habitat metrics, which included foliage density, ground cover, and canopy cover,
were also collected for the same seven habitats. Visitation rates of Coyotes were determined from scent station lines parallel
to the small mammal trapping transects. A multiple regression analysis indicated that Coyote visitation rates across the study
site were influenced positively by vole (Microtus spp.) abundance and negatively by canopy cover. When Coyote visitation
rates were regressed on vole abundance for only the habitats in which voles occurred, the relationship was not significant.
This may be attributed to the general avoidance of wooded areas by Coyotes. Coyotes did, however, respond to experimentally-
induced abundant patches of Peromyscus. These findings suggest Coyotes selectively use grassland habitats within a hetero-
geneous environment and may modify their use according to prey availability.
Key Words: Coyote, Canis latrans, habitat use, heterogeneous environment, prey availability, scent station, Illinois.
The Coyote, Canis latrans, is among the most adapt-
able of North American predators. Across an expan-
sive range, the species occupies a variety of habitats
and consumes a diversity of foods (Bekoff 1978). As
such, the Coyote has been the focus of various local
and regional studies of distribution, activity patterns,
and diet selection. In particular, spatial and temporal
activity patterns have been explicitly described (e.g.,
Andelt and Gipson 1979; Holzman et al. 1992), yet
there has often been only circumstantial evidence as
to causal factors (e.g., Person and Hirth 1991). Under-
standing potential determinants of Coyote spatial dis-
tribution and activity patterns requires an understanding
of factors such as diet composition and specific use of
available habitat types.
Predators exhibiting flexible behavior patterns, such
as Coyotes, provide an opportunity for studying possi-
ble rapid responses to prey availability. Previous studies
have shown that diets (Andelt et al. 1987: Brillhart
and Kaufman 1995; Todd et al. 1981) and temporal
activities of Coyotes (Shivik and Crabtree 1995) can
vary seasonally based upon prey availability. Because
space use and movements of vertebrate predators are
closely coupled to foraging behavior, Coyotes could
also alter their spatial use patterns in response to chang-
es in prey availability. However, vertebrate predators
frequently move over large spatial scales, whereas their
smaller prey tend to be restricted to specific habitats
or patches within a habitat. The study of prey in only
one or a limited number of locations used by the pred-
ators (Hamlin et al. 1984; Jaksic et al. 1993; Korsch-
gen and Stuart 1972) may preclude accurate inferences
on the foraging behavior of vertebrate predators. Thus,
it is important to relate predator foraging behavior
among habitats to prey abundances within habitats of
heterogeneous landscapes (Dunk and Cooper 1994;
Korpimaki 1994).
In addition to prey, variations in vegetation structure,
such as foliage density and height, among different
habitats can also influence the movements and activities
of vertebrate predators (Clark et al. 1993; Lamberson
et al. 1994), especially in fragmented landscapes.
Habitat differences may constrain predator foraging
in certain areas through predators selectively using or
avoiding particular habitat types (DeJong 1995; Small-
wood 1995). As a result, predators may not respond
to changes in prey availability within certain habitats.
However, vegetation measures used to quantify pred-
ator habitat use may also be related to or reflect prey
usage (Anthony et al. 1981). Such inter-relatedness
must be considered when making inferences of pred-
ator behavior.
We investigated the relationships of spatial and tem-
poral distribution of prey and vegetation characteristics
to the habitat visitation of Coyotes across a hetero-
geneous environment. We incorporated experimental
manipulations of habitat and prey, along with natural
perturbations, to elicit predator behavioral responses
341
342
within a relatively short time scale. Data collected on
prey abundance and habitat variables were used to ad-
dress whether scent station visitation rates of Coyotes
vary among habitats and within a particular habitat in
response to changes in prey availability.
Study Areas
The study site was located in northern Illinois at
Fermi National Accelerator Laboratory (Fermilab) in
Batavia, Illinois (41°50'N, 88°15'W). Fermilab encom-
passes approximately 3200 ha and is characterized as
a heterogeneous area, marked by distinct habitat bound-
aries. The areas surrounding Fermilab consisted of
small open spaces of mainly agricultural land inter-
spersed with light industry and residential neighbor-
hoods, providing potential predator access into or out
of the study site. The study was conducted at seven
different locations within Fermilab, representing five
habitat types: (1) oldfield, dominated by Queen Anne’s
Lace (Daucus carota) and Tall Goldenrod, (2) tallgrass
prairie, dominated by Big Bluestem (Andropogon ger-
ardii) and Indian Grass (Sorgastrum nutans); (3) brome
grass field, dominated by Smooth Brome (Bromus
inermis); (4) shrubby oldfield, a heterogeneous mix of
dense shrubs and shrub-grassland mixture dominated
by Tall Goldenrod (Solidago altissima) and Gray Dog-
wood (Cornus racemosa) with small stands of Trem-
bling Aspen (Populus tremuloides); and (5) oak wood-
land, dominated by mature oaks (Quercus spp.), one
woodland (Oak Woods I) characterized by less dense
canopy (primarily Q. macrocarpa and Q. rubra) than
the other (Oak Woods II; predominantly Q. alba and
Q. rubra; Figure 1). These different habitats were cho-
sen because they represented the heterogeneity of the
study site and included all prey species potentially
found in Coyote diets at Fermilab. A concurrent inves-
tigation indicated that three prey, voles (primarily
Meadow Voles, Microtus pennsylvanicus, and rarely
Prairie Voles, M. ochrogaster), Eastern Cottontails
(Sylvilagus floridanus), and mice (Peromyscus spp.),
constituted 39.4%, 31.3%, and 8.4% of the Coyote
diets, respectively, which was at least two times great-
er than the proportion of any other prey item (Randa
1996).
Methods
Availability of prey
From March 1994 through May 1995, small mam-
mal species compositions and abundances were esti-
mated by mark-recapture live-trapping on three, 192 m
transects located within each of the seven habitats
(Figure 1). The transects were parallel and spaced from
70 to 85 m to help maximize their independence in
relation to small mammal movements. At least 50 m
was maintained from each transect to habitat bound-
aries to avoid edge effects. Seventeen trap stations were
spaced at 12-m intervals along each transect, totaling
51 trap stations per habitat. One 23 x 9 x 7.5 cm
THE CANADIAN FIELD-NATURALIST
Vol. 118
Sherman live-trap, baited with a peanut butter and
oats mixture, was placed at each station. All habitats
were trapped for two nights on a monthly basis. Traps
were checked early morning and late afternoon (ca.
every 12 hr). Captured individuals were marked with
a uniquely numbered eartag (Monel Number 1, Na-
tional Band and Tag Co., Newport, Kentucky).
Nocturnal visual counts, using a high-powered spot-
light (Woolf et al. 1993), were conducted for Eastern
Cottontails in each of the seven habitats. The counts
were conducted twice during each of the 15 small
mammal trap sessions by sighting with binoculars, at
one end and midway, along the small mammal trap-
ping transects. Animals within ca. 25 m of the tran-
sect were counted. For the visual counts, the trapping
transects were lengthened to 250 m, delineated by flag-
ging at opposing ends, to allow for the larger spatial
movements of rabbits. Care was taken not to double
count animals potentially moving between transects.
For the experimental studies, fire was used as a
means of manipulating prey. Tallgrass Prairie I was
burned between the October and November 1994
small mammal surveys, a period of time when small
mammal abundances peak in northern Illinois (Yunger
2002). This site was adjacent to Oak Woods I (Figure
1), which concurrently experienced a high acorn
production year. Both habitats contained two closely
related species of small mammals (Peromyscus mani-
culatus, the Deer Mouse, in the prairie and P. leu-
copus, the White-footed Mouse, in the woods), which
were similar in body size and morphology. Numerical
responses, caused by immigration of Deer Mice to
prairie burns, have been documented previously (Cook
1959; Kaufman et al. 1983, 1988). Similarly, acorns
have been shown to be an important local food source
for mice (Peromyscus spp: Ostfeld et al. 1996; Wolff
1996). Consequently, we predicted a localized increase
of P. maniculatus in Tallgrass Prairie I and P. leucopus
in Oakwoods I. The proximity of these two habitats
provided the opportunity to compare changes in Coy-
ote habitat visitation following the manipulations of
prey abundance.
Prey also was manipulated in Tallgrass Prairie II
through food supplementation. From October 1994
through March 1995, 10 kg of commercial rodent chow
was hand broadcasted at weekly intervals on two of
four (i.e., two treatment and two control), 0.60-ha
square plots. As part of a separate study on the popu-
lation dynamics of small mammals (Yunger 2002),
prey numbers were determined by monthly trapping
on a 6 X 6 grid with 12-m spacing in each plot.
Predator spatial and temporal visitation responses to
resulting changes in prey due to the food supplemen-
tation experiment were also compared to the natural
increase in acorns of Oak Woods I and to the prey
response to experimental burning of Tallgrass Prairie I.
Visitation rates of Coyotes
2004 RANDA and YUNGER: SCENT STATION VISITATION RATES OF COYOTES
es me mee
n e le
hu
|
=
A
(
(|) Ibo!
oO
a
senses
“amas om sow 6 ame a
: 1 | ear
Bee oo
Bea Pha 1 Oldfield
Wea 2 Tallgrass Prairie I
mane 3 Oak Woods I
4 Shrubby Oldfield
5 Oak Woods II
6 Brome Grass Field
10) 500 m Ace
N ——— ee ransect 7 Tallgrass Prairie II
FIGURE 1. Map of Fermilab showing the seven different study locations (habitats) and approximate locations of scent station
transects in each habitat. Dashed line represents boundary of Fermilab. Roads, buildings, and open water (dark
shaded areas) are included to further depict heterogeneity of the study site.
344
Coyote visitation rates were monitored through the
use of scent stations. These were constructed by exca-
vating a 50-cm diameter by 10-cm deep circular depres-
sion, rimmed up to the ground surface with a 10-cm
wide strip of aluminum flashing to inhibit invasive
growth from surrounding vegetation, and filled with
fine-grained sand. The resulting stations were level
with the ground surface and fairly inconspicuous
except for the lack of vegetation. Scent stations were
located along 175-m transects, parallel to the small
mammal trapping transects, in each of the seven loca-
tions. Transects were spaced ca. 100 m apart while
maintaining at least 50 m from a transect to the habi-
tat edge. Eight scent stations were spaced every 25 m
along each transect in the seven habitats, for a total
of 24 scent stations per location. At the start of each
monitoring period, all scent stations were baited by
placing a cotton swab dipped in a liquid commercial
predator lure (Cronk’s Predator 500, Wisscasset, Maine)
upright in the middle of the scent station and the sand
was smoothed. Stations were simultaneously monitored
for a minimum of 2 nights (without precipitation), |
to 3 times monthly (mean of 2.1 times per month);
sand was not smoothed or otherwise disturbed by the
authors during each monitoring period. Monthly scent
station use was calculated for each habitat based upon
visitation rates, or the proportion of scent stations
exhibiting Coyote tracks in a given habitat, and divid-
ed by the total number of operative nights to account
for any variation in sampling duration.
Within-habitat Coyote visitation rates were evaluated
through the small mammal food supplementation
experiment conducted in Tallgrass Prairie II. In Jan-
uary 1995, one scent station was placed at each corner
of the four plots previously described for this habitat.
These 16 stations were monitored from February 1995
through May 1995 to compare scent station visitation
rates of Coyotes to prey numbers in supplemented
and non-supplemented plots.
Vegetation analysis
Vertical foliage density, percent ground cover, and
canopy cover were used to describe habitat structure
for each of the seven habitats. Vegetation measurements
were collected at 24 stations per habitat, along alter-
nating stations of the small mammal trapping transects.
Foliage density was measured using a modified profile
board technique (MacArthur and MacArthur 1961).
Percent cover of three, 30 x 50-cm profile boards,
divided into 15, 10 x 10-cm cells, was measured at
0.5 m, 1.0 m and 1.5 m from ground to mid-level of
the board. A cell was considered covered if 50% or
more of the cell, viewed from a 5-m distance, was ob-
structed by vegetation. The proportion of cells covered
determined percent cover of an individual board. All
readings were taken facing north and there was no
apparent patterning or trending in vegetation struc-
ture and diversity among each of the four cardinal
directions. To arrive at a single foliage density value
THE CANADIAN FIELD-NATURALIST
Vol. 118
for each habitat, the proportion of vegetation cover
was averaged across the three vertical profile boards
for each sampling station, then the mean of the result-
ing 24 values was calculated.
Percent ground cover was assessed at each sam-
pling station by the amount of vegetation (herbaceous,
woody, and leaf litter) occupying a 1-m? quadrat against
visible patches of ground (Brower et al. 1990). Canopy
cover was estimated by the presence or absence (scored
as | or 0, respectively) of vegetation viewed through
a vertical ocular tube (James and Shugart 1970) at
each sampling station. Average ground cover and
canopy cover for each habitat was obtained by taking
the mean of the 24 values of each metric.
The vegetation analysis was conducted once in
March 1994 and once in August 1994, representing
vegetation structure characteristic of the non-growing
and growing seasons, respectively. Two months of the
year, May and November, represent transitions between
the growing and non-growing seasons and hence, char-
acteristic vegetation density. For this study, vegetation
variables for May were described by the August sur-
vey (i.e., high foliage density), and vegetation variables
for November were described by the March survey
(i.e., low foliage density).
Data analysis
Analyses of small mammal prey were based upon
minimum number known alive (MNKA). This esti-
mate was generated for each individual transect per
month using Package C. M. R. (Le Boulengé 1987).
The estimates then were averaged for the three tran-
sects to yield monthly small mammal species compo-
sition and abundance for each habitat.
To examine whether Coyotes shifted visitation rates
in response to prey, it was necessary to determine
whether spatial and temporal differences in prey abun-
dances existed. Analysis of covariance (ANCOVA),
conducted with SAS PROC GLM (SAS Institute Inc.
1990), was used to compare abundances of the most
important prey species identified in Fermilab Coyote
diets (Randa 1996). Specifically, analyses were con-
ducted to test for significant fluctuations in prey abun-
dances over time among each of the seven habitats.
ANCOVA can be used to test for an interaction or
heterogeneity of slopes (Littell et al. 1991) and was
chosen because sampling units (i.e., habitats) were
not replicated in space. Temporal changes of prey popu-
lations were indicated by crossing the categorical vari-
able (1.e., prey abundances across habitats or prey abun-
dances per habitat) with the continuous covariate (time).
Traditional model building techniques were used
(Box et al. 1978) in which non-significant, higher-
order interactions were removed from the model. If
no significant sources of variation were detected, the
full model was reported. If significant interaction of
variables occurred (i.e., heterogeneity of slopes), sig-
nificance of main effects were inferred from the plot-
ted data. Statistical inferences were based on type III
2004
sum-of-squares and significance accepted at a = 0.05.
Multiple regression (SAS PROC REG; SAS Insti-
tute Inc. 1990) was used to evaluate the effect prey
availability and vegetation structure had on Coyote
visitation rates. Six independent variables were used
in the model: the abundances of the three main prey
genera, (1) Microtus, (2) Peromyscus, and (3) Sylvi-
lagus, and the three vegetation variables, (4) vertical
foliage density, (5) percent ground cover, and (6) can-
opy cover. Each observation in the multiple regres-
sion represented a single measure of the independent
variable in one of the seven habitats during one of 15
months. Thus, there were 105 observations for each
independent variable, or a total of 630 data points for
the regression analysis. Data were logarithmic-trans-
formed prior to analysis to help satisfy assumption of
normality of the residuals. Collinearity diagnostics,
such as tolerance values and variance inflation factors,
indicated a lack of colinearity between the regres-
sors, hence all independent variables were retained in
the model.
Simple linear regression, performed with SAS PROC
REG (SAS Institute Inc. 1990), was used to compare
Coyote visitation rates against mice abundances in
each of the two adjacent habitats, Tallgrass Prairie I
and Oak Woods I. We performed a separate analysis for
the response of Coyotes to prey increase following
manipulation of the prey’s food supply. Visitation rates
of Coyotes around the experimental plots in Tallgrass
Prairie II were analyzed using a one-way repeated
measures analysis of variance ((mANOVA), with SAS
PROC GLM (SAS Institute Inc. 1990). Inferences
were based on Huynh-Feldt adjusted P-values for the
rmANOVA.
Results
Among-habitat prey fluctuations
There was variation in spatial-temporal abundances
of prey species (Figure 2) with significant species
(R? = 0.658, Fro. 264) = 6.21, P = 0.002), time (Fry 264) =
21.29, P < 0.001), and time? (Fy, 264) = 14.17, P <
0.001) effects, indicating that overall numbers of the
three prey differed significantly. The significant time
X species (Fy 264) = 18.29, P < 0.001) and time* x spe-
cies (Fi, 964; = 11.74, P < 0.001) interactions indi-
cated that the rate at which prey species numbers
changed also differed significantly. This was primar-
ily due to the substantial increase in mice numbers
(Figure 2). Furthermore, the significant time x habi-
tat x species (Fry. 264) = 4.51, P < 0.001) and time? x
habitat x species (Fi, 364; = 4-84, P < 0.001) inter-
actions indicated that the differential rates in changes
of numbers of species also changed among the dif-
ferent habitats. For example, the highest abundances
of mice and voles occurred in November 1994 in the
habitats Oak Woods I and Tallgrass Prairie I, res-
pectively. The highest Sylvilagus abundance was docu-
mented in October 1994 in the Oldfield, with nearly
equally high numbers recorded in July 1994 in the
RANDA and YUNGER: SCENT STATION VISITATION RATES OF COYOTES 345
two prairie sites, probably following the weaning period
of young rabbits in northern Illinois (Hoffmeister 1989).
These abundance peaks are reflected in the quadratic
function of the change in prey numbers over time.
Among-habitat Coyote visitation rates
Scent station visitation rates fluctuated widely among
habitats and over time; no signs of Coyotes were found
in Oak Woods II and the majority of tracks were re-
corded in the grassland habitats (Figure 3). Overall,
the multiple regression of Coyote scent station visita-
tion rates across Fermilab with the three main prey
(Figure 4) and the three habitat structure variables
(Figure 5) was significant (R* = 0.241, Fy, og) = 4.40,
P = (0.003; Table 1). The unexplained variance in the
model may be attributed to the observed variation in
Coyote visitation (Figure 3) and 0 values recorded for
prey abundances. Based upon results of the multiple
regression, we conducted a separate analysis to discern
whether the visitation rates in grasslands by Coyotes
was due to prey (Microtus) or avoidance of wooded
areas, from which voles were absent. Regression of
scent station visitation rates with vole abundance, ex-
cluding data from the two oak woods, was not signi-
ficant (7? = 0.050, Fy, 73; = 3.75, P = 0.057).
In comparing Coyote visitation in the two adjacent
habitats, Tallgrass Prairie I and Oak Woods I, scent
station visitation rates, when averaged over the study
period, were over three times greater in the prairie
(0.035 + 0.011 (mean + SE ); range 0.000—0.0645),
than the woods (0.008, + 0.003, range 0.000—0.0179;
tog) = 2-486, P = 0.026). However, mice abundance
was two times greater in the oak woods (4.7 individ-
uals per transect + 1.4, range 0.0—19.3) than the
prairie (2.3 individuals per transect + 0.6, range
0.3—8.0; fig) = 1.637, P = 0.113).
Within-habitat Coyote visitation rates
The fire in Tallgrass Prairie I did not result in a
substantial increase in prey (Figure 2). However, the
perturbation in Oak Woods I was followed by a con-
siderable increase in mice abundance, enabling a
within-habitat comparison to Coyote activity. Despite
the high prey abundance, Coyote visitation rates were
not significantly related to mice abundance (7° = 0.158,
Fry, 13) = 1.03, P = 0.389) in Oak Woods I.
Food supplementation in Tallgrass Prairie II resulted
in an approximately three-fold increase in numbers
of mice compared to the non-supplemented plots by
February 1995 (Figure 6). Numbers subsequently dec-
lined until densities converged on the supplemented
and non-supplemented plots in May 1995. Coyotes
responded to the peak in mice densities with mean
visitation around the food supplemented plots over five
times greater than on non-supplemented plots in Feb-
ruary 1995 (Figure 6). Coyote visitation around these
plots in the ensuing three months reflected the trend
in prey availability. The result was a significant food
effect (Fi, >, = 25.60, P = 0.037), a significant time
effect (Fi; 6 = 9-79, P = 0.013), and a significant
346 THE CANADIAN FIELD-NATURALIST Vol. 118
@—® Tallgrass Prairie I &—L Oak Woods II
4— A Oldfield
O--O Shrubby Oldfield
v--v Brome Grass Field
C—O Tallgrass Prairie II
@— 8 Oak Woods I
Peromyscus
Microtus
Mean Number of Individuals per 200-m Transect
Months
FiGuRE 2. Abundances of the three main prey, Peromyscus, Microtus, and Sylvilagus, in each of the seven habitats over time.
2004
0.35
0.30
O25
0.20
0.15
0.10
0.05
Mean Scent Station Visitation Rate
(proportion stations visited / operative days)
0.00
RANDA and YUNGER: SCENT STATION VISITATION RATES OF COYOTES 347
Tallgrass Prairie I
Tallgrass Prairie II
Oakwoods I
Oakwoods II
Oldfield
Shrubby Oldfield
Brome Grass Field
Months
FicureE 3. Habitat visitation of Coyotes, based upon monthly average scent station visitation rates, over time among the
seven habitats.
visitation X time interaction (F/; ) = 10.32, P = 0.012).
Vegetation characteristics of habitats
Of the three vegetation metrics collected, percent
ground cover and canopy cover estimates were fairly
consistent between the non-growing and growing
seasons for each of the seven habitats sampled (Table
2). Vertical foliage density was greater in the growing
season than the non-growing season for all habitats,
reflecting the increase in above-ground plant biomass.
Tallgrass Prairie I had the greatest difference in ground
cover and foliage density between these seasons. This
was due to the almost complete absence of litter and
standing vegetation during the March survey, except
for small clumps of tall grasses, a result of the previous
fall’s fire. There were similar trends of vegetation met-
rics among similar habitats. Vertical foliage density
was greatest in the prairies compared to other habitats
during the growing season, but was relatively low for
the woods. The habitats dominated by grasses, the
prairies and brome grass field, exhibited > 97% ground
cover, exceeding estimates of other habitats. Canopy
cover, as expected, was highest in the woods, with
Oakwoods II having a denser overstory than Oak-
woods I. The presence of canopy in the brome grass
field was attributed to a few isolated trees located
near the middle of the field, which was not expansive
enough to markedly influence Coyote visitation.
Discussion
Coyote habitat visitation, measured through scent
station visitation rates, fluctuated greatly over time,
showing no clear temporal pattern among habitats.
However, overall visitation indicated an extensive use
of grasslands and avoidance of woodlands. Through-
out the duration of the study, there was no evidence
of Coyote tracks or scat in Oak Woods II, a mature
woodlot with few gaps in its overstory, even though
its entire western side bordered a tallgrass prairie, a
habitat where Coyote scat and tracks in snow were
observed. Oak Woods I also experienced relatively
little Coyote visitation during most of the study.
Although scent station transects were 50 m from
habitat edges, all Coyote tracks were observed at the
western end of the transects, which were closest to a
grassy area near the woods. The shrubby oldfield
experienced slightly more visitation, overall, than the
woods, but tracks were found primarily at scent sta-
tions within open grassy areas and in the western por-
348 THE CANADIAN FIELD-NATURALIST Vol. 118
Peromyscus
Sylvilagus
Mean Coyote Visitation Rate (proportion stations visited / operative days)
0.0 0.5 1.0 IS 2.0 De) 3.0
Mean Number of Prey per 200-m Transect
Ficure 4. Partial regression plots for activity of Coyotes vs. abundances of each of the three main prey species. Each point
represents a single observation recorded during | of 15 months in one of the seven habitats.
) 2004 RANDA and YUNGER: SCENT STATION VISITATION RATES OF COYOTES 349
vertical foliage density
canopy cover
ground cover
Mean Coyote Vistation Rate (proportion stations visited / operative nights)
Means of Vegetation Variables
| Ficure 5. Partial regression plots for activity of Coyotes vs. each of the three vegetation variables. Each point represents a
single observation recorded during | of 15 months in one of the seven habitats.
350
GY
WSS
WN
4
‘
Lf
Ny
NS
SS
fee
KK
Mean Number of Peromyscus per Plot
Yj
Y
j
L
Y
Months
THE CANADIAN FIELD-NATURALIST
—@— Peromyscus density, +F
—O©Q-—. Peromyscus density, -F
WZ, Visitation rate, +F
[___] Visitation rate, -F
Vol. 118
Mean Coyote Visitation Rate
(proportion stations visited / operative nights)
FIGURE 6. Comparison of activity of Coyotes and abundance of mice on food-supplemented (+F) and non-supplemented (-F)
plots in Tallgrass Prairie II.
tion of this habitat which bordered a tallgrass prairie.
These observations were supported by the significant
negative relationship of canopy cover to Coyote visita-
tion rates in the multiple regression analysis. Hence,
Coyotes may move a limited distance into woods but
tend to avoid core areas of heavily wooded habitats.
This behavior was corroborated by a two-year radio
telemetry study of Coyotes in northeastern Illinois
(Roth et al. 1999°).
The multiple regression analysis also indicated scent
station visitation rates by Coyotes were affected by
abundance of voles, which was not found in the oak
woods studied. However, a simple regression of Coy-
TABLE |. Parameter estimates for independent variables used
in the multiple regression analysis of Fermilab Coyote activities.
Variable df Regression
coefficient Jz
Intercept 0.0261 0.040
Peromyscus 1 -0.0082 0.192
Microtus 1 0.1192 0.006
Sylvilagus -0.0169 0.359
Foliage Density 1 -0.0441 0.295
Canopy Cover 1 -0.0632 0.004
Ground Cover 1 0.0082 0.871
ote visitation rates on vole abundance, excluding data
from the two woods, did not reveal a significant rela-
tionship. Thus, it appeared that factors other than prey,
such as vegetation structure, strongly influenced Coy-
ote habitat visitation at Fermilab. In addition, overall
visitation rates were not related to the abundance of
Eastern Cottontails, which comprised the greatest
biomass of prey in the Coyote diets (Randa 1996).
This could possibly be attributed to the association of
cottontail rabbits along habitat edges (Althoff et al.
1997; Mankin and Warner 1999; Smith and Livaitis
2000). Although some of the scent station transects
were located within habitat areas where rabbits were
found, Coyotes could have spent more time foraging
for rabbits along these edges where transects were
not located.
The selective use or visitation of grasslands by the
Coyotes in this investigation may be associated with
their historical range. Prior to European settlement,
Coyotes occupied the southwest and central plains
of the U. S. including grassland of southern Canada.
Clearing of forests and extermination of the Grey Wolf
(Canis lupus) facilitated the north- and eastward expan-
sion of Coyotes. Coyotes moved northward along the
Great Lakes, and colonized the northeastern U.S.
)
2004. RANDA and YUNGER: SCENT STATION VISITATION RATES OF COYOTES 35]
TABLE 2. Summary of vegetation characteristics for the seven different habitats sampled twice during 1995 at Fermilab; NG
= non-growing season sampling, G = growing season sampling.
Mean Vertical Mean Percent Mean Canopy
Foliage Density* Ground Cover Cover?
Habitat NG G NG G NG G
Tallgrass Prairie I 0.031 0.703 352, 98.0 0.000 0.000
Tallgrass Prairie II 0.320 0.761 OED 97.5 0.000 0.000
Oakwoods I 0.196 0.377 94.7 89.7 0.750 0.792
Oakwoods II 0.132 0.172 66.4 52.4 1.000 1.000
Oldfield 0.328 0.459 89.4 89.2 0.000 0.000
Shrubby Oldfield 0.248 0.587 96.7 89.5 0.389 0.340
Brome Grass Field 0.180 0.346 100.0 99.7 0.042 0.021
“Based upon the average proportion of three profile boards obscured by vegetation for 24 sampling stations per habitat.
>Based upon presence/absence scores (1/0 respectively) for 24 sampling stations per habitat.
(Richens and Hugie 1974) and the Midwest (Moore
and Parker 1992) by the 1940s. Most Coyotes still in-
habit deserts and grasslands, and those in regions with
forests tend to use open, non-forested areas in a great-
er proportion than available (Todd et al. 1981; Toweill
and Anthony 1988; Cypher 1991; Holzman et al.
1992; Murray et al. 1994; Kamler and Gipson 2000).
Tracks of Coyotes observed in the snow at our study
site indicated that grasslands, such as the brome grass
field and tallgrass prairie, were occasionally traversed
by Coyote tracks following a relatively straight path,
reflecting non-foraging behavior. Hence, these open
areas may not only serve as preferential foraging sites
but as areas facilitating movement between habitats.
A preferential use of grasslands may explain why
chipmunks and tree squirrels, which were moderately
common in the woodlands, were rarely detected in
Coyote diets (Randa 1996).
Selective use of grasslands may have restricted the
ability of Coyotes to respond spatially and temporally
to localized patches of abundant prey within a habi-
tat. In Fall 1994, when mice densities in Oak Woods
I were more than twice the prey abundances at any
other location, Coyote visitation did not increase sig-
nificantly in that habitat. This discrepancy of prey abun-
dance and coyote response in woodland corresponds
with findings in southeastern Quebec (Richer et al.
2002). However, Coyotes demonstrated an ability to
closely track prey within a grassland (Tallgrass Prairie
II) as their visitation rates were correlated with ex-
perimentally manipulated abundant patches of mice.
The high level and subsequent decline in Coyote visi-
tation rates detected on scent stations around food-
manipulated plots paralleled the change in mice
densities. Hence, once mice decreased following a
peak in densities on these plots, Coyote visitation rates
likewise diminished. It was unlikely that Coyotes were
responding to a novel item in the environment (such
as the odor of the food) because supplementation had
been initiated four months prior to the scent station
monitoring. Because voles were not detected in this
habitat during the experiment, a similar test of within-
habitat Coyote response to abundant patches of this
commonly consumed prey was not feasible. Yet, as
with mice, Coyotes could have responded to isolated
patches of voles within habitats throughout Fermilab,
given that voles were still a major component of Coy-
ote diets despite their low availability.
One limitation of the scent station transects was the
difficulty in identifying Coyote responses to possible
small, isolated patches of prey. Also, due to the large
areas over which Coyotes may move, there was not
sufficient separation to avoid visitation by the same
individual between scent station transects (Diefenbach
et al. 1994; Roughton and Sweeny 1982). However,
by intensively sampling each habitat, these transects
were effective in discerning overall trends (i.e., among-
habitat comparisons) in Coyote visitation rates and rel-
ative habitat use; they were not intended to indicate
finer-scale or localized responses (e.g., patch-level
foraging) within the study site.
The results we obtained from both the experimen-
tal plots and scent station transects demonstrated that
Coyotes exhibit variable responses to prey availability,
depending upon habitat type. Reacting relatively quick-
ly to a local increase in prey, as seen around the ex-
perimental plots in prairie, would enhance Coyote
foraging efficiency. However, preferential use of open
areas, as suggested by the transect data, may con-
strain foraging efficiency during periods of very low
prey densities when alternative prey in woodlands is
under-utilized. Hence, supporting Coyote populations
near urbanized areas, as in northern Illinois, requires
open land expanses such as grasslands to facilitate
movements across large spatial extents within the land-
scape and to provide an adequate prey base.
Acknowledgments
P. L. Meserve lent support and guidance throughout
the course of this investigation. S. Scheiner and C.
von Ende provided statistical advice. D. Cooper shared
in much of the field activity. J. Mendelson, E. Miller,
392
C. Petersen, B. Satterfield, and several anonymous
reviewers provided helpful comments on earlier drafts
of this manuscript. R. Walton oversaw Fermilab activ-
ities associated with this project and helped obtain
funding. The National Environmental Research Park
of the U.S. Department of Energy (MO-RS023), and
the Department of Biological Sciences, Northern
Illinois University provided funding for this study.
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June 1999,
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Accepted 14 October 2004
Presence of Cavities in Snags Retained in Forest Cutblocks:
Do Management Policies Promote Species Retention?
Ki T. Everett!:? AND KEN A. OTTER?
‘Forestry Program, University of Northern British Columbia, Prince George, British Columbia V2N 4Z9 Canada
"Ecosystem Science & Management Program, University of Northern British Columbia, Prince George, British Columbia
V2N 4Z9 Canada
3Current Address: Department of Biology, University of Victoria, Victoria, British Columbia V8W 2Y2 Canada
Everett, Kim T., and Ken A. Otter. 2004. Presence of cavities in snags retained in forest cutblocks: do management policies
promote species retention? Canadian Field-Naturalist 118(3): 354-359.
Tree cavities, which are frequently excavated by primary cavity nesters, are typically used by a number of avian and non-avian
species and are thus important components in maintaining biodiversity in forest ecosystems. One way to provide these
habitat opportunities in harvested areas is through the retention of snags. In this study, we assessed the habitat and snag
characteristics that promote cavity excavation, using the presence of cavities to infer activity of primary cavity excavators.
Snags retained closer to the forest/cutblock edge contained a greater density of cavities than trees further from edge. However,
the proportion of cavities found within cutblocks declined at a more rapid rate with distance from edge than did those in adja-
cent forested stands. There was also a tendency for cavities to occur more frequently in trees that were at the advanced stages
of decay. The results of our study suggest management for snags in harvest areas should include the retention of snags
closer to the forest edge combined with incorporating trees showing signs of advanced decay.
Key Words: tree cavities, snags, forest edge, birds, mammals, reptiles, British Columbia.
Snags (standing dead trees) provide specialized hab-
itat for many species, which in turn play an integral role
in maintaining ecosystem functions (Machmer and
Steeger 1995*). Approximately 16% of the indigenous
birds, mammals, and reptiles in British Columbia de-
pend to some extent on snags or cavities for repro-
duction, feeding, and shelter (Backhouse and Lousier
1991*). These dependent species then create habitat
opportunities for other wildlife species, facilitate seed
dispersal, increase soil aeration, accelerate organic
decomposition, and can even aid in controlling forest
pests (Machmer and Steeger 1995*). Although snags
play an important role in the ecosystem, their removal
has traditionally occurred in past forest management
(ostensibly to reduce hazards — lightning attraction,
falling snags, etc. — and foci of infection for healthy
trees).
By retaining trees of varying ages, diameters, and
decay classes in cutblocks, the vertical structure of
vegetation, total percent vegetation, and percent decid-
uous cover increase. These changes can lead to greater
species richness and diversity in both plant and mam-
mal communities (Davis et al. 1999*). Population den-
sities of cavity-nesting species are often limited by
potential nest sites (Runde and Capen 1987), and inten-
sive forest management that removes snags reduces
their densities in managed stands compared to natural
stands (Haapanen 1965; Pojar 1995).
Primary cavity nesters (those which excavate their
own cavities, such as woodpeckers and some chicka-
dees: Thomas et al. 1979) appear to prefer stands with
a high number of snags (Zarnowitz and Manuwal 1985;
Raphael and White 1984). As most primary cavity-
nesting birds rarely occupy nests that they themselves
have not excavated (Short 1979), suitable trees, in-
cluding snags, must be available for excavation for
nests or roosts. Snags offer softer excavating substrates
as well as important foraging sites for these species.
Conversion of natural forests into intensively managed
stands which lack snags may, therefore, have long-term
negative effects on the entire cavity-nesting populations,
as secondary cavity-nesting species rely on primary
excavators for cavity creation (Peterson and Grubb
1983).
Bodies that govern forestry practices recognize the
importance of snags, and advocate the retention of a
variety of tree species at various stages of decay in
managed forests (e.g., Machmer and Steeger 1995*).
In an effort to reduce the impact of large openings
created by cutblocks, some forest companies retain
windfirm deciduous trees and advanced regeneration
that fall below utilization standards to aid in main-
taining structural diversity in cutblocks. This limits
the distance wildlife must travel through the cutblock
without vegetative cover. The traditional paradigm has
been that efforts such as these will be sufficient to
maintain wildlife and biodiversity throughout managed
forests.
One aspect of snag retention policy that has been
overlooked, however, is the behavioral characteristics
of primary cavity-nesting species that may deter mem-
bers of this guild from occupying trees left specifically
for their use. Many forest birds avoid areas outside
forested cover (Hegner 1985; Desrochers and Hannon
354
2004
1997), as open spaces leave these species susceptible
to hawk and falcon predation (Corral 1989). Several
studies have shown that many forest dwelling species
are reluctant to cross gaps between fragmented forest-
ed areas (Lens and Dhondt 1994; Desrochers and
Hannon 1997). Desrochers and Hannon (1997) found
that forest birds were three times less likely to cross
gaps 70 metres wide, and eight times less likely to
cross gaps 100 metres wide compared to similar dis-
tances within the forest. Machtans et al. (1996) also
found that movement rates of forest birds across cut-
blocks were significantly lower than movement rates
within the forest. Instead, forest birds preferred to travel
much greater distances through corridors, rather than
crossing narrow gaps (Desrochers and Hannon 1997).
The avoidance of open spaces indicated that forest
birds — with the majority of those studied belonging
to the cavity-nesting guild — have fewer habitat oppor-
tunities as the landscape becomes increasingly frag-
mented. Although retained snags may be scattered
throughout cutblocks to provide nest sites, the gap
between the forest edge and the snag may be too sub-
stantial for birds to cross. In turn, the number of cavity-
nesting birds may decline with increased distance into
cutblocks as compared to the surrounding forest.
In this study, we documented the presence of cavi-
ties in retained snags within forest cutblocks as a mea-
sure of use by cavity-excavating species, and compared
this to similar trees found within the surrounding for-
est. If primary cavity nesting species avoid openings
in forest cover, we predict fewer cavities as one travels
further from the forest edge into cutblocks. By assess-
ing attributes of cavity-possessing trees, we attempt
to identify which tree characteristics and tree species
cavity nesting birds tend to utilize. Our aim is to
provide well-substantiated recommendations towards
the placement and creation of retained snags within
cutblocks that maximize potential usage by cavity
nesting species.
Methods
Study Area
This study was carried out from 30 September to 5
November 2000, approximately 30 kilometers west of
Prince George, British Columbia (53°36'35"N,
122°57'29"W). All samples were located within the
Sub-Boreal Spruce biogeoclimatic zone, which covers
much of the central interior of British Columbia
(MacKinnon et al. 1992). The study area was primarily
composed of coniferous and mixedwood forests, with
species including Lodgepole Pine (Pinus contorta
var. latifolia), hybrid White Spruce (Picea glauca x
engelmannii), Sub-alpine Fir (Abies lasiocarpa), Doug-
las-fir (Pseudotsuga menziesii var. glauca), Trembling
Aspen (Populus tremuloides), Black Cottonwood (Pop-
ulus balsamifera ssp. trichocarpa) and Paper Birch
(Betula papyrifera). Harvested areas are typically re-
planted with Lodgepole Pine, with a small component
of hybrid White Spruce on moister sites.
EVERETT AND OTTER: PRESENCE OF CAVITIES IN SNAGS 355
Sampling Procedure
We randomly selected eight cutblocks for the survey
from a Forest Development Map. The cutblocks ranged
in age from 3 to 10 years post-harvest, and from 30 to
60 hectares in size. A line-transect method of sampling
was used. In this method, all retained snags falling with-
in 5 metres of each side of the transect were measured.
We ran transects on a bearing perpendicular to the for-
est edge, with a random point of commencement along
the edge being selected from the Forest Development
map. Measurements were carried out until the centre-
line of the cutblock was reached and at least 20 snags
were encountered. In one case, the cutblock contained
only 17 retained snags. Due to the minimal number
of retention trees present, the line-transect method
would have been relatively ineffective; therefore; all
retention trees in the cutblock were measured.
Snags were defined as any dead, standing tree (Smith
et al. 1997: 489). We recorded all cavities that were
either actively excavated or were natural cavities of
similar size, which displayed signs of active use (e.g.,
modification to the cavity, presence of feathers in
entrance, etc.). Cavities were only recorded if they had
a minimum diameter of 3.5 cm, as the cavity had to
be large enough for use by a small bird or mammal.
However, as our study was looking for evidence of use
of the trees rather than specifically focusing on nesting,
we did not distinguish between cavities used for roost-
ing versus those where nesting had occurred. For each
snag encountered along the transect, we recorded sev-
eral attributes: tree species, height, diameter at breast
height (DBH, measured at 1.3 m from the base of the
tree), decay class, number of cavities, distance from
the nearest timber edge, percent overhead cover, and
the number of snags and live trees within an 11.28 m
radius around the trees. Only trees greater than 10 cen-
timeters DBH were recorded, as this reduced the chance
of incorporating regeneration into the study. Decay
class was determined using a six-step hardwood classi-
fication scheme combined with a corresponding nine-
step coniferous classification scheme (Ministry of
Forests 2000*).
Similar transects were placed in the adjacent forest-
ed stands running perpendicular to the edge. In order
to measure a similar number of trees over the same dis-
tance in both habitat types, every third tree classified
as decay class 2 or greater was measured. In order to
determine the initial tree for measurement along each
transect, a coin toss was completed to decide if the
first or second tree should be measured. For each tree
encountered along transects in forested stands, the
same attributes were measured as those collected for
cutblock sampling.
Statistical Analysis
A multiple regression was used to determine if the
habitat (forest or cutblock) and distance from the for-
est edge influenced the proportion of cavities found
(SYSTAT 9.01). To compare the distribution of tree
356
types across the two habitats, we employed a Chi-
square and used a Mann-Whitney U test to compare
the frequency of decay classes of trees between cut-
blocks and forested stands.
To determine which characteristics tended to predict
the presence of cavities in wildlife trees, we conduct-
ed a Principal Component Analysis (PCA) on trees in
the forested stands. As the forest stands constitute the
natural habitat of many of the primary cavity-nesting
species, determining the characteristics of cavity-bear-
ing trees in these areas may give insight into which
types of wildlife trees are important to retain in
cutblocks. The following characteristics of the focal
tree and the immediate area were subjected to PCA:
height, diameter, and decay class of the focal tree, along
with the total number of trees, number of live trees,
number of snags, and percent overhead cover within
the 11.28 metre radius plot. A linear regression was
used to compare the number of tree cavities against
the PCA factor scores. The PCA was carried out in
SYSTAT 9.01 using Varimax rotation.
Two retention trees measured had extremely high
numbers of cavities and were identified during initial
analysis as significant outliers in the data set (Durbin-
Watson D Statistic = 1.984, P < 0.01). These were
excluded from subsequent analysis.
Results
In total, 185 trees were measured at our eight sam-
pling sites; 94 trees within cutblocks and 91 trees within
forested stands. We found 46 cavity-bearing trees, con-
taining a total of 67 cavities. Of the 46 trees containing
cavities, 29 were deciduous while the remaining 17
were conifers.
A greater proportion of deciduous trees contained
cavities compared to coniferous species. Species of
willow had the highest proportion of cavities, with
two of the three trees observed containing cavities.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Trembling aspen was found to have the second highest
frequency of cavities with 17 of the 62 trees observed
containing cavities. A breakdown of the number of
cavities recorded by species is given in Table 1.
The species composition of trees differed between
the two habitats (x? = 76.6, df = 6, p< 0.01 — Figure 1).
Snags in cutblocks were primarily deciduous species;
although these trees were also present in forested
stands, the latter stands had a proportionately higher
coniferous component.
Distance From Edge and Cavity Abundance
Distance from forest edge and stand type (cutblock
or forest) both had a significant effect on the number
of cavities found (multiple regression: 17=0.051,
Fo 19) = 4-857, p = 0.009). The further a tree was
located from the forest-cutblock edge, the lower the
frequency of cavities (p = 0.027). There was also a sig-
nificant effect between the stand types, as more cavities
were found in the forest than were found in the cut-
block (p = 0.020). In the forest stands, the decline in
number of cavities found with distance from the edge
was not as dramatic as that seen in cutblocks (Figure
2a and b).
Stand Characteristics Associated with Snags
The principal component analysis identified two
factors that accounted for 56.2% of the total variance
among retained snags (Table 2). Principal component
one (PC 1) accounted for 31.2% of the variance, with
strong positive weightings for a high number of total
trees and a high number of live trees within an 11.3 m
radius plot. As a result, PC 1 can be considered a meas-
ure of the density of trees surrounding the snag.
Principal component two (PC 2) accounted for
25.0% of the total variance, with a strong positive weight-
ing for decay class and a strong negative weighting
for tree height. PC 2 indicates trees at the latter stages
of the decay process, as tree height frequently decreases
TABLE |. A breakdown of the number of cavities by tree species.
Tree Species Number
of trees
observed
Trembling Aspen
Populus tremuloides 62
Lodgepole Pine
Pinus contorta var. latifolia 52
Paper Birch
Betula papyrifera Sy)
Hybrid Spruce
Picea glauca X engelmannii 24
Willow
Salix sp. 3
Black Cottonwood
Populus balsamifera ssp. trichocarpa 8
Douglas Fir
Pseudotsuga menziesii glauca 4
Total (Average) 185
Total number
of trees
Percentage
of trees Total number
with cavities with cavities of cavities
17 27.4 32
13 25.0 14
8 25.0 10
4 16.7 5
2 66.7 3
2 25.0 3)
0 0 0
46 (24.9) 67
2004
70 | Cutblock
” Forest
a)
o
Qa
2)
S38
ae
ES
25
CJ
Q
n
x
o
”
Populus balsamifera
Populus tremuloides
Betula papyrifera
Pseudotsuga menziesii
Pinus contorta
Picea glauca
Tree Species
FiGure 1. Distribution of sampled snags within cutblocks
versus surrounding forest stands.
as the tree reaches the higher decay classes (Towers
et al. 1992).
Response of Cavity Nesters to Stand Characteristics
There was no significant relationship between the
number of cavities found and PC | (regression: r* =
0.003, Fo 99) = 0.281, p = 0.60). There was, however, a
significant effect between the number of cavities being
found and PC 2 (regression: 1? = 0.092, F,, 99) = 9.13,
p = 0.003) indicating that more cavities occurred in
trees with a higher amount of decay.
On average, the snags retained in clearcuts had
less decay than the comparison cohort of trees in the
forested areas (MWU: U = 2918.5, n= 93, 91, p<0.01).
Table 2. Principal component analysis of stand characteris-
tics in forest stands. The first two Principal Components ac-
count for greater than 50% of the total variance among stand
attributes; therefore only these two factors were considered
in subsequent analysis. Variables that were within 10% of
the highest loading were considered to be strong weightings,
and are shown in bold.
Variable Real PE2
(clustering of (decay
retention trees) stage)
Tree Diameter -0.407 -0.395
Tree Height 0.272 -0.714
Decay Class -0.353 0.738
Total Number of Trees 0.947 0.212
Number of Live Trees 0.956 0.115
Number of Snags 0.000 0.392
Percent Overhead Cover -0.029 0.573
Percent of Total Variance
explained by each Factor SIRS 25.02
EVERETT AND OTTER: PRESENCE OF CAVITIES IN SNAGS
a. Forest
n
ut
=
>
<x
oO
LL
Oo
a 0 100 200 300 400
rea)
=| b. Cutblock
=)
Zz
[o)
TDC O
yea ae I EE Be UE
100 200 300 400
DISTANCE FROM EDGE (m)
FIGURE 2. Regressions of distance from forest edge against the
number of cavities located in trees in forested stands
(a — shown by a dotted line) and cutblocks (b — shown
by dashed line).
Discussion
Edge Effects on Cavity-nesting Birds
The number of cavities located within both cutblocks
and forested stands were related to the distance from
forest edge. Trees located farther from the forest edge
had a tendency to contain fewer cavities than trees
located closer to the forest edge. There was also a
greater abundance of cavities located within forested
stands than within cutblocks. Yet, although the number
of cavities declined rapidly as the distance from cut-
block edge increased, the equivalent decline was less
rapid in forested stands. This suggests that retained
snags farther from forest cover were underutilized by
cavity-excavating species.
One possible bias in our results might arise if cavi-
ties found in the cutblocks existed prior to harvesting.
Although we focused on measuring cavities that ap-
peared to be recently used/excavated, it was occasion-
ally difficult to distinguish between recently excavated
cavities and cavities that may have existed prior to
logging. However, if some of the cavities existed prior
to harvest our results would over-estimate the level of
activity of cavity-excavating species in cutblocks, thus
minimizing the perceived effect of harvesting on cavity
nesters. Despite the possible bias of including pre-exist-
ing cavities, we continued to see a reduced number of
358
cavities in clearcuts. Thus, the magnitude of the effect
we report may be even more pronounced between the
different habitats.
Several possible explanations may exist for the low-
er densities of cavities within cutblocks. The reduced
number of cavities in cutblock trees could be due to
the reluctance of many species of forest birds to cross
large openings. Desrochers and Hannon (1997) found
that forest birds were extremely vulnerable to raptors
when they fly in the open, and thus were hesitant to
enter such areas. Secondly, the lower densities of tree
cavities within cutblocks could be due to the retention
of trees with minimal habitat value for cavity nesting
species. Cavity nesters tended to prefer deciduous tree
species, as a greater number of cavities were found in
these trees than in coniferous tree species. In conifer-
dominated ecosystems, such as boreal and sub-boreal
forests, deciduous trees often have greater heartwood
decay than conifers and may be preferred as nesting
substrate once the trees become snags, resulting in
increased avian diversity (Martin and Eadie 1999).
Yet, deciduous species accounted for a larger number
of snags in the cutblocks than the forests in our study,
and there was still a lower number of cavities in cut-
blocks than neighboring forests. While the retention
of these deciduous snags likely increases diversity
along the edge, the reluctance of birds to venture into
cutblocks may have a larger influence on snag use
farther from forest cover.
The highest density of cavities was located within
100 metres of the forest edge. Higher bird populations
located at the forest edge compared to the community
interiors has also been found in several other studies
(see Gates and Gysel 1978; McElveen 1979; and
Streikle and Dickson 1980). Several theories exist to
support such behaviour. Marcot (1983) suggested that
many cavity-nesting species nest in the nearby forest,
whereas they use cutblocks for foraging, resulting in
higher densities of birds seen along the community
edge. Both the Northern Flicker (Colaptes auratus) and
the Downy Woodpecker (Picoides pubescens), primary
cavity excavators, prefer to nest in old trees near open-
ings or on the edge of the forest (Ehrlich et al. 1988).
Our results suggest this pattern may occur within our
study area. Cavity density was highest at edges, but
remained high for greater distances into forests than
into cutblocks. Thus, marginal species attracted to edges
may prefer to either nest on the edge or penetrate into
the forest, rather than establish nests in snags retained
in the cutblocks. Coupled with non-edge species, this
would create the pattern of greater cavity abundance
in forested sites.
Tree Attributes and Cavity Abundance
Within forested stands, cavities were found more
often in trees that contained a combination of high lev-
els of decay and shorter tree height. Decayed portions
of the tree allow for easier cavity excavation for weak-
er cavity excavators, and the bark cover retains mois-
THE CANADIAN FIELD-NATURALIST
Vol. 118
ture and warmth as well as providing protection from
predators (Runde and Capen 1987). Decayed portions
of the tree also provide valuable foraging habitat as
they often contain high levels of beetle larvae, carpen-
ter ants, and termite activity, all of which act as food
resources for woodpeckers (Mannan et al. 1980). This
too may explain the lower use of cavities in cutblocks,
as trees retained in these areas had less decay com-
pared to trees sampled randomly in the surrounding
forests. This is likely the result of trees with greater
decay being removed as potential hazards during for-
estry operations. Retention of these higher decay class
trees, however, may be valuable in future planning. It
is important to retain trees at a variety of levels of
decay, as the nesting success of some primary cavity
excavators is higher in snags in the 2-3 decay class
range (Fort and Otter 2004).
Management Implications and Recommendations
Primary cavity nesters require specific habitat con-
ditions (Conner et al. 1976), and without these condi-
tions territory selection and reproductive success may
be compromised (Kilham 1966). As a result, popula-
tion densities of both primary and secondary cavity
nesters may decline.
In order to maintain the population levels of pri-
mary cavity-excavators it is essential to provide ade-
quate habitat through efficient forest management.
Snags and snag patches may be most efficient if they
are placed within 100 metres of the forest edge, as
this limits susceptibility of forest-dwelling birds to
predators. The retention of trees for the purpose of
managing cavity nesting birds should focus on main-
taining a high deciduous component within the stand.
Cavity nesters tended to select a high level of decidu-
ous trees for cavity excavation throughout this study.
Maintaining a variety of deciduous and coniferous
trees within cutblocks could prove to be beneficial
for population densities of cavity nesters, as well as
many other species of snag users.
Acknowledgments
We thank Sarah Parsons, Emma Tayless, and Der-
rick Lalonde for their help in the field, as well as Rod
Lenton and Chris Jones from Timberline Forest Inven-
tory Consultants Ltd. for providing maps and access
advice. We thank Kelly Sherman for providing advice
for sample planning as well as proof-reading numerous
drafts. Susan Stevenson and two anonymous reviewers
kindly provided feedback on the manuscript
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Received 28 March 2003
Accepted | October 2004
Summer Diet of Two White-tailed Deer, Odocoileus virginianus,
Populations Living at Low and High Density in Southern Québec
CLAUDE DAIGLE!:* , MICHEL CRETE! 3, Louts LESAGE” *, JEAN-PIERRE OUELLET?, and JEAN Huor?
' Ministére des Ressources naturelles, de la Faune et des Parcs du Québec, Direction du développement de la faune, 675
boul. René-Lévesque est, BP 92, Québec, Québec GIR 5V7 Canada; corresponding author
> Département de biologie et Centre d’études nordiques, Pavillon Vachon, Université Laval, Sainte-Foy, Québec G1K 7P4
Canada
> Département de biologie et Centre d’ études nordiques, Université du Québec a Rimouski, 300 Allée des Ursulines, Rimouski,
Québec GS5L 3A1 Canada
+ Present address: Environment Canada, Region de Québec, Service Canadien de la faune, 1141 Route de LEglise, C.P. 10100,
Ste-Foy, Québec G1 V 4H5 Canada
Daigle, Claude, Michel Créte, Louis Lesage, Jean-Pierre Ouellet, and Jean Huot. 2004. Summer diet of two White-tailed Deer,
Odocoileus virginianus, populations living at low and high density in southern Québec. Canadian Field-Naturalist
118(3): 360-367.
We investigated summer diets of two White-tailed Deer (Odocoileus virginianus) populations through rumen content analyses.
Samples from 93 deer were collected in a low density, LD (1 deer/km?) and a high density, HD (14 deer/km?) area of south-
ern Québec during the growing seasons of 1997 and 1998. Availability of preferred forage in forests was greater in LD than
in HD, whereas agriculture covered a larger proportion of the area in HD than LD. Rumen composition differed between the
two populations. Deer from HD consumed less forbs and leaves of shrubs and trees than did LD deer, whereas they con-
sumed more fruits, grasses and farm crops. The rarity in HD rumens of food items common in LD, as well as in many parts
of the White-tailed Deer range (i.e., Lilliacae), indicated that deer could not compensate for the rarity of preferred forest
forage by increasing foraging time and had to feed on cultivated crops. Rumen contents of LD deer had a higher level of cell
solubles and lignin, which reflected their greater reliance on quality forage growing in forests. Feeding habits and forage
quality can explain why deer body size decreased in HD between the 1970s and 1990s whereas LD deer remained large.
Key Words: White-tailed Deer, Odocoileus virginianus, diet, density, forest, agriculture, plant, Québec, Canada
Nous avons examiné le régime alimentaire estival de deux populations de cerf de Virginie (Odocoileus virginianus) par analyse
du contenu des rumens. Des échantillons ont été prélevés sur 93 cerfs provenant d’un secteur a faible densité de cerfs, LD,
(1 cerf/km?) et d’un secteur a haute densité, HD, (14 cerfs/km?) du sud du Québec durant la saison de croissance des végé-
taux de 1997 et 1998. La disponibilité des aliments forestiers préférés des cerfs était plus grande dans LD que dans HD alors
que la proportion du territoire agricole était supérieure dans HD. La composition des rumens des cerfs de chacune des régions
différait. Les cerfs de HD ont consommé de moins grandes proportions de plantes herbacées et de feuilles d’arbustes et d’ar-
bres que ceux du secteur LD, mais de plus grandes proportions de fruits, de graminées et de plantes agricoles. La rareté dans
les rumens du secteur HD d’aliments communs dans ceux du secteur LD et dans plusieurs autres régions de l’aire de répar-
tition du cerf (e.g., Lilliacae), indique que les cerfs du secteur HD ne pouvaient compenser pour la rareté de leurs aliments
préférés par un accroissement de la durée de la quéte alimentaire, et qu’ils devaient consommer des plantes agricoles. Les
cerfs de LD ont mangé des aliments contenant plus de solubles cellulaires et de lignine que ceux de HD, ce qui refléte une
consommation de plantes forestieres de bonne qualité. Le régime alimentaire et la qualité de la nourriture peuvent expliquer
pourquoi la taille des cerfs de HD a diminué entre les années 1970 et 1990 alors que celle des cerfs de LD est demeurée grande.
White-tailed Deer, Odocoileus virginianus, are selec-
tive feeders and although they ingest a wide variety of
plants, only a few taxa make up large proportions of
their diet (Johnson et al. 1995; Healy 1971; Korschgen
et al. 1980; McCaffery et al. 1974). Plant phenology
influences their diet; forbs and leaves of deciduous
woody plants are common food items in spring and
summer, and fruits become major components of the
autumn diet. White-tailed Deer also consume mush-
rooms in natural ecosystems (Crawford 1982; Johnson
et al. 1995; Korschgen et al. 1980; Short 1971; Skinner
and Telfer 1974), whereas farm crops can be major
food sources in agricultural landscapes (Nixon et al.
1991). During winter, White-tailed Deer switch to twigs
of both deciduous and evergreen woody plants and,
where snow cover allows access, they also use grasses
and farm crops left after harvest (Johnson et al. 1995;
McCaffery et al. 1974; McCullough 1985; Nixon et
al. 1991; Skinner and Telfer 1974).
Forage competition results in consumption of food
of reduced quality or availability, which lengthens
ingestion and digestion. At high density, forage compe-
tition can modify feeding habits of ungulates, in partic-
ular for small, selective species (Kie and Bowyer 1999)
and reduce body size in cervids (Ashley et al. 1998;
Créte et al. 1993; Hjeljord and Histol 1999; Lesage et
al. 2001). In mid-latitude deer, forage competition
during the growing season likely determines adult body
360
2004
size because growth and replenishment of body reserves
occur during this period of the year (Hjeljord and Histol
1999; Lesage et al. 2001; Boucher 2004).
On the south shore of the St. Lawrence River in
| Québec, the carrying capacity of the deer range de-
creases northward because suitable forest stands for
wintering become increasingly rare with increasing
| winter severity (Boucher 2004). Density averaged ~1
| deer/ km? in northernmost hunting zones of Québec
| whereas it locally exceeded 30 deer/km? in southern
zones after populations erupted due to mild winters
and a conservative hunting regime. Forage competi-
_ tion in winter regulates deer numbers in the absence
_ of Grey Wolves (Canis lupus) and under conservative
| hunting regime (Dumont et al. 2000), but agriculture
can help deer to survive winter by providing some food
_ during the dormant season (Rouleau et al. 2002a). In
recent decades, browsing pressure exhibited a pro-
_ nounced gradient on the south shore of the St. Law-
rence River, which resulted in a scarcity of preferred
summer forage in southern vs. northern zones (Rou-
| leau et al. 2002a). Vegetation sampling throughout
| the deer range in Québec showed a general pattern of
| negative relationship between deer density on one
hand, and preferred forest forage and deer size on the
_ other (Boucher 2004). Deer living at low density tend-
ed to avoid cultivated fields (Lesage et al. 2002) and
reached the largest size among Québec deer (Lesage
| etal. 2001).
We studied the summer feeding habits of White-
| tailed Deer in two areas which differed markedly with
respect to deer density, forage availability, impor-
_ tance of agriculture, and winter severity. The objective
_ of this study was to compare composition and quality
_ of summer diets of these two White-tailed Deer pop-
| ulations. We anticipated that preferred forage of deer
| living at low density would be less abundant in rumens
of deer living at high density and that the low density
population would consume forage of higher quality
due to relaxed forage competition during summer.
Study Area
Samples were collected in a low-density area (LD)
and a high-density area (HD) (Figure 1). The LD study
area is located in a transition zone between northern
hardwood forests and boreal forests (Rowe 1972*).
Among trees, Balsam Fir (Abies balsamea), White
Spruce (Picea glauca), Eastern White Cedar (Thuja
occidentalis), Trembling Aspen (Populus tremuloides),
and Yellow Birch (Betula alleghaniensis) dominate
(Lamoureux 1994*). Commercial logging has been
intensive in this region and the spruce budworm
(Choristoneura fumiferana) adversely impacted fir
and spruce stands in the late 1970s. Agriculture rep-
resents about 10% of the land use in the study area
and hay; alfalfa (Medicago sativa), cultivated and up-
graded pastures, oat (Avena sativa), and barley (Hor-
deum vulgare) cover most cultivated fields. The grow-
DAIGLE, CRETE, LESAGE, OUELLET, AND HUoT: SUMMER DIET OF DEER 36]
ing season averages 160 days (Wilson 1971*) and
snow cover often exceeds 50 cm for more than SO days.
Deer density was estimated through double-count aerial
surveys (Potvin et al. 1992) and averaged 1.1 deer/km?
in summer 1998 (Lamoureux and Pelletier 2000*).
Northern hardwood forests cover most of the HD
study area. Commercial logging has affected mainly
coniferous stands on small areas due to land owner-
ship and forest composition (Gosselin 1994*). Most
common tree species include Sugar Maple (Acer sac-
charum), Red Maple (Acer rubrum), Yellow Birch,
American Beech (Fagus grandifolia), White Ash (Frax-
inus americana), Balsam Fir, Hemlock (Tsuga cana-
densis), Eastern White Cedar, and White Spruce.
Forests have been cleared for agriculture throughout
the region. They have progressively grown back on
abandoned farms; and introduced plants such as apple
trees (Malus pumila) are common in today’s forests.
Agriculture now covers about 23% of the area. Hay,
corn (Zea mays), uncultivated pastures, cultivated
and upgraded pastures, and alfalfa dominate cultivat-
ed fields. The growing season averages 190 days and
snow cover rarely exceeds 50 cm. Deer density aver-
aged 14.1 deer/km? in summer 1996 (Dicaire 1999*);
locally it may exceed 30 deer/km?.
Methods
Forage composition — We collected rumen samples
from road kills during the growing season (13 May —
2 November 1997 and 1998). Rumen samples were
generally collected within 3 days after collision (maxi-
mum 5 days), provided that identifiable forage frag-
ments remained. Rumen content was hand mixed and
two one-litre samples were extracted. The first litre
was frozen for forage identification and the other pre-
served in 4% formalin for chemical analysis. At the
laboratory, frozen samples were thawed and washed
through a 7.9 mm and a 4.0 mm mesh size sieve (Créte
et al. 1990; Gauthier et al. 1989). About 50 ml of the
particles kept by the 4.0 mm sieve were spread into a
20 x 50 cm sampling tray (Chamrad and Box 1964)
and covered with 1 cm of water. One hundred particles
were systematically selected by point sampling (Créte
et al. 1990) and identified through macroscopic and
microscopic (10 — 25x) examination to family, genus
or species whenever possible. Reference plant samples
served for comparison during the identification process.
Samples were grouped by taxon and their volume
measured by water displacement (+0.25 mL). Plants
were grouped into eight categories for statistical analy-
ses: graminoids (Graminae and Cyperacae), farm crops,
forbs (without flowers or fruits), leaves of shrubs and
trees, wild flowers, wild fruits, mushrooms, and un-
known.
Forage quality — We reasoned that rumens of deer
consuming poor quality forage would contain fewer
nutrients with rapid assimilation and more nutrients
with slow digestibility than counterparts feeding on
362
better quality forage. Poor quality forage could also
include more secondary compounds slowing or in-
hibiting digestion. We measured cell solubles, lignin,
and phenolics as proxy for rapid digestibility, slow
digestibility and defensive compounds. We also deter-
mined nitrogen (N) content because it proved to be a
good indicator of summer diet quality in Caribou
(Rangifer tarandus) (Créte et al. 1990). We used the
detergent method (Gauthier et al. 1989; Goering and
Van Soest 1970) to measure cell solubles (1-NDF) and
acid detergent lignin (ADL) (Mould and Robbins
1982). Cell solubles are highly digestible whereas
lignin is largely not (Robbins 1993: 251, 294). Total
nitrogen content (N) was measured with an automat-
ed Macro-Kjeldahl analyzer and total phenolic con-
tent was determined by a calorimetric method using
the Folin-Ciocalteu reagent (Marigo 1973; Sauvesry
et al. 1991). Proteins are also highly digestible (Rob-
bins 1993: 294) whereas phenolics includes 8000 sub-
stances, of which tannins are known for reducing pro-
tein digestion (Robbins 1993: 300). Some samples
could not be analysed due to inadequate quantities.
All analyses were duplicated or triplicated whenever
a difference of more than 5% was found between the
first two measurements. The average of the two clos-
est estimates served as results.
Forage availability — We estimated forage avail-
ability during a companion study in the same study
areas (Rouleau et al. 2002a). We measured forage bio-
mass between the ground and 1.5 m in height at sites
used by radio-collared deer in the two areas through-
out the growing season with the help of 11 linear
regression models. Vertical and lateral plant coverage
over 2-m transects served as dependant variables in
regression models to predict plant biomass by species
(Rouleau et al. 2002b).
Data analysis — In a first step, we determined
whether sex (for deer >1 year old) and age (fawns vs.
>1 year old) influenced forage composition or quality
as summer progressed using MANOVA. We restricted
the analysis to the HD area because our samples from
deer with known sex and age were too small in the LD
area. Analyses were performed on sex and age with
respect to months, including sex by month, and age
by month interactions.
We used ANOVA for contrasting forage composi-
tion and quality between the two study areas. We
pooled months two by two for this analysis to ensure
adequate sample size for each period in both regions.
ANOVA were followed by pairwise protected LSD
tests (PROC GLM, PDIFF option, SAS Institute Inc.
1988). For all analyses, we ensured that residuals were
normally distributed (Shapiro-Wilk test) and homog-
enous (visual inspection of the plot). For forage com-
position, we carried out ANOVA on ranks because we
could not normalise residuals. We estimated means and
their standard error with the LSMEANS statement
(SAS Institute Inc. 1988).
THE CANADIAN FIELD-NATURALIST
Vol. 118
Results
Rumen samples were collected from 93 deer (HD
68 / LD 25): 64 adults, 11 fawns, and 18 of unknown
age. On a volumetric basis, 80% of the particles
examined could be identified to 68 food items. Males
and females showed no overall differences in the food
items they selected in the HD area when considering
forage categories (F = 0.52; df = 6, 38; P = 0.79) or
diet quality (F = 0.21; df = 5, 22; P = 0.95), without
sex X age interaction for composition (F = 0.77;
df = 24, 134; P = 0.76) and quality (F = 0.69; df = 20,
74; P = 0.83). Neither did age influence forage com-
position (F = 0.26; df = 6, 49; P = 0.95) or quality
(F = 2.27; df = 5, 28; P = 0.08), nor did it interact with
month on a composition (F = 2.31; df = 6, 53; P = 0.05)
or quality (F = 1.43; df = 5, 28; P = 0.24) basis. Given
these results, we did not take into account age and sex
in subsequent analyses.
Diet composition — Rumen contents differed between
the two study areas (Figure 2). In spring, rumens con-
tained no farm crops in LD but 13% in HD (P = 0.03).
Grasses (P = 0.08) and flowers (P = 0.07) also tended
to be more important food items in HD than in LD.
Conversely, forbs (P = 0.04) and leaves of shrubs and
trees (P = 0.12) accounted for a larger volume in LD
samples. Diets during July-August were more-com-
parable; the only significant difference was for forbs:
32% in LD vs. 7% in HD (P = 0.01). Rumens collected
during September and October contained more mush-
rooms (P < 0.01) and leaves of shrubs and trees
(P = 0.08) in LD, whereas those collected in HD includ-
ed more fruits (P < 0.01) and grasses (P = 0.08).
Differences between the two study areas were more
striking when considering taxa for the whole growing
season (Table 1). For this comparison, we eliminated
fruits, mostly apples, because they were almost restrict-
ed to HD and their more three-dimensional shape
contrasting with that of most other two-dimensional
plant tissues resulted in exceptionally large volume.
Excluding fruits, 19 food items each accounted for
more than 1% of the rumen volume in LD, summing
up to 95 % of volume, compared with 20 food items
making up 87 % of rumen content in HD. Forest forbs,
such as Yellow Clintonia (Clintonia borealis) and Wild-
Lily-of-the-Valley (Maianthemum canadense) were
common food items in LD but rare in rumens collect-
ed in HD. They were replaced in HD by forbs typical
of openings and by farm crops, such as clover (77i-
folium sp.) and alfalfa. Mountain Maple (Acer spica-
tum) and Mountain Ash (Sorbus americana), the most
common shrub leaves in rumens collected in LD, were
replaced by Red Maple, Choke Cherry (Prunus vir-
giniana), and Sugar Maple in HD; the latter species
were also consumed by LD deer, but to a much lesser
extent. Finally, apples, the most common item in HD
rumens, were found in only one LD sample.
Diet quality — Nitrogen (F = 0.91; df = 1, 52; P = 0.34)
and phenolic content (F = 0.13; df = 1, 52; P = 0.71)
2004
DAIGLE, CRETE, LESAGE, OUELLET, AND Huot: SUMMER DIET OF DEER 363
| Saint-Jean)
| Lac
70° 68° 66° 64°
) Septlles aaa |
| fe na
| ae
et nee
lle “ieee,
48° |
| White-Tailed Deer
rer! distribution Af
|__| Study areas
Ficure |. White-tailed Deer distribution in Québec and location of the two study areas, low density (LD) and high density (HD).
did not differ between the two areas, with nitrogen
remaining stable as the growing season progressed,
| and phenolic content declining in September-October
(Table 2). However, LD rumens contained more cell
solubles (F = 5.66; df = 1, 69; P = 0.02) and lignin (F
= 4.68; df = 1, 69; P = 0.03) than those from LD.
Discussion
Diet composition — Forage availability is reflected in
diet composition. Although climate differed between
LD and HD, the two regions shared most plant taxa
and natural forage species had similar digestibility in
both areas throughout the growing season (Lesage et
al. 2000). However, biomass of preferred forage species
found at sites used by deer was much larger in LD than
HD (Rouleau et al. 2002a). Food items which domi-
nated in LD diets remained almost absent from HD
rumens. For instance Liliacae, such as Yellow Clintonia
and Wild-Lily-of-the- Valley, which White-tailed Deer
normally consume in the Northeast (Crawford 1982;
Korschgen et al. 1980; McCaffery et al. 1974; Skinner
and Telfer 1974; Waller and Alverson 1997) occupied
a marginal volume in HD rumens. Liliacae are partic-
ularly vulnerable to deer browsing (Créte et al. 2001;
Waller and Alverson 1997) and can be used as indi-
cators to estimate the impact of White-tailed Deer on
plant communities (Balgooyen and Waller 1995). Wild-
Lily-of-the-Valley was common in HD in the early
1980s (Guérard and Legris 1984*). At the time of our
study, its biomass was 20 times lower in HD than in
LD (Rouleau et al. 2002a) and occurred as a marginal
food item in the diet of HD deer (Table 1). Although
not abundant on a volumetric basis, Wild-Lily-of-the-
Valley occurred in 16% of the rumens collected in
HD, showing that deer were still looking for this species
even though its availability was largely reduced. Moun-
tain Maple, which is known to be affected by deer
(Balgooyen and Waller 1995), was a common species
in HD in the past (Guérard and Legris 1984*), but
seemed almost extirpated at the time of our study
(Rouleau et al. 2002a). In LD, where natural forage is
abundant (Rouleau et al. 2002a), Lesage et al. (2002)
found that deer avoided cultivated fields. Our results
support their findings and indicate that White-tailed
Deer prefer to consume forest forages when they are
readily available during the growing season. In HD,
where most preferred food items had become scarce
(Rouleau et al. 2002a; Boucher 2004), deer switched
to other natural forage still persisting (e.g., Red Maple,
Choke Cherry and Sugar Maple) and relied on farm
364 THE CANADIAN FIELD-NATURALIST Vol. 118
May-June
GLD
gm HD
Farm crops Forbs Flowers Fruits Grasses Leaves Mushrooms
July-August
Farm crops Forbs Flowers Fruits Grasses Leaves Mushrooms
September-October
Farm crops Forbs Flowers Fruits Grasses Leaves Mushrooms
FIGURE 2. Composition (% volume + SE) of rumen samples collected in a low-density LD (n = 25) and a high-density HD
(n = 68) area of southern Québec during the growing seasons of 1997 and 1998.
crops for a large part of their summer diet. Comparison Fruits, mostly apples (90%), were a major compo-
of forage availability and consumption (Table 1) sug- __ nent of the fall diet in HD. Our results support the idea
gests that Red Maple, Choke Cherry, and Sugar Maple that fruits are important food items where and when
suffered high browsing pressure in HD. they are available (McCaffery et al. 1974; Short 1971;
2004
DAIGLE, CRETE, LESAGE, OUELLET, AND HUoT: SUMMER DIET OF DEER 365
| TABLE |. Most common food items (volume >1%) found in White-tailed Deer rumens from a low density LD (n=23) and a
high density HD area (n=63) of southern Québec during the growing seasons of 1997 and 1998.
Skinner and Telfer 1974). Apple trees and oak are
absent from forests in LD. We assumed that apples
found in one LD sample came from baits set by hunters.
Baiting was also common in HD, but we think that
apples ingested by deer in this region primarily origi-
nated from uncultivated apple trees growing in young
forests based on the fact that most specimens found
in rumens were smaller than commercial apples.
Mushrooms were a common food item in both study
areas. Like apples, but to a lesser extent, their shape and
size may have exaggerated their relative importance
on a volumetric basis. Their frequent occurrence in
rumens indicates that they represented a common food
item for White-tailed Deer. Mushrooms were consumed
mostly in spring in HD and in fall in LD, which may
be explained by different seasonal availability or by the
possibility that White-tailed Deer feed on them when
preferred foods are rare at both ends of the growing
season. Many studies reported large amounts of mush-
| % volume % occurence Availability (g/m)
| Food items Category LD HD LD HD LD HD
Leaves, stems, and grain
| Acer spicatum Leaf 26.9 0.6 30.4 4.8 19.0 <0.)
Fungi Mushroom 14.7 16.4 26.1 20.6 <0. 1 <0.)
| Botrychium sp. Forb a2, 0 4.3 0
| Clintonia borealis Forb 6.2 0.1 34.8 1.6 Dei 0.1
| Maianthemum canadense Forb 5.9 Ie) 47.8 15.9 el 0.2
| Sorbus americana Leat 4.4 0 26.1 0 <0.1
| Fraxinus nigra Leaf 4.0 0 4.3 0
| Epilobium angustifolium Forb 3.6 0 PAVE 0 0.8
Prunus virginiana Leaf 3.6 8.9 Paved 28.6 <0.1 <0.1
Prunus pennsylvanica Leaf pos) 0.9 26.1 4.8 <0.1
| Trillium sp. Forb PRS} 0.2 13.0 6.3 <0.1 <0.1
Aralia nudicaulis Forb 23 2.1 8.7 6.3 2.3 <0.1
» Acer rubrum Leaf 1.9 10.3 PSH 41.3 2.6 0.1
| Taraxacum officinale Forb 19 2D 13.0 Vas7) 0.9 0.2
Populus tremuloides Leaf od Ie 13.0 95 4.3 0.1
| Graminae Grass ites) 8.4 43.5 76.2 2.0
| Acer saccharum Leaf 13 6.6 13.0 14.3 1.6 <0.1
Taxus canadensis Leaf 1.3 <0.1 4.3 1.6
| Salix sp. Leaf Les 0.5 8.7 4.8 <0.1
| Solidago sp. Forb 0 1.2 0 4.8
| Fragaria sp. Forb 0 1.5 0 19.0 0.1
_ Lotus corniculatus Farm crop 0 1.6 0 1.6
| Prunus serotina Leaf 0 1) 0 Hilal 0.3
| Sonchus sp. Forb 0.2 1.9 4.3 322 <0.1
| Rubus sp. Leaf 0.7 23 8.7 27.0
| Potemogeton sp. Forb 0 3.0 0 32
| Malus pumila Leaf 0 32 0 6.3
| Zea mays Farm crop 0 3.6 0 7.9
Medicago sativa Farm crop 0 3.8 0 7.9
Trifolium sp. Farm crop 0.1 4.8 4.3 20.6
Fruits
Malus pumila Fruit 100 90.1 4.3 36.5 <0.1 <0.1
Quercus sp. Fruit 0 3.6 0 1.6
Fragaria sp. Farm crop 0 Sal 0 1.6
Crataegus sp. Fruit 0 22 0 6.3
rooms in White-tailed Deer diet (Crawford 1982; John-
son et al. 1995; Korschgen et al. 1980; McCaffery et
al. 1974), but nobody has yet considered the potential
impact of deer herbivory on mushrooms.
Diet quality - LD deer had access to a greater bio-
mass of preferred forage (Rouleau et al. 2002a) and
consumed more forbs and leaves of shrubs and trees
than HD deer, which compensated by ingesting farm
crops, grasses and fruits. Different forage intake result-
ed in a diet containing more cell solubles and lignin
in LD than in HD deer. Rumen contents did not differ
with respect to phenolics, which may have reflected
the complex nature of the chemical group (Robbins
1993: 253). Protein content followed a similar trend
as that for cell solubles, although the difference between
LD and HD was small and non-significant. Between
May and September, cell solubles were 8% greater in
LD than HD rumens. Cell solubles, which are composed
of sugars, protein, non-protein nitrogen, lipid, organic
366
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 2. Mean (SE; n) content (%) of cell solubles, lignin, phenolics, and nitrogen in White-tailed Deer rumen samples collected
in a high-density (HD) and a low-density (LD) study area of southern Québec during the growing seasons of 1997 and 1998.
May-June
HD LD
Cell solubles 32.4 40.7
(1.4; 21) (2.0; 14)
Lignin 222 23.3
(1.0; 21) (1.2; 14)
Phenolics 3i5) 3.6
(0.1; 16) (0.2; 13)
Nitrogen Te 7.0
(0.3; 16) (0.3; 13)
acid and soluble minerals (Iason and Van Wieren 1999),
are highly and rapidly digestible, whereas cell walls (1-
cell solubles) are only partly digestible and necessitate
some retention in the rumen for microbes to degrade
them (Iason and Van Wieren 1999). LD does benefit-
ed therefore from a richer diet than HD counterparts
during the end of gestation and peak lactation, a peri-
od with elevated energy demand in cervids (Mauget
et al. 1997). In late summer, the high consumption of
apples, which contain little fiber (Robbins 1993), can
explain the improved quality of rumen contents in HD.
The higher concentration of lignin in LD than in HD
rumens likely came from the greater consumption of
farm crops and grasses in the latter area, which have
a lower level of lignin than natural forages do (Rob-
bins et al. 1987).
The difference in forage quality likely reduced the
growth and condition of White-tailed Deer in HD,
where strong competition for forage has prevailed.
Deer density in HD increased by 10 fold since the late
1970s, whereas it remained relatively low and stable
in LD (Lesage et al. 2001). Deer had the same size in
both study areas before 1987 (Potvin 1989), but their
body mass progressively decreased in HD (Lesage et
al. 2001; Potvin 1994*). At the time of our study, the
eviscerated carcass mass of fully grown male deer aver-
aged 80 vs. 116 kg in HD and LD, respectively (Lesage
et al. 2001). Additional measurements throughout the
deer range in Québec revealed that deer size began to
decline when forage competition intensified in sum-
mer; 1.e., forage availability <10 000 kg/deer (Boucher
2004). Our results concur with the hypothesis that rural
deer living at high density cannot fully compensate for
the rarity of natural forage in woodlots during summer
by consuming cultivated plants (Rouleau et al 2002a).
All of these studies suggest that deer populations have
reached excessive densities in HD.
Acknowledgments
We thank R. Bélanger, J. Boisvert, B. Deschamps,
and M. Desrochers from Transports Québec, who kind-
ly gave us access to deer carcasses. J. Bachand, C.
Bélanger, M. Bélanger, N. Bergeron and E. Jeanson
helped in collecting the rumen samples. We are grateful
to G. Picard for conducting the chemical analysis, to
July-August September-October
HD LD HD LD
34.1 42.7 40.7 3919
(1.8; 11) (2.1; 4) @i5223) @a72)
21.9 23.4 17.8 24.0
(1.4; 11) (2.3; 4) (1.0; 23) (6322)
3.4 Bi) 2.4 Di
(0.2; 7) (0.3; 4) (0.1; 16) (0.4; 2)
6.8 6.5 6.9 7.0
(0.4; 7) (0.6; 4) (0.3; 16) (0.8; 2)
N. Desrosiers, and E. Normand for their assistance in
the laboratory, and to C. Roy for helping with plant
identification. G. Daigle, from the Service de consul-
tation statistique, Université Laval, did the statistical
analysis.
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Received 31 March 2003
Accepted 1 November 2004
Winter Habitat Use by Wolves, Canis lupus, in Relation to Forest
Harvesting in West-central Alberta
GERALD W. Kuzyk!, JEFF KNETEMAN?, and FIONA K. A. SCHMIEGELOW!
' Department of Renewable Resources, University of Alberta, Edmonton, Alberta, T9H 4N1 Canada
> Fish and Wildlife Division, Alberta Sustainable Resource Development, Hinton, Alberta, T7V 2E6 Canada
> Corresponding author: gkuzyk @ualberta.ca
Kuzyk, Gerald W., Jeff Kneteman, and Fiona K.A. Schmiegelow. 2004. Winter habitat use by Wolves, Canis lupus, in relation
to forest harvesting in west-central Alberta. Canadian Field-Naturalist 118(3): 368-375.
Forested landscapes in west-central Alberta are facing increased pressures from forest harvesting and other land-use
activities, which may alter the movements and distribution of Wolves and ungulates. Information on habitat use by Wolves in
logged forests is scarce, potentially limiting effective land-use planning in the boreal forest. Nine Wolves, from four Wolf
packs, were fitted with GPS radiocollars in the Rocky Mountain foothills, near Grande Cache, Alberta (2000-2001). We
found Wolves did not use the landscape randomly, but rather exhibited a significant preference for non-forested natural
habitats (shrubs, water), relative to their availability. Within forest habitats, Wolves used cutblocks proportionately more than
unharvested forest and non-forested anthropogenic habitats (pipelines, clearings); however, selection of forest cutblocks was
not statistically significant. We found no evidence that Wolves preferred or avoided forest cutblock edges. Wolf pack
territories contained various levels of timber harvesting, but most areas were still in the early stages of harvest. Nevertheless,
these areas have been allocated for large-scale harvesting. Understanding the potential responses of Wolves to rapidly
changing landscape mosaics poses a significant challenge to researchers and managers, but such information is important to
informing future land-management and conservation strategies for boreal forest Wolf-prey systems.
Key Words: Wolf, Canis lupus, Caribou, Rangifer tarandus, forestry, habitat, Moose, Alces alces, predation, Alberta.
Much of the world’s boreal forest is undergoing in-
creased demands from resource extraction industries,
where related activities such as forest harvesting may
alter habitat use by large carnivores (McLellan and
Hovey 2001; White et al. 2001). Wolves (Canis lupus)
are a common predator of ungulates in Canada’s for-
ests, yet there are few data on how their use of habitat
might be affected by forest harvesting (Jedrzejewska
et al. 1994; Kohira and Rexstad 1997; Kunkel and
Pletscher 2000). Logging of forests can change the spa-
tial dynamics of Wolves and their prey, resulting in
conflict between resource development and wildlife
management (Hervieux et al. 1996). For example, in
Alberta, Woodland Caribou (Rangifer tarandus caribou)
are classed as a threatened species (Edmonds 1998),
and Wolf predation is considered a primary reason for
their decline (Edmonds 1988; McLoughlin et al. 2003).
It is therefore important to understand how Wolves
respond to forest harvesting, as habitat use by Wolves
may change in response to logging activities, and could
affect predation risk to Caribou and other ungulates.
Forest harvesting can cause habitat fragmentation
and alter predator-prey systems. Predators may follow
habitat edges due to ease of travel (Bider 1968). As
well, when patch size decreases, predator numbers may
increase due to increased prey density and diversity
(Gates and Gysel 1978; Yahner 1988). For example,
Red Fox (Vulpes vulpes) and Coyote (Canis latrans)
densities can increase with more landscape fragmenta-
tion, and habitat edges are favored for hunting (Oehler
and Litvaitis 1996).
In a Wolf-prey system in Canada’s boreal forest,
forestry activities have the potential to alter the preda-
tion risk to ungulates from Wolves in three ways. First,
differential spatial and temporal habitat selection sep-
arates Woodland Caribou and Moose (Alces alces)
distribution, reducing the risk of predation to Caribou
from Wolves (Bergerud and Elliot 1986). Caribou sel-
ection for higher elevations reduces the chance of en-
counter by Wolves hunting Moose, a primary prey spe-
cies, in lower elevations riparian areas (Seip 1992). If
the spatial separation of Caribou and Moose is altered
by logging roads and forest cutblocks, it has been ar-
gued that Wolves will have increased access to, and
greater encounter rates with Caribou, resulting in a Cari-
bou decline (Bergerud 1988; Seip 1992). In northeast
Alberta, linear developments (roads, seismic lines,
trails) were found to affect the spatial separation be-
tween Caribou and Moose, where linear corridors en-
hanced Wolf travel efficiency (James 1999) and Cari-
bou mortalities caused by Wolves were found closer
to linear corridors than expected by chance (James
and Stuart-Smith 2000).
Second, Caribou select for older forests (Szkorupa
2002) and distribute at low densities (Bergerud 1988).
Caribou spatial overlap with Wolves is reduced and,
correspondingly, so too is the risk of detection and pre-
dation. Reducing the amount and patch size of older
forest by timber harvest may temporarily increase
Caribou densities (Bergerud 1988), and Moose, deer
(Odocoileus spp.) and Elk (Cervus elaphus) may use
these remaining patches for cover. Higher densities of
368
2004
Caribou in more constricted areas, and wider distribu-
tion of Wolves in response to primary prey distribution,
may increase the chances of Caribou being detected
by Wolves.
Third, Moose, Elk and deer are attracted to recently
logged areas that support high quality regenerating
forage (Peek et al. 1976; Tomm et al. 1981; Stelfox et
al. 2001). This represents a concentrated prey base for
Wolves, which may influence how Wolves use land-
scapes. If Wolves frequent forest cutblocks searching
for Moose, Elk and deer, and if cutblocks occur near
preferred Caribou habitats, this may increase predation
risk to Caribou. All three outcomes potentially affect-
ing Caribou depend on information about Wolf behav-
ior and use of changing landscapes.
Forest harvesting in west-central Alberta was large-
ly initiated in the late 1960s and has accelerated in
recent years. Energy sector activities (oil and gas ex-
ploration and development) are also altering these
landscapes, resulting in cumulative land use impacts
(Hervieux et al. 1996). For decisions concerning long
term wildlife conservation, resource managers and
land-use planners require new information about how
Wolves use habitat in logged forests and under chang-
ing landscape conditions.
ALBERTA
Study area
shown indetai
400 Kilomaers
7
gs Wolf locations (GPS)
© Wolf pack territory
». Town of Grande Cache
— Major Rivers
Zones
Data Source: Alberta Environment Natural Resources,
Govemment of Canada 2000; DEM published with permission of
Alberta Sustainable Resource Development. Natural Resource
Canada and the Spatial Data Warehouse. Weyerhaeuser Company.
KUZYK, KNETEMAN, and SCHMIEGELOW: HABITAT USE BY WOLVES
369
We used Global Positioning Systems (GPS) radio-
collar technology to examine winter habitat use of
Wolves in west-central Alberta. We chose to examine
fine-scale Wolf movements that correspond with John-
son’s (1980) third order habitat selection: movements
of animals within their home range. We examined two
questions. First, do Wolves use forest cutblocks prefer-
entially over other habitat types? Second, do Wolves
prefer cutblock edges? We predicted that Wolves would
prefer forest cutblocks over other habitats, due to the
expected increase in ungulate densities in regenerating
forests. We also predicted Wolves would prefer forest
cutblock edges relative to areas farther away from them,
due to ungulate use of cutblock edges for feeding and
proximity to cover (Stelfox et al. 2001*).
Study Area
The study area is approximately 5000 square kilo-
meters, located in the foothills of west-central Alberta,
near the town of Grande Cache (54°N 119'W) (Fig-
ure 1). The area is classed into subalpine and boreal
natural subregions (Beckingham and Archibald 1996),
and contains several main rivers and a dendritic pat-
tern of creeks; lakes are scarce. Elevations range from
1300-1800 meters, and the climate is subarctic, with
Map compied by S. Shirkoffand G. Kuzyk. Unwersty of Alberta
FiGure 1. Distribution of four Wolf packs monitored in winters of 2000 and 2001 in west-central Alberta.
370
short wet summers and long cold winters. Temperatures
average 16°C in July and -13.5°C in December (Beck-
ingham and Archibald 1996). The forests are primarily
Lodgepole Pine (Pinus contorta) and some White
Spruce (Picea glauca). The wetland complexes support
mostly Black Spruce (Picea mariana) and some Tam-
arack (Larix laricina). Some south facing slopes sup-
port Trembling Aspen (Populus tremuloides) and wil-
low (Salix spp.).
This area supports a high diversity of large mam-
mals: Woodland Caribou, Moose, Elk, Mule Deer
(Odocoileus hemionus), White-tailed Deer (Odocoileus
virginianus), Bighorn Sheep (Ovis canadensis), Moun-
tain Goats (Oreamnos americanus) and Wild Horses
(Equus cabalus). Wolves, Coyotes (Canis latrans),
Grizzly Bears (Ursus arctos), Black Bears (Ursus
americanus) and Cougars (Felis concolor) also exist
throughout the study area.
Major land use activities include forest harvesting,
oil and gas exploration and development, coal mining,
commercial trapping, and public uses such as hunting,
fishing, hiking, horse packing and camping. Access
is primarily on roads created for resource extraction,
pipelines and seismic lines. Further descriptions of
the study area can be found in Edmonds (1988) and
Smith et al. (2000).
Wolf Location Data
Nine Wolves in four packs were captured and fitted
with GPS radiocollars in winters of 2000 and 2001
(Table 1). Three packs were located in areas with a
migratory mountain Caribou population and one pack
with a sedentary boreal Caribou population. All Wolf
handling was approved by the Faculty of Agriculture,
Forestry and Home Economics Animal Care Policy
(Number 96-99D), subject to the protocols of the
Canadian Council of Animal Welfare. Wolf captures
were accomplished by helicopter darting (Ballard et al.
1991) or netgunning, then physically restraining the
Wolf with restraining forks, and hand-injecting 1-2 mls
of telazol at 200 mg/ml (Kuzyk 2002a). Wolves were
fitted with store aboard GPS radiocollars (Lotek En-
gineering Sytems, Newmarket, Ontario). In the winter
of 2001, the Prairie Creek and Cutbank packs each had
two members with GPS radiocollars. To avoid pseudo-
THE CANADIAN FIELD-NATURALIST
Vol. 118
replication (Hurlburt 1984), location data and asso-
ciated patterns of habitat use from these individuals
were averaged for their respective packs (Table 1).
As this study was designed to understand Wolf hab-
itat use in winter, the following criteria were used to
select Wolf location data:
(1) Location data from 31 January to 25 April 25 in 2000
and 2001 were used for analyses. These dates were used for
two reasons: first, most Caribou in the study area (the migra-
tory mountain ecotype) leave the forested foothills in late
winter and spring to calve in the nearby mountains (Edmonds
1988); second, a spring cutoff time also has ecological rele-
vance to Wolves. In spring near whelping time, Wolves are
thought to change their hunting patterns by switching from
hunting as a pack and preying on ungulates, to hunting
alone or in small units in search of smaller prey, with their
activities centering on the den and pups (Mech 1970). There-
fore a single GPS collared Wolf would no longer represent
the behavior of their pack, and would not meet our design
criteria.
(2) To provide consistency in GPS collar programming,
six-hour locations were chosen (4 per day) as the minimum
common sampling unit for analysis. Wolves are sporadic in
their movements, and may travel at rates of about 8 km/hr
while hunting (Mech 1966), or relatively short distances when
near a killsite (Kuzyk 2002a). When near a killsite, they sel-
dom rest in one location for periods longer than six hours
(Mech 1970).
(3) Wolf locations outside calculated pack territories were
not used. These Wolves were assumed to be dispersing from
their natal territory and thus behaving differently from their
pack (Gese and Mech 1991).
Data were differentially corrected using N4Win
Version 2.40 program (Lotek Engineering Inc. 2000)
and were assumed accurate within 14 meters, 95% of
the time (Lotek Engineering Inc. 2000). Wolf locations
with Dilution of Precision (DOP) values greater than
15 were removed from the analysis (<2 % of total loca-
tions). High DOP values and radiocollar malfunctions
made for unequal locations per Wolf pack (range 152
to 279) over the duration of this study (Table 1).
Habitat Classification and GIS Methods
Wolf location data were imported into ArcView
Version 3.1 (Environmental Systems Research Insti-
tute Inc., Redlands, California). Current, digital forest
inventory coverages were obtained from Weyerhauser
Canada Limited, Canadian Forest-Products and Al-
TABLE |. Wolf packs with associated number of GPS locations and area of habitat use (territory size) in west-central Alberta
in winters of 2000 and 2001.
Wolf Pack Wolf Year Dates Number of Locations Area (km?)
Cutbank W5 2000 24 January — 16 March 185 714
Prairie Creek W9 2000 28 January — 25 April 252 286
Simonette W13 2000 31 January — 25 April 279 786
*Prairie Creek W5 and W9 2001 18 February — 25 April 231 182
*Cutbank W19andW21 = 2001 15 February — 25 April 258 448
Lynx Creek W22 2001 15 February — 25 April 247 1848
Simonette W30 2001 17 February — 4 April 152 398
* Locations were averaged for two collared Wolves which belonged to the same pack.
2004
KUZYK, KNETEMAN, and SCHMIEGELOW: HABITAT USE BY WOLVES
37]
TABLE 2. Description of habitat categories used in compositional analysis for Wolf packs in west-central Alberta during late
winters of 2000 and 2001.
Habitat 2
Unharvested forest
all harvestable forest
burn
Habitat |
Forest cutblocks
all harvested forest
Habitat 3 Habitat 4
Non-forest (natural) Non-forest (anthropogenic)
herbaceous grassland clearing
sand, flooded land right-of-way
closed and open shrub industrial infrastructure
coniferous scrub pipelines
deciduous scrub
brush, windfall
open and treed muskeg
water
geophysical
perennial forest crops*
*Perennial forest crops are denoted as anthropogenic by the forest companies and account for < 0.6km?* of one Wolf pack’s
territory. (Simonette pack — total territory size is 786 km7).
TABLE 3. The percentage of use (GPS locations) and availability (area in km?) of five habitat categories for Wolf pack
territories in west-central Alberta during late winters of 2000 and 2001.
Cutblock Forest Non-forest* Non-forest* Non-forest
Shrubs Water Anthropogenic
Wolf Pack Year Used_1 Avail_1 Used_2 Avail_2 Used_3 Avail_3 Used_4 Avail_4 Used_5 Avail_5
Cutbank 2000 34.1 28.9 57.8 64.6 7.0 A: 1.1 0.3 0.0 0.8
Prairie Creek 2000 Lieve Aes) 77.8 80.2 6.7 4.8 LED, 1.0 2.4 Hes)
Simonette 2000 PN SYS) 61.6 78.8 Gs 3.0 DES 0.6 TD 1.8
Prairie Creek 2001 6.3 5.9 81.2 87.1 9.1 4.1 fe 1.1 M7 1.8
Cutbank 2001 Asay SD) 35/9 60.0 20.2 3.4 0.4 0.3 0.4 0.8
Lynx Creek 2001 0.8 5.4 1S} 85.9 202 8.5 0.8 0.1 0.8 0.2
Simonette 2001 16:4: - 1420 68.4 78.3 113) 5) 0.7 0.5 1.3 Le,
Total Mean 19.1 16.9 65.7 76.4 1220 5.0 le, 0.6 2.0 1D,
SE S27, 4.3 6.0 3.9 23, 0.7 0.3 0.1 0.9 0.2
*Non-forest natural is subdivided into shrub and water categories for descriptive purposes only.
berta Government Phase 3. The minimum mapping
unit for these coverages was | ha for forest polygons.
However, the resolution of line features, such as roads,
was much greater, as these were spatially referenced
from high-resolution remotely sensed data (~5 m res-
olution), or from GPS readings taken in the field. Thus,
the resolution of our animal location data was com-
mensurate with the resolution of the landscape cover-
ages used, for purposes of evaluating coarse-scale habi-
tat use. Minimum convex polygons (MCPs) of Wolf
territories were initially calculated with an animal
movement extension in ArcView (Hooge and Eichen-
laub 1997). MCPs were considered an appropriate
method for delineating general territory boundaries
in order to evaluate coarse-scale habitat use. Due to a
small portion of the GIS coverages missing within each
Wolf pack territory, territory sizes for subsequent
analyses were adjusted by summing all the areas within
the MCPs for which we had GIS coverages (Table 1).
As Wolves live in a defined territory (Mech 1970),
each territory was classified into four habitat categories
to reflect coarse scale patterns of use. These categories
were: (1) forest cutblocks, (2) unharvested forest, (3)
non-forest natural (shrubs and water) and (4) non-
forest anthropogenic (pipelines, wellsites) (Table 2).
The area of non-forest natural was divided into “shrub”
and “water” classes for descriptive purposes (Table
3), but the data were pooled for analysis. As the focus
of this study was to determine habitat use of Wolves
in managed landscapes, a further analysis was con-
ducted to determine Wolf use of forest cutblock edges.
Forest cutblocks were buffered using specified dis-
tances starting from the edge of the forest-cutblock and
proceeding into the forest. We did not use locations
inside cutblocks in this analysis. Buffer distances were
consistent with those studying Caribou avoidance of
linear features (Dyer et al. 2001; Oberg 2001), starting
from the edge of the cutblock to 100 m, 101-250 m,
251-500 m, 501-1000 m and >1000 m. The category
of >1000 m was also chosen as the farthest distance
for comparison to Smith et al. (2000), who found that
Caribou in west-central Alberta may avoid cutblocks
by about 1200 m.
Statistical Analysis
Compositional analysis (Aebischer et al. 1993) was
conducted by integrating Wolf GPS location data and
forest inventory data within a GIS (ArcView 3.1) to
B72
determine if there was a preference in Wolf use of habi-
tat or buffer categories. Aebischer et al. (1993) suggest
a minimum of six radiotagged animals are required to
perform compositional analysis, and replication across
years is acceptable. Therefore, our sample of seven
Wolves over two winters was adequate for this test.
Compositional analysis compares the amount of “used
habitat” to the amount of “available habitat” and tests
whether habitats are preferred or avoided more than
expected by random (Johnson 1980). The number of
Wolf locations in each habitat or buffer category rep-
resented used habitat. The available habitat was the
total area of each habitat or buffer category (Table 3).
If there was no use of a habitat category, 0% use was
replaced with 0.001%, as this represented a value lower
than the smallest recorded nonzero percentage (Aebis-
cher et al. 1993).
A chi-square test was used to determine if Wolf use
of habitat or buffer categories was significantly non-
random, then each habitat category was ranked in terms
of its use. To determine if any habitats were selected
over others, a difference for each pair-wise comparison
was calculated using log ratios. This compared each
habitat category within each Wolf pack territory. The
means and standard errors for each comparison were
calculated across all Wolf packs, and the pair-wise
differences were tested for significance using a t-test
(Aebischer et al. 1993). Alpha level for all tests was
set at 0.05.
Results
Wolf Habitat Use
Territory size for the four Wolf packs ranged from
182 — 1848 km? (Table 1). The availability of each of
the four habitat categories varied markedly: the per-
centage of forest averaged 76.40% (SE 3.90) for all
packs, and thus was the most dominant habitat, where-
as non-forest anthropogenic cover averaged only 1.23%
(SE 0.25) of available habitat across Wolf territories
(Table 3). Wolves showed a significant deviation from
random use of the four habitat types (v7 = 7.815, df = 3,
p = 0.036) selecting non-forest natural (shrubs-water)
habitats over both forest (t = -4.281, df = 6, p = 0.005)
and cutblocks (t = -2.92, df = 6, p = 0.027), in relation
to their availability (Table 4). No other pair-wise com-
parisons were significant. However, when ranked in
preference by habitat type, forest cutblocks were pref-
THE CANADIAN FIELD-NATURALIST
Vol. 118
erred more than both forest and non-forest anthropo-
genic areas.
Wolf Response to Forest Cutblock Edges
The available areas for all distance buffers less than
1000 m were similar, with variation due mostly to
dissolving buffers for adjacent cutblocks. Wolf use of
distance buffers did not deviate significantly from ran-
dom (x7 = 2.349, df = 3, p = 0.503). When buffer dis-
tances were compared using compositional analysis,
no significant difference was found between distance
categories related to forest cutblock edges. When
ranked, the 501-1000 m buffer distance was the most
preferred, followed by the 0-100m buffer, with the
least preferred being the buffer >1000 m.
Discussion
Wolves have been described as habitat generalists
(Mech 1970; Mladenoff et al. 1995). On a coarse spa-
tial scale, Wolves inhabit large tracts of forest (Mech
1995) and may prefer mixed wood forests over either
homogenous coniferous or deciduous forests (Mladen-
off et al. 1995; Krizan 1997). Wolves may use forests
altered by logging, as these areas provide good deer
habitat, and thus support an important prey base for
Wolves (Mladenoff and Sickley 1998). In this study,
GPS radiocollar technology allowed for a more re-
fined examination of Wolf habitat preferences, show-
ing Wolves in our study area do not use the landscape
randomly. In general, Wolves preferred habitats with
young vegetation, in both non-forest natural habitats
and forest cutblocks. This is consistent with increased
ungulate abundance in areas of young vegetation (Peek
et al. 1976; Stelfox et al. 2001*), which attract Wolves
(Bergerud 1988). However, increased road access into
these areas may also allow humans to alter activity
patterns of Wolves (Theuerkauf et al. 2003), or affect
Wolf numbers by direct or indirect killing (Mech
1995, Mladenoff and Sickley 1998). In this study, the
least used habitat by Wolves was non-forest anthro-
pogenic (pipelines, right-of-ways), possibly to avoid
human contact. Two radio-collared Wolves were known
to have been shot during this study, and several other
collars were lost to unknown factors (Kuzyk 2002a).
We found little support for our first prediction that
Wolves select forest cutblocks. Wolves did use cut-
blocks proportionately more than their availability and
were ranked above forest or anthropogenic features,
TABLE 4. Results from compositional analysis (p values in parenthesis; + denotes row > column and — column > row) for
comparing four habitat categories for four Wolf packs in west-central Alberta during late winters of 2000 and 2001.
1 2)
Cutblock Forest
1 Cutblock +(0.947)
2 Forest -
3 Non-for_natural + +
4 Non-for_anthro. - -
* denotes significance at (p<0.05).
3 4
Non-for_natural Non-for_anthropogenic
-(0.027) * +(0.902)
-(0.005) * +(0.903)
+(0.177)
— 2004
| but differences were not significant. Similarly, Wolves
_ in Ontario were found to use cutblocks in proportion
to their occurrence (Krizan 1997). We had the advan-
tage of GPS radiocollars which allowed for a large
collection of location data, compared with the traditi-
onal VHE collars used by Krizan (1997). However, we
acknowledge that our analyses still lacked statistical
power, due to the relatively small sample of Wolves
radiocollared.
The amount of harvested forest differed substan-
| tially between Wolf packs and may have accounted
|
for variation in Wolf use of forest cutblocks. The Lynx
Creek pack had only 5% of its territory as forest cut-
blocks, whereas 36% of the Cutbank pack’s territory
consisted of recent cutblocks. This seven-fold differ-
ence in the amount of harvested forest between packs
may have influenced habitat preferences. Kohira and
Rexstad (1997) found no evidence that Wolf diets
differed between logged and unlogged areas in the
coastal rainforests of Alaska. About 6% of that total
study area was logged, with the amount of area logged
ranging from 1-26% between Wolf pack territories.
This differs from our study area, where about 17%,
or approximately three times as much area has been
logged. In southeast British Columbia, researchers also
did not find evidence that forest harvesting increased
the vulnerability of Moose to predation by Wolves,
where about 13% of the area was logged (Kunkel and
Pletscher 2000).
Wolves in our study did show a significant prefer-
ence for non-forested natural habitats (shrubs/water)
over cutblocks and forest, which might be explained
by a number of selection criteria. Wolves prefer to
rest in open areas, and may travel several kilometers
to reach such preferred sites (Mech 1970). Wolves in
this study area were observed on numerous occasions
resting in open meadows, muskegs, hillsides and beav-
er ponds, often when they were near killsites (Kuzyk
2002a). The shrubs in these habitats have open crowns,
which allows both penetration of sunlight and structure
for protection from the wind, thus providing Wolves
cover while resting.
The shrubs in this non-forest habitat type also pro-
vide forage and cover for ungulates. During this study,
Wolves made deer kills in shrubby willow areas, and
Moose, deer and Elk kills in or near riparian areas
(Kuzyk 2002a). Elk are primarily grazers, and may be
attracted to these shrub patches due to the increased
availability of grasses. Bjorge and Gunson (1989), in a
nearby Wolf study, noted that Elk, especially Elk calves,
were a preferred prey for Wolves in winter. During the
limited kill rate work associated with this study (Kuz-
yk 2002a), only one cow Elk kill was documented. In
Jasper National Park, Wolves hunt deer while mov-
ing to pockets of Elk (Carbyn 1974; Weaver 1994). It
is possible that shrubby areas do represent reliable
patches of prey, and the Wolves investigate them for
prey regularly.
KUZYK, KNETEMAN, and SCHMIEGELOW: HABITAT USE BY WOLVES
373,
Water was also included in this preferred habitat
class. It is common for Wolves to use frozen waterways
as travel routes where snow is most compacted and
ice makes travel easy. In winter Wolves probably use
creeks and rivers to travel among ungulate winter
ranges. Also there is an increased chance of encounter-
ing Moose that use riparian areas in winter (Hayes et
al. 2000) and Wolves are known to frequently kill
ungulates on iced surfaces (Mech 1991).
Our second prediction of Wolf preference for for-
est cutblock edges was also not supported. There was
no significant difference in Wolf preference for any
buffer distance categories, nor was the 0-100 m buffer
class ranked highest. Habitat was not controlled for
in the buffer categories, which may have confounded
the analysis. The behaviors of Wolves, such as feeding
at killsites, resting and hunting may also be diluting
the effect of any preference or avoidance of cutblock
edges. Wolves hunt a diversity of prey, and chase dis-
tance varies with each prey type (Paquet 1989). For
example, the average chase distance for a Moose is
883 m (Paquet 1989). Depending on where Wolves lo-
cate them, Moose could choose to run to the nearest
forest to avoid attacking Wolves (Stephens and Peter-
son 1984), or remain stationary and aggressive (Mech
1966), or stationary and non-aggressive (Kuzyk 2002b),
and still avoid attack by Wolves. These results, and
those related to broader habitat selection questions,
suggest that consideration of behaviors associated with
different habitat types is an important component of
interpretation in Wolf habitat use studies.
Forest harvesting alters both the amount and spatial
distribution of habitat types. We measured habitat use
by Wolves directly, and found that Wolf use of land-
scapes was not random. We suggest that patterns of
habitat use may be influenced by the relative avail-
ability of different habitat types, specifically natural
shrubs and waterways, and to a lesser degree, by re-
cent forest cutblocks. Nevertheless, our results clearly
show that consideration of shrub/waterway habitats is
an important criterion for land-use decisions regard-
ing Wolves. In our study area, Caribou prefer forests
greater than 80 years old, especially those stands aged
120-160 years (Szkorupa 2002), and have been found
to avoid forest cutblocks by 1200 m (Smith et al.
2000). As most of the winter range of these Caribou
has been allocated for timber extraction, areas of older
forest will become increasingly small and isolated. If
the forest continues to be harvested at present rates,
all Wolf packs we studied will have a substantial
amount of logged area within their territories within
a relatively short time. As Moose, deer and Elk are
the primary prey of Wolves in this study area, informa-
tion is required on how these ungulates are respond-
ing to the changing landscape mosaic, as this may
ultimately determine how Wolves use the landscape.
Understanding the dynamic relationship between pred-
ator and prey in a system undergoing rapid change
374
poses an enormous challenge. Future research on Wolf
habitat use should concentrate on increasing sample
sizes, refining habitat classifications, and linking be-
havior with patterns of habitat use.
Acknowledgments
Funding for this research was provided by the West-
Central Alberta Caribou Standing Committee, the Al-
berta Sport, Recreation, Parks and Wildlife Foundation,
and a University of Alberta Challenge Grant in Bio-
diversity (supported by the Alberta Conservation Asso-
ciation). A University of Alberta Graduate Research
Assistantship and Margaret Brown Award in Environ-
mental Studies and Wildlife Resources also provided
financial assistance to G. Kuzyk. Additional financial
support and digital forest inventory data were kindly
provided by Weyerhaeuser Canada Ltd. and Cana-
dian Forest Products. S. Shirkoff provided GIS sup-
port. We are thankful for the safe and expert piloting
conducted by C. Wilson from Bighorn Helicopters
and D. Dennison from Coyote Air during wolf cap-
tures and monitoring. K. Smith and R. Hayes kindly
reviewed the manuscript and added helpful suggestions.
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Received 4 April 2003
Accepted 23 November 2004
Bird Communities of the Garry Oak Habitat in Southwestern British
Columbia
WAYNE R. ERICKSON
Forest Practices Branch, British Columbia Ministry of Forests, P.O. Box 9513, Stn Prov Govt, Victoria, British Columbia
V8W 9C2 Canada
Erickson, Wayne R. 2004. Bird communities of the Garry Oak habitat in southwestern British Columbia. Canadian Field-
Naturalist 118(3): 376-385.
Identifying the bird communities of a habitat could contribute to conservation efforts and provide benchmarks for ecosystem
studies. Garry Oak (Quercus garryana) ecosystems in British Columbia are among the most endangered in Canada and
warrant conservation. Four bird communities were determined by analyzing an extensive sample of Garry Oak habitat bird
data. These communities were defined objectively by aggregations of the bird species themselves from across the various
sites and areas. Characteristic species of these communities include American Goldfinch (Carduelis tristis), Spotted Towhee
(Pipilo maculatus), Bewick’s Wren (Thryomanes bewickii), Rufous Hummingbird (Selasphorus rufus) and Chestnut-backed
Chickadee (Poecile rufescens) in community 1; House Wren (Troglodytes aedon), Olive-sided Flycatcher (Contopus cooper),
Purple Finch (Carpodacus purpureus), White-crowned Sparrow (Zonotrichia leucophrys), and Pine Siskin (Carduelis pinus)
in community 2; Western Tanager (Piranga ludoviciana), Yellow-rumped Warbler (Dendroica coronata), American Goldfinch,
Pine Siskin, Pacific-slope Flycatcher (Empidonax difficilis), Cassin’s Vireo (Vireo cassinii) and Chipping Sparrow (Spizella
passerina) in community 3; and Northwestern Crow (Corvus caurinus) and European Starling (Sturnus vulgaris) in commu-
nity 4. Differences between the communities are suggested from the life history traits of the species, including a community
consisting mostly of insectivores when on breeding territory (number 1), one with species foraging primarily in shrubs and
trees (community 3), and another with tree-nesting ground gleaners (number 4). One community (number 3) had analogues
in two widely disparate areas: oak-associated in north-central New Mexico, and aspen (Populus tremuloides)-related in
northcentral British Columbia; otherwise communities reported in the literature were generally not directly comparable.
Key Words: bird communities, Garry Oak, Quercus garryana, multivariate classification, British Columbia.
Garry Oak, Quercus garryana habitat is unique
within Canada, and related biogeographically to Cal-
ifornia (Erickson 1996). Garry Oak ecosystems are at
their northern margin in British Columbia, and are
among the most endangered ecosystems in Canada
(Erickson 1993*, 2000a). Native stands have been
reduced by urban development and are threatened
with invasion by alien species. Bird communities of
Garry Oak habitat in the Pacific Northwest have not
yet been fully investigated. Defining these communi-
ties is a basic step toward conservation, and a requisite
to identifying critical habitat requirements. Predictive
abilities and assessments for preservation and man-
agement of the Garry Oak habitat could be strength-
ened by further understanding these communities.
Garry Oak occurs in an area of southwestern British
Columbia with a distinctive modified mediterranean
climate in the strong rain-shadow of the Olympic and
Vancouver Island mountains. Mild, wet winters, vari-
able precipitation and regular summer drought are typ-
ical. The result on the landscape is a mosaic of park-
lands with spring forb meadows and oak clumps; mossy
bluffs often with shrub oaks; open grassy savannahs;
and woodlands sometimes mixed with Douglas-fir
(Pseudotsuga menziesii). As well as being diverse and
productive for plant growth, this landscape is attractive
for human habitation and agricultural development.
The consequence has been habitat loss and endanger-
ment for Garry Oak ecosystems. There is a scientific
and conservation interest in knowing more about the
elements of these ecosystems, including their bird
communities. Garry Oak habitat has been selected
as a focus of Partners in Flight for its importance to
migrating and wintering birds in the Pacific Northwest
(de Groot et al. 2000). Their work includes restoration
of habitat within the British Columbia range of Garry
Oak (Figure1).
The purpose of this paper is to identify the bird com-
munities of Garry Oak habitat, make comparisons of
the life history traits of constituent species, and com-
pare these communities with the literature on other
habitats.
Methods
I used Detrended Correspondance Analysis (DCA,
PCORD 3.0, McCune and Mefford 1997*) (Hill and
Gauch 1980; Peet et al. 1988); interpretive graphing;
and a quantitative similarity index (Motyka’s modifi-
cation of the Sorenson index, Brower et al. 1990): to
determine bird communities.
I took records of bird species occurrence by ear and
by sight while sampling representative ecological plots
over 120 Garry Oak areas (Figure 2). This was part of
an ecological reconnaissance in 1993 and 1994, cov-
376
2004
in British Columbia
| Ficure 1. Garry Oak range in British Columbia. This map is
courtesy of British Columbia Ministry of Water, Land
and Air Protection, December 2003.
ering an area bounded by East Sooke, Gonzales Hill
and Courtenay on Vancouver Island; and East Point,
Saturna Island, and Helliwell Point, Hornby Island
on the Gulf Islands (Erickson 1996). These locations
are between approximately 48°N, 123°W and 49°30'N,
125°W. The Garry Oak stands sampled were primarily
mature, but their canopy varied from shrub-like with
exposure, to large and open on deep soils. Elevations
ranged from sea level to about 550 m. Plots were
approximately 200 m?, consisted of relatively uniform
vegetation and topography, and varied in size accord-
ing to plant community boundaries. Species presence
was recorded in an observation effort of approximately
90 minutes per plot. A total of 1243 records were taken
ERICKSON: BIRD COMMUNITIES OF GARRY OAK HABITAT
SEH
on 286 plots (Erickson 2000b). Sampling was primarily
in spring, during May and June. This time interval has
migratory bird influx, spring vegetation growth, territory
establishment, nesting, summer plant growth cessation
and bird dispersal.
The data set had been previously checked with spe-
cies accumulation curves (McCune and Mefford 1997;
Erickson 2000b, unpublished data; Smith et al. 2002)
to determine the adequacy of the sample. Occurrence
by plot of all species with a frequency 5% for each
year was entered into a data set; 23 species in 1993, and
29 species in 1994. This qualifying criterion reduced
the number of plots to 135 in 1993 and 127 in 1994, for
a total of 262 in the analysis. The DCA method uses
chi-squared distances to simultaneously ordinate, in this
case, bird species data against plots, and vice-versa.
Axis solutions account for, and therefore represent the
most variation in the data set. Bird species are sepa-
rated and referenced by their scores relative to the de-
trended and re-scaled axes. Graphing the axis combi-
nations provides a view of the reference coordinates
in multivariate space. DCA is among the most widely
used analytical methods in ecology (Peet et al. 1988).
It has been applied in bird community work in oak
woodland and other settings (Huff and Raley 1991;
Pojar 1995; Garcia et al. 1998; Abernethy et al. 2001*;
Parody et al. 2001).
In the interpretive graphing method I framed pro-
portional circles on Axis | vs. 2, and Axis 1 vs. 3, on
the DCA output graphs in order to outline potential
bird groups. The circles represent four potential bird
groups for each year’s data, a number which was deter-
mined from species accumulation curve results. These
Helliwell Point
Sea
) Nanaimo
Vancouver Island $
So
[Sime eames |
re; <1 UU ¢ =
5 oe. | S
eS oe
Cone E
: : Se
Georgia Strait Ne
Tee
xX Sea
2e
NS SS x ;
SS East Point
se =
Gonzales Hill
+etoria
Notes: 1 to 10 plots per circle. Note lateral map distortion
\ East Sooke
Sse
RS ES]
FiGure 2. Garry Oak bird community sampling on Vancouver Island, British Columbia.
378
TABLE |. Characteristic species classification.
Species classification Symbol and similarity value
d (10)
c (7)
n (3)
Distinct
Companion
Non differential
results indicated that groups of approximately 35 plots
could potentially cover >60% of the total species. The
circles were centred on the graph coordinates from
the median of the top-ranking species. Species rank
was judged from the scores against each axis and the
dominant axis combination (1 and 2) in the DCA result
(Table 1, 2). These groups quantitatively represent the
co-occurrence of species in different plots from the
data, and they served as the first stage in identifying
bird communities. Species were classified according to
their distinctness to a group from the graphs and numer-
ic values assigned (Table 1). Quantitative similarity
index comparisons were then completed and the groups
aggregated into communities based on the results.
Results
Species scores against the DCA axes are shown in
Tables 2, 3 and 4. Four bird communities of Garry
Oak habitat were identified by the analysis (Figures
3-6). Combinations of characteristic species, includ-
ing most of the twenty top-ranking species in overall
frequency, helped define the communities (Table 5).
Characteristic species included American Goldfinch
(Carduelis tristis), Spotted! Towhee (Pipilo macula-
tus), Bewick’s Wren (Thryomanes bewickii), Rufous
Hummingbird (Selasphorus rufus) and Chestnut-backed
Chickadee (Poecile rufescens) (community 1); House
Wren (Zroglodytes aedon), Olive-sided Flycatcher (Con-
topus cooperi), Purple Finch (Carpodacus purpureus),
White-crowned Sparrow (Zonotrichia leucophrys), and
Pine Siskin (Carduelis pinus) (community 2); West-
ern Tanager (Piranga ludoviciana), Yellow-rumped
Warbler (Dendroica coronata), American Goldfinch,
Pine Siskin, Pacific-coast Flycatcher (Empidonax dif-
ficilis), Cassin’s' Vireo (Vireo cassinii) and Chipping
Sparrow (Spizella passerine) (community 3- 1993 only);
and Northwestern Crow (Corvus caurinus) and Euro-
pean Starling (Sturnus vulgaris) (community 4- 1994
only).
Three groups had resulted in each of the two years,
which were then reduced to the four communities.
Two of these occurred across the years and two were
unique to a single year. Communities were defined by
the combination of their characteristic species. Simi-
larity index values were quite low for the two across-
year communities: 0.36 for community | and 0.43 for
community 2. The two within-year communities had
no similarity to each other (0 index value).
THE CANADIAN FIELD-NATURALIST
Vol. 118
Association with a group on both axis combinations
unique to a group on both axis combinations
unique to the group on one axis combination
distinct on one axis combination
TABLE 2. Garry Oak bird species in 1993 with the highest
scores against DCA axes, with median species designated*.
Species Score
Axis |:
Northwestern Crow 522
Song Sparrow 499
California Quail* 388
Spotted Towhee* 388
Cedar Waxwing 388
Bewick’s Wren 378
Axis 2:
Cedar Waxwing 495
Pine Siskin 446
Bewick’s Wren 400
Western Tanager* 388
Cassin’s Vireo* 384
Yellow-rumped Warbler 384
California Quail Sl
Song Sparrow 345
Axis 3:
Chestnut-backed Chickadee 428
Rufous Hummingbird 336
Northern Flicker* 318
Pacific slope Flycatcher 294
Cedar Waxwing 2S)
TABLE 3. Garry Oak bird species in 1993 and 1994 with the
highest scores against DCA axis combination | and 2, with
median species designated*.
Year and Species Score Score
1993 axis | axis 2
California Quail 388 371
White-crowned Sparrow 183 250
Olive-sided Flycatcher* 119 230
American Goldfinch 302 342
House Wren 69 135
1994
Brown Creeper 222 230
Rufous Hummingbird 406 275
Brown-headed Cowbird* 373 262
Northern Flicker* 258 426
Pacific-slope Flycatcher 216 162
Cassin’s Vireo 254 224
Note: The former common names (Common Flicker, Rufous-
sided Towhee, Common Starling, and Solitary Vireo) were
used in the data and Figures for Northern Flicker, Spotted
Towhee, European Starling and Cassin’s Vireo.
' The former common names, (Common Flicker, Rufous-sided Towhee, Common Starling, and Solitary Vireo) were used
in the data and Figures 1-4 for Northern Flicker, Spotted Towhee, European Starling and Cassin’s Vireo.
2004
TABLE 4. Garry Oak bird species in 1994 with the highest
scores against DCA axes, with median species designated*.
Species Score
Axis 1:
Song Sparrow 583
Northwestern Crow* 460
European Starling* 420
Rufous Hummingbird 406
Axis 2:
Common Flicker 426
White-crowned Sparrow 40]
Song Sparrow* 294
Chipping Sparrow 283
Rufous Hummingbird PAIS
Axis 3:
European starling 506
Violet-green Swallow 396
Olive-sided Flycatcher* 378
House Wren* 358
White-crowned Sparrow 327
Spotted Towhee 326
Note: The former common names (Common Flicker, Rufous-
sided Towhee, Common Starling, and Solitary Vireo) were
used in the data and Figures for Northern Flicker, Spotted
Towhee, European Starling and Cassin’s Vireo.
The overall frequency (Erickson 2000b) of these
characteristic species gives an indication of the abun-
dance of the communities. Community 1 was most fre-
quent, with the #3-rank Spotted Towhee; the #4 Chest-
nut-backed Chickadee; #6 American Goldfinch; #14
Bewick’s Wren and #16-rank Rufous Hummingbird.
4PiSi
Unngmed group
Community 3
SomMRWa ele
Axis |
ERICKSON: BIRD COMMUNITIES OF GARRY OAK HABITAT 379
Community 2 had the #5-rank White-crowned Sparrow;
#10 House Wren; #12 Pine Siskin; #13 Olive-sided
Flycatcher; and the #19-rank Purple Finch. Commu-
nity 3 had the #6-rank, American Goldfinch; #7
Pacific-coast Flycatcher; #11 Chipping Sparrow; #12
Pine Siskin; #18 Yellow-rumped Warbler; #21
Cassin’s Vireo; and #24-rank Western Tanager. Com-
munity 4 had the #15 rank Northwestern Crow and the
#26 rank European Starling.
Discussion
Sampling and analysis
Communities are differentiated here by their visual
distinctness in the multivariate space defined by bird
frequency and composition, and by differences defined
using thresholds in quantitative index of similarity com-
parisons. Both measures use quantity along with com-
position, which ensures that the communities arising
from the data are actually different from each other.
Although eigenvalues can measure the overall strength
of a multivariate relationship, such as the multivariate
coefficient of variation for each axis in an ordination,
they are not a test statistic in Detrended Correspondance
Analysis.This method uses detrending and rescaling to
avoid the spurious, secondary arch effect of previous
techniques, but this in turn prevents the use of eigen-
values. Although the differences by year were signifi-
cant for many species in previous t-test comparisons
(Erickson, unpublished data), these tests are not used
here, as they are not appropriate for analysis of non-
experimental survey data (e.g., Hurlbert 1984).
Sampling occurred on discrete but much smaller
(0.02 ha) plots in this study than in many others. How-
se ogee nl 2
OCWa
Community 4
4NWCr
FiGurE 3. Garry Oak bird communities from DCA analysis of 1993 data, Axis 1 vs. 2. Large square represents the multi-
variate space formed from the data centred on the DCA axes. Circles are objectively defined groups or communities.
Small square is a subjectively placed community. Bird species coordinates are marked by a cross and designated by
the first letters of the common name (former names as noted in the text). Other data points are the plot coordinates.
380 THE CANADIAN FIELD-NATURALIST Vol. 118
Cc ity 4
Unnamed group saa
Community 3
| ” PSEI
aI sar
SowRWa
FiGure 4. Garry Oak bird communities from DCA analysis of 1993 data, Axis | vs. 3. Large square represents the multi-
variate space formed from the data centred on the DCA axes. Circles are objectively defined groups or communities.
Small square is a subjectively placed community. Bird species coordinates are marked by a cross and designated by
the first letters of the common name (former names as noted in the text). Other data points are the plot coordinates.
oF
{ChSp
Vie
f
Community 3 GS ;
Fh OWA
/ ie
een ies
|
w
Axis 2
Conur a:
4WCSp
Community |
94 group 4
DSp
Ficure 5. Garry Oak bird communities from DCA analysis of 1994 data, Axis 1 vs. 2. See explanation for Figure 4.
ever, the number of plots was correspondingly larger
(262 plots) and records were taken over a much longer
observation period (90 minutes per plot) than in many
studies. Consequently, the results do not represent ex-
treme low values in comparison to studies using other
methods in oak woodlands. In my species accumula-
tion curves, about one half the species were covered
by 15 randomly selected plots, and three-quarters of
the species by 45 plots (Erickson 2000a).
The average number of species detections per plot
(3.7, 1993; 5.0, 1994: Erickson 2000a) is from the
same order of magnitude for two count periods (3
species, 5 species per 0.28 ha plot) in Jalisco, Mexico,
oak woodland; but lower than two other count peri-
2004
Community 2
/
SEI
-HoWr |
4GSw
chSp \
aQn \
4RBNu
Axis 3
| ; ” deel
\ PSFI
Axis |
ERICKSON: BIRD COMMUNITIES OF GARRY OAK HABITAT
\ REC'Bp
4PuFi
th.QCWa?
NRG oe
eee SvaTBCh |:
Community3—\, Community 1
CeWa
381
CoSt
Community 4
I
it eet AS
94 group 4
BHCo \
4RuHu,
FIGURE 6. Garry Oak bird communities from DCA analysis of 1994 data, Axis 1 vs. 3. See explanation for Figure 4.
_ ods (10, 12 species: Corcuera and Butterfield 1999).
_ My averages were much lower than those recorded on
multiple plot, large-area studies: 21 to 25 late-spring
_ species on five, 70 to 130 ha, stands in Oregon (Ander-
_ son 1970), and 9 to 29 breeding species from 40 ha
oak census plots in Pennsylvania (Probst 1980). My
total number of species detections (66) is higher than
in a number of studies in oak woodland (e.g., 38 spe-
cies in Dedon et al. 1984; 20 to 62 species in Leidolf
et al. 2000; 43 to 51 species in Stone no date*; 50 and
58 species in each of two seasons, five forest types,
Corcuera and Butterfield 1999) but is lower than in
some other comparable results (e.g., 77 species in Gar-
cia et al. 1998). My total would be increased by an
additional 12 species which I recorded as “out of plot’,
“out of habitat’, or “overhead”. However, much of this
difference is irrelevant, in that my interest in defining
bird communities was at the plot (not area) level, and
was focused on frequently occurring species which are
easily detected within my plot parameters, not on less
common species used to round out a full species list.
The graphical location method is an objective one,
in its centering technique and the proportional alloca-
tion of multivariate space to each community. Unbi-
ased shapes, such as squares or circles, were used to
define multivariate species aggregations and overlap
in composition was accepted. Other methods include
subjective ones (e.g., Pojar 1995), and other objective
approaches, such as the use of a “fuzzy-clustering
partition coefficient” (Abernethy et al. 2001*). These
methods tend to result in elliptic forms, irregular bound-
aries and volumes of multivariate space, and no overlap
in composition. The elliptical forms assume a trend in
dimensionality that does not actually occur with the
DCA methodology, as it has demonstrated potential
to produce evenly distibuted sample points in multi-
variate space (Peet et al. 1988).
Communities ;
Of the six groups first resulting from the DCA analy-
sis, two from each year were similar enough (similarity
index > 0.33) to combine. One group from 1994 was
dropped because it had less than my conceptual thresh-
old of three species. Two within-year communities were
not differentiated by the results of the other year, but
it was possible to represent them subjectively. To do so,
I placed the square frame (Figures 3-6) on the graphs of
the other year, and in doing so, included species and
multivariate space not already covered. Through this
process, Dark-eyed Junco (Junco hyemalis) was added
to community 3 as a distinct species in 1994, although
in 1993 it was limited to one of the two one-axis com-
binations. The two top-ranking species in frequency,
Orange-crowned Warbler (Vermivora celata) and Amer-
ican Robin (Turdus migratorius) did not contribute to
the characteristic combination of species for the com-
munities. American Robin did qualify as a character-
istic species, but was not used because it was in three
out of four communities.
Consideration was given to dropping another group
which occurred only in 1994, as it had only two dis-
tinct species, Northwestern Crow and European Star-
ling. However, it was kept (as Community 4) because
these two species are potentially important as ecolog-
ical indicators. They may both signify a disturbance
zone and represent a source of disturbance themselves,
via nest predation and nest cavity competition. In
addition, this community can be characterized by the
absence of other species. There may be an inversely
382
THE CANADIAN FIELD-NATURALIST
TABLE 5. Bird communities and characteristic species of Garry Oak habitat.
Species Group
94-3
Community |
American Goldfinch
Spotted Towhee
Bewick’s Wren
Rufous Hummingbird
Chestnut-backed Chickadee
Community 2
House Wren
Olive-sided Flycatcher
Purple Finch
White-crowned Sparrow
Pine Siskin
Community 3
Western Tanager
Yellow-rumped Warbler
Pacific-slope Flycatcher
Cassin’s Vireo
Chipping Sparrow
Dark-eyed Junco*
Community 4
European Starling
Northwestern Crow
Other species:
Song Sparrow n
California Quail d
Violet-green Swallow
Orange-crowned Warbler n
Townsend’s Warbler
Brown Creeper
Cedar Waxwing n
Swainson’s Thrush n
Common Flicker
American Robin n n
Vol. 118
93-3 94-2 93-2 94-1
Cc (¢
(e n
n
n nN
d d
Cc d
(e Cc n
Cc n n
n n (©
d d
d
n Cc
(Gj
c c
n
d
d
(&
n
n
n n
n n
n
Nn (© Cc
Notes: Communities are shown in the boxes. See Table | for species classification codes. The addition of Dark-eyed Junco
to community 3 is partly subjectively derived.
proportional relationship to the presence of North-
western Crow and European Starling across various
sites. In this study, the lack of importance of another
disturbance indicator, Brown-headed Cowbird (Molo-
thrus ater), contrasts with the high numbers of cowbird
nestlings on two Garry Oak sites west of Victoria,
British Columbia (Shepard 2000). However, the present
results reflect only detections of adults and fledged
birds in a reconnaissance investigation.
Cross-year similarity index values were relatively
low, approximately one-half of my expected threshold
value of 0.66. Therefore I considered using the concept
of assemblages to denote a weaker level of association.
However, both the terms community (e.g., Huff and
Raley 1991; Pojar 1995; Garcia et al. 1998; Abernethy
et al. 2001*; Parody et al. 2001) and assemblage (e.g.,
Manuwal 1986; Corcuera and Butterfield 1999; Hagar
and Stern 2001) receive only general use in the litera-
ture, and the term community is referred to more wide-
ly. The year differences I encountered could relate to
increases in bird frequency and dominance shifts in
1994, possibly linked to yearly weather (Haila et al.
1993; Erickson 2000b).
The communities may differ in the life history traits
of their characteristic species, as shown in Table 6
(Leidolf et al. 2000; Ehrlich et al. 1988), and there-
fore in their general habitat and guild use. Species of
community | have mixed nest locations and most are
insectivorous when on breedng territory. Those of com-
munity 2 have an equal dominance of granivores with
insectivores. Most species of community 3 forage in
shrubs and trees. Community 4 species are tree-nest-
2004
Community and species
Community 1:
Nest Location
TABLE 6. Life history traits for characteristic species of Garry Oak bird communities.
Foraging Layer
ERICKSON: BIRD COMMUNITIES OF GARRY OAK HABITAT
American Goldfinch SH
Spotted Towhee GR/ SH
Bewick’s Wren TR
Rufous Hummingbird VN/TR
Chestnut-backed Chickadee SN
American Robin SH/ TR
Community 2:
House Wren TR
Olive-sided Flycatcher TR
Purple Finch TR
American Robin SH/ TR
White-crowned Sparrow SH
Pine Siskin TR
Community 3:
Western Tanager TR
Yellow-rumped Warbler TR
American Goldfinch SH
American Robin SH/ TR
Pine Siskin TR
Pacific-slope Flycatcher TR
Cassin’s Vireo TR
Chipping Sparrow SH/ TR
Dark-eyed Junco GR
Community 4:
Northwestern Crow TR
European Starling TR
Foraging Method Food Type
HB/ SH/ TR FG GV
GR GG IN/ OM
GR GG IN
HB HG NE
SH/ TR BG IN
GR/ SH/ TR GG/FG IN/ FR
GR GG IN
AIR HA IN
GR GG GV
GR/ SH/ TR GG/ FG IN/ FR
GR GG GV
HB/ SH/ TR FG GV
SH/ TR FG IN
SH/ TR FG IN
HB/ SH/ TR FG GV
GR/ SH/ TR GG/FG IN/ FR
HB/ SH/ TR FG GV
AIR HA IN
SH/ TR FG IN
GR GG IN/ GV
GR GG GV
GR GG OM
GR GG IN
Note: Nest location: TR-tree, VN-vine; GR-ground, SH-shrub, SN-snag. Foraging Layer: AIR-air, GR-ground, HB-herb, SH-
shrub, TR-tree. Foraging Method: BG-bark glean, FG-foliage glean, GG-ground glean, HA-hawk, HG-hover and glean. Food
Type: FR-frugivore; GV-granivore; IN-insectivore; NE-nectarivore, OM-omnivore.
ing ground gleaners. Shared traits are as follows: tree
nesting insectivores (community 2,3) and ground glean-
ing (1,2,4). The comparison may suggest general habi-
tat and guild relationships for the communities. This
could include open savanna settings (community 2,4)
and shrubby woodlands or shrub oak (community
1,3). More work is needed on habitat relationships
though.
Comparison with other studies
In this study, bird communities have been delineat-
ed within the Garry Oak habitat at a detailed level by
aggregations of the bird species themselves. This ap-
proach is not typical in the literature. There are indica-
tions of different bird communities in the discussion
of Hagar and Stern (2001) for Garry Oak woodlands,
including Chipping Sparrow as a species of semi-open
woodland and Orange-crowned Warbler as shrub-
associated. Dedon et al. (1984) employed habitat suit-
ability class lists, possibly comparable to more detailed
communities, in California Black Oak (Quercus kel-
loggii) habitat. One shrub community was identified
to subdivide Gambel Oak (Quercus gambellii) wood-
lands (Stone no date*) in Colorado. Artman et al.
(2001) found in Ohio that differences in bird commu-
nities within mixed oak forests could be related to
three moisture index classes. Pojar (1995) described
separate bird communities within Trembling Aspen
forests of north-central British Columbia.
In most oak woodland bird studies, bird communities
have been identified at a more general level. Broad
habitat groupings have formed bird communities,
guilds have been separated by shared traits, or com-
munities have been grouped by successional stages
(e.g., Anderson 1970; Smith 1977; Probst 1980; Davis
et al. 2000; Hagar and Stern 2001). Both Leidolf et al
(2000) and Stone (no date*) described bird commu-
nities associated with four different Gambel Oak habi-
tats (i.e., oak woodland, submontane shrub, Ponderosa
Pine (Pinus ponderosa)/oak woodland, and mixed
conifer/oak woodland), and locations. Garcia et al.
(1998) and Corcuera and Butterfield (1999) referred
to separate bird communities in oak woodlands, mixed
oaks (Quercus rugosa, Q. candicans, Q. obtusata, Q.
laurina) and other groupings for north-central Michoa-
can, Mexico.
Some comparisons and comments can be made
about the composition of communities from the present
study in relation to these others. Shepard (2000) out-
lined the importance of House Wren (found in com-
munity 2) for two Garry Oak sites west of Victoria,
384
British Columbia. However, those sites had steady num-
bers of Red-breasted Nuthatch (Sitta canadensis) and
Brown Creeper (Certhia americana), species which
were unimportant in the present study. Most of the
frequent birds from my study were present in Black
Oak habitat in northern California, but no more than
one or two species were listed by habitat suitability
class (Dedon et al. 1984). Five of the seven species
of community 3 were resident or breeding species in
the ponderosa pine/Gambel Oak forest in north-central
New Mexico (Leidolf et al 2000). The two remaining
species are not found in the range of Gambel Oak.
However, the shrub subdivision in Gambel Oak bird
communities (Stone no date*) is not similar to the
four communities except for the presence of Spotted
Towhee. A community from Trembling Aspen forests
in north-central British Columbia had similarities
(4/7 species) to community 3 (Pojar 1995). Although
this was labelled a group of conifer-related species,
three of four species were associated with Gambel Oak
and Trembling Aspen in southwestern Colorado (Stone
no date*). In addition, Shepard (2000) mentioned high
densities of Pacific-slope Flycatcher, also a species of
community 3; and the importance of Chesnut-backed
Chickadee (found in community 1), for two Garry Oak
sites in British Columbia. These species have similarly
been thought of as conifer (Douglas-fir)-related (Huff
and Raley 1991). Neither the other two Trembling
Aspen bird communities (Pojar 1995), nor the ones
described for Douglas-fir habitat (Shepard 2000; Huff
and Raley 1991) had any substantial similarity to the
four communities in the present study.
Summary
Testing of wildlife habitat relationship models based
on broad habitats (e.g., oak woodland, old-growth
Douglas-fir forest) has given results which questioned
their basic utility (e.g., Dedon et al. 1984; Laymon
1989). This suggests that other methods could be
examined. An alternative approach, which empirical-
ly defines spatial and temporal bird aggregations as
bird communities, is presented here, and may war-
rant further investigation.
The four communities identified in this work could
serve as benchmarks in Garry Oak ecosystem studies.
Like any classification, they should be tested with fur-
ther field work and analysis, particularly for differen-
tiation by habitat features. For example, Erickson and
Campbell (2001) related correlations involving mois-
ture regime, oak diameters, tree form complexity, total
wildlife habitat features, and, for one year, average
number of bird species per plot. Monitoring is recom-
mended as a first step in maintaining characteristic
Garry Oak bird communities, a focus which should
parallel growing concern for this endangered habitat
and contribute to increasing conservation efforts.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Acknowledgments
The field work for this study was completed in an
M.Sc. program at the University of Victoria, toward
which British Columbia Ministry of Forests approved
a part-time education leave. Both Canadian Wildlife
Service and a Canadian Wildlife Service employee’s
fund provided grants which assisted in the first year
of the study. I thank A. J. Erskine for a helpful
review.
Documents Cited (marked * in text)
Abernethy, V. J., D. I. McCracken, A. Adam, I. Downie,
G. N. Foster, R. W. Furness, K. J. Murphy, I. Ribera,
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Received 17 April 2003
Accepted 24 January 2005
Invertebrate Diversity under Artificial Cover in Relation to Boreal
Forest Habitat Characteristics
STEVEN H. FERGUSON! and DANIELLE K. A. BERUBE?
'Fisheries and Oceans Canada, Freshwater Institute, 501 University Crescent, Winnipeg, Manitoba R3T 2N6 Canada
> Department of Biology, Lakehead University, 955 Oliver Road, Thunder Bay, Ontario P7B 5E1 Canada
Ferguson, Steven H., and Danielle K. A. Berube. 2004. Invertebrate diversity under artificial cover in relation to boreal forest
habitat characteristics. Canadian Field-Naturalist 118(3): 386-392
We investigated invertebrate diversity in boreal forests using an experimental design that consisted of counting soil inverte-
brates under artificial cover. The aim was to assess the utility of using soil invertebrate diversity as a measure of ecosystem
health. The study area was grouped into five habitats: upland hardwood, lowland hardwood, conifer, shrub, and conifer-
grass. Simpson’s and Shannon’s indices of invertebrate diversity were negatively correlated with percent herbaceous cover.
Number of recognizable taxonomic units (RTU richness) was negatively correlated with percent litter cover. The number of
individual invertebrates was positively correlated with soil moisture and negatively correlated with percent conifer cover.
Invertebrate diversity varied among habitat types, with conifer forests (spruce, fir, pine) having the highest diversity and
regenerating conifer-grass forests having the lowest diversity, suggesting that successional stages affect diversity. The most
productive sites, upland and lowland hardwood habitats, had the highest abundance of soil invertebrates, although interme-
diate diversity compared to the other five habitats. The results are consistent with the view that diversity increases and then
decreases with productivity and disturbance over succession (ca. 50-100 yr). Hence, maintenance of soil invertebrate diversity
in managed boreal forests requires the provision of a varied landscape with a mosaic of disturbance regimes.
Key Words: arthropods, biodiversity, conifer, earthworms, indices of diversity, moisture, Ontario.
Concerns about the effects of the widespread loss
of biodiversity have prompted many recent studies
investigating the relationship between biodiversity
and ecosystem function (Symstad et al. 2000). Inver-
tebrates are important in the functioning of nearly all
environments, with changes in species composition
potentially reflecting changes in the ecosystem (Majer
1990; Madden and Fox 1997). Hence invertebrates
are increasingly being viewed as reliable indicators to
assess human impacts on the general level of distur-
bance of an ecosystem (Majer 1983; Greenslade 1984;
Andersen 1990). Biodiversity includes all levels of
natural variation and thus diversity indices provide a
relative measure of variation within a community (Til-
man and Pacala 1993). Monitoring diversity across
spatial and temporal scales allows for measurement of
system complexity, functionality, and stability. Knowl-
edge of diversity helps in understanding changes in
ecosystem complexity before and after disturbance.
Information on the habitat characteristics that influence
diversity at various levels and knowledge of habitat
changes resulting from human disturbance are required
for management and conservation (Madden and Fox
19977):
Forest managers can assess diversity changes asso-
ciated with human disturbances that include various
forestry practices through an understanding of the
relationship between animal diversity and forest struc-
ture to determine ecosystem changes (Noss 2000).
Animal diversity includes soil invertebrates common-
ly found under logs and rocks in managed forests
(Kolstrom and Lumatjarvi 1999). Downed wood is im-
portant for organisms in providing shelter and moisture,
and in preventing light penetration. The use of soil
fauna diversity has the potential to act as a surrogate of
forest biodiversity. A number of forest characteristics
have been shown to relate to soil invertebrate diversity,
including understorey vegetation and litter (Bird et al.
2000), plant functional diversity (Siemann et al. 1998),
coarse woody debris (Marra and Edmonds 1998),
conifer species composition (Lattin 1993), forest suc-
cession (Paquin and Corderre 1997), soil moisture
(MacKay et al. 1986) and structural complexity (Fer-
guson 2001).
To further this research, we used a method of sur-
veying invertebrate diversity under artificial cover and
relate indices of invertebrate diversity to measured for-
est characteristics. The study design consisted of (1)
surveys of soil invertebrates (springtails, beetles, cen-
tipedes, slugs, earthworms and isopods) found under
sand-filled cardboard boxes placed on the forest floor;
and (2) surveys of the sampled forest characteristics
(snags, logs, soil moisture, overstorey, understorey,
and ground cover). Forest characteristics were used
to identify habitats within a boreal forest landscape,
and diversity of soil invertebrates was measured. The
goal was to relate forest habitat characteristics to soil
invertebrate diversity to assess their utility as surro-
gate measures of ecosystem changes associated with
forest management practices.
386
2004. FERGUSON and BERUBE: INVERTEBRATE DIVERSITY 327
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Ficure 1. Location of study area in northwestern Ontario and dendrogram of 20 plots (0) located within a 1 km? stand of
boreal forest grouped using cluster analysis based on forest characteristics (e.g., Overstorey. understorey, ground
cover, moisture, coarse-woody debris).
388
Study Area
The study area (Figure 1) was located in northwest-
ern Ontario, Canada, and consisted of a 1 km? area of
boreal forest located along the McIntyre River within
Lakehead University’s natural forest (48°22'N,
89°19'W). The mixed boreal forest consisted of Jack
Pine (Pinus banksiana Lamb.), Black Spruce (Picea
mariana (Mill.) B.S.P.), Balsam Fir (Abies balsamea
(L.) Mill.), White Spruce (P. glauca (Moench) Voss),
White Birch (Betula papyrifera Marsh.), and Trem-
bling Aspen (Populus tremuloides Michx.). The study
site lies within the Boreal Ecosystem that consists of
rolling rocky uplands with coarse well-drained soils
(Rowe 1972). The climate is humid continental with
a mean minimum January air temperature of -15°C
and a mean maximum daily air temperature for July
of 18°C (Environment Canada 2001"). Mean annual
precipitation is approximately 700 mm, including a
mean winter snowfall of 196 cm (Environment Cana-
da 2001"). For the study period (May to September),
mean monthly daily air temperature (1961-1990 nor-
mals) varied from 9.0°C in May to 17.7°C in July
(annual mean = 2.4°C) and precipitation varied from
69.3 mm in May to 88.5 mm in August (annual mean
= 58.6 mm) (Environment Canada 2001").
Methods and Materials
Study design and sample plots
The sampling method was designed to assess soil
invertebrate diversity under a standardized collection
technique that optimized sampling replication, effort,
and coarse taxonomic resolution. Coarse woody debris
occurred in various shapes, sizes, and material. The
use of cardboard boxes standardized the collection and
reduced this variability while sampling a more diverse
fauna than other methods such as pitfall traps. We
decided to use a coarse taxonomic resolution (Bolger
et al. 2000), thereby allowing inexperienced observers
with minimal training to obtain reasonable survey
counts efficiently. A trade-off associated with group-
ing invertebrates occurs between ease of surveys by
observers with minimal taxonomic experience and
the loss of more detailed guild and life history infor-
mation related to individual species.
Twenty plots, each consisting of three adjacent boxes,
were randomly distributed within the forest (minimum
distance between plots was 5 m; Figure 1). Each box
consisted of two 2-liter milk cartons with a plastic
coating of red and white color. These were fitted one
inside the other to create a solid box and filled with
sand (approximately 2 kg) to create a footprint-sized
depression 21 by 9.5 cm. Boxes depressed the leaf
litter an average of 1.3 cm (Ferguson 2000), creating
a microhabitat of increased humidity and decreased
temperature similar to that beneath a log or rock rest-
ing on the forest floor.
Boxes were overturned and the numbers of all soil
invertebrates (>1 mm) were visually counted. Boxes
were lifted individually without disturbing adjacent
THE CANADIAN FIELD-NATURALIST
Vol. 118
boxes or the underlying litter. Twenty weekly surveys
were conducted from 9 May to 24 September 2000
between the hours of 1100 to 1700. The survey num-
bers reflect a relative abundance of soil invertebrates.
Observer bias was consistent across the landscape.
Recognizable Taxonomic Units (RTU; Bolger et al.
2000; Ferguson 2004) were used to group all macroin-
vertebrates (>3 mm) observed under boxes based on
differences in size and feeding habits (Eisenbeis and
Wichard 1987; Brock et al., 1994) and included spring-
tails (Collembola), spiders (Araneae), ants (Formicidae),
ant larvae, centipedes (Chilopoda), Diplura, adult flies
(Diptera), phytophagous mites (Acarina: Oribatida),
bugs (Hemiptera and Homoptera), Pseudoscorpionida,
wasps (non-ant Hymenoptera), moth and butterfly larvae
(Lepidoptera), Gastropoda (snails and slugs), Isopoda
(woodlouse; Tracheoniscus rathkei), beetles (Coleoptera
and Staphylinidae species — adults and larvae), milli-
pedes (Diplopoda), and earthworms (Oligochaeta).
Forest characteristics measured
Site-specific habitat variables were measured 21-
23 August 2000 using 5 x 5 m quadrats centered at
three box plots. One quadrat was located at the centre
of each plot. Four other quadrats were located 10 m
from the centre in cardinal compass directions. A total
of 100 quadrats were sampled for the following habitat
characteristics: percent overstorey cover (>5 m), per-
cent understorey cover (saplings and shrubs 0.5-5 m),
percent herbaceous cover, percent litter cover, percent
grass cover, percent moss cover, percent fern cover,
number of snags (dead standing trees with dbh > 5 cm),
number of decaying logs (> 5 cm diameter), percent
cover by conifers, and a relative measure of soil mois-
ture (1.e., xeric=1, mesic=2, hydric=3). Values for the
five quadrats were averaged for each plot.
Measures of invertebrate diversity
Diversity of soil invertebrates was calculated for
each plot across surveys using RTU richness (num-
ber of RTU at each site), Shannon-Wiener, and Simp-
son’s Indices of Diversity (Ludwig and Reynolds
1988). Shannon’s entropy (H) is a measure of species
diversity used in relation to relative frequencies
(probabilities) of the different species i of the sample
and was calculated as:
H=-% [(n/n) In(n/n)] , from i=1 ton (1)
where n, is the number of individuals belonging to
the ith RTU in the sample and 7 is the total number
of individuals in the sample. H = 0 (minimum value)
when the sample contains only a single RTU, where-
as diversity H increases with the number of RTUs. H
is maximum when all RTUs are equally distributed in
the sample. The Shannon-Wiener index of diversity
is sensitive to changes in the rare species in a com-
munity sample (Pielou 1966). Invertebrate diversity
was also measured by Simpson’s index of diversity
(Simpson 1949), which is sensitive to changes in the
more abundant species and was measured as:
A= 1- Yn (n, - 1)/n(n-1) (2)
2004
Simpson’s index varies from 0 to 1, and gives the
probability that two individuals drawn at random from
a population belong to the same RTU. If the number
approaches () then individuals belong to the same RTU
and the diversity of the community sample is low.
These diversity measures were calculated using the
minimum number of invertebrates observed for the
RTU in a given sampling period and were represent-
ed by an average value for each survey.
Statistical analysis
We performed a cluster analysis of the 11 forest
measures to group the 20 sampling sites into forest
habitats. Classification of habitats types was conducted
by the average-linkage clustering method using a Euclid-
ean distance similarity index (Romesburg 1984). All
variables were standardized between 0 and 1.
Many (8 of 17) forest and soil invertebrate variables
were not normally distributed (Wilk’s statistic) and
transformations (e.g., log, arc-sine) failed to normalize
all variables. Therefore, we used nonparametric analy-
ses by ranking nonparametric data before correlation
analyses (Conover and Iman 1981). Measures of diver-
sity (Simpson’s and Shannon’s), RTU richness, and
number of individuals were normally distributed and
did not require transformations. We report untrans-
formed means in the Figures and Tables in the Results
section to simplify presentations.
Analyses were performed to determine the relation-
ship between (1) soil invertebrate diversity indices and
forest characteristics, and (2) soil invertebrate numbers
for each of the abundant RTU (springtails, beetles,
centipedes, slugs, earthworms, and isopods) and for-
est characteristics. We tested for significant effects of
forest characteristics on dependent measures (e.g.,
diversity) with Spearman’s correlations and partial
correlation analyses (i.e., multiple regression of ranked
data without replacement). ANOVA was used to com-
pare forest characteristics, indices of diversity, and soil
invertebrate abundance relative to forest types, fol-
FERGUSON and BERUBE: INVERTEBRATE DIVERSITY 389
lowed by a Tukey multiple range test if the ANOVA
was significant. Spearman correlations for nonpara
metric data and Pearson’s correlations for parametric
data compared RTU abundance with forest character-
istics. Sample units were the 3-box groups (n = 20)
sampled every week (n = 20). All statistical analyses
were done using SAS (SAS Institute Inc., Cary, North
Carolina 1987) statistical software for microcomput-
ers:
Results
Both indices of soil invertebrate diversity (Shan-
non’s and Simpson’s) were negatively related to per-
cent herbaceous cover (R? = 0.32, F = 5.89, P = 0.01,
n= 20 and R? = 0.35, F = 6.64, P = 0.01 respectively;
Table 1, Figures 2A, and 2B). RTU richness (number
of RTU) was negatively correlated with percent litter
cover, which explained 48.6% of the variance in the
model (F' = 17.0, P= 0.001, n = 20; Table 1, Figure 2C).
Diversity indices were also related to litter cover as
herbaceous cover and litter cover covaried (r = -0.94).
Soil moisture (69.5% of variation explained) and per-
cent conifer cover (9%; Figure 2D) best explained the
number of individual invertebrates. Greater numbers
of soil invertebrates occurred in wet habitats and with
less conifer cover (Table 1).
The forest measures were grouped into five forest
types defined as upland hardwood, lowland hard-
wood (mesic), shrub, conifer, and conifer-grass (Fig-
ure 1). The upland hardwood forest consisted prima-
rily of Trembling Aspen, with little understorey (47%
cover) and the most abundant herbaceous cover
(90%; Table 2). The soil invertebrate community in
the upland hardwood forest consisted of numerous
individuals (mean = 24/plot), moderate RTU diversity,
and large numbers of isopods (Table 2). The lowland
hardwood habitat consisted of mixed hardwoods in a
mesic site that included an intermittent stream with a
deep humus layer. The soil invertebrate community
TABLE 1. Seven multiple regression results used to determine the significant effects of 11 forest characteristics on (1) Shannon’s
index of diversity; (2) Simpson’s index of diversity; (3) RTU richness (where RTU = recognizable taxonomic units); (4)
Number of individual invertebrates, (5) springtail abundance; (6) earthworm abundance; (7) isopod abundance. Of the 11
explanatory variables included (soil moisture, % overstorey, % understorey; % herb cover; % litter; % grass: % moss; % ferns:
number of snags; number of logs; and % conifer cover), only those with significant (P < 0.05) relationships are shown.
Dependent Independent Coefficient Partials Model
variable variable direction R? R? P
(1) Shannon’s diversity index % herb cover negative 0.318 0.318 0.008
(2) Simpson’s diversity index % herb cover negative 0.349 0.349 0.006
(3) RTU richness % litter cover negative 0.486 0.486 0.001
(4) Number of RTU Soil moisture positive 0.695 0.695 0.0001
% conifer cover negative 0.087 0.782 0.02
(5) Springtail abundance % conifer cover negative 0.224 0.224 0.04
(6) Earthworm abundance Conifer cover negative 0.657 0.657 0.0001
Number of logs positive 0.100 0.757 0.02
(7) Isopod abundance % conifer cover negative 0.624 0.624 0.0001
390
Shannon's index
0 25 50 75
Percent herb cover
Species richness
100
0 25 50 75
Percent litter cover
THE CANADIAN FIELD-NATURALIST
Vol. 118
©
Ce)
Simpson's index
Percent herb cover
800
600
400
Number of individuals
0 25 50 75
Percent conifer cover
FIGURE 2. Bivariate relationships between two indices of diversity (Simpson’s and Shannon’s) of soil invertebrates and major
explanatory habitat variables: (A) Shannon’s index of diversity, and percent herbaceous cover (y = -0.307x + 2.29,
7 = 0.318); (B) Simpson’s index of diversity and percent herbaceous cover (y = -0.0810x + 0.883, 7 = 0.349);
(C) RTU richness (number of Recognizable Taxonomic Units) and percent litter cover (y = -0.0692x + 18.6, 7° = 0.486):
and (D) number of individual invertebrates and percent conifer cover (y = -9.38x + 712, r? = 0.695).
living in this forest consisted of moderate diversity,
the greatest number of individuals (mean = 37/plot),
and the most springtails and earthworms. The shrub
habitat had the highest understorey cover (78%), low-
est overstorey (34%), and moderate conifer and litter
cover. The soil community in the shrub habitat was
moderately diverse and consisted of a moderate num-
ber of individuals (mean = 16/plot). The conifer for-
est was the most extensive habitat and was composed
of a mixed softwood/ hardwood (56/44%) forest with
high overstorey cover (66%), high understorey cover
(66%), low herb cover (33%), and high litter cover
(64%). The conifer forest supported the highest soil
invertebrate diversity although few RTU (low RTU
richness) and few individuals (mean = 10/plot; Table
2). The conifer-grass forest type was represented by a
relatively low overstorey (55%), intermediate under-
storey (56%), high conifer cover (53%) with the most
grass (13%) and more herb than litter cover (66/22%).
The soil invertebrate community in the conifer-grass
habitat was the least diverse with the lowest RTU
richness and fewest individuals per plot (n = 9).
The abundance of three out of the six most numerous
RTU were significantly related to forest characteristics
2004 FERGUSON and BERUBE: INVERTEBRATE DIVERSITY 39 |
TABLE 2. Comparison of forest and soil invertebrate characteristics for five forest types. Mean invertebrate abundances
(numbers per m7) are given for six of the more common invertebrates. Means with the same letters do not differ significantly
according to Tukey’s multiple range test.
Upland
hardwood
Variable F IP (n= 6)
Forest characteristics
Snags 6.0 0.005 ab 13.3
Logs 10.5 0.0003 ab 7.0
Soil moisture 26.7 0.0001 b 0.6
Overstorey Sel 0.008 ab 52.8
Understorey 4.4 0.01 b 46.5
Herb 28.3 0.0001 a 89.5
Litter 26.0 0.0001 c 2.8
Grass 2967]: 0.0001 10), 117/
Conifer 19.0 0.0001 b 21.8
Indices of diversity
Shannon’s 5.64 0.006 a2.15
Simpson’s 37 0.002 ab 0.191
RTU richness S/3 0.005 a 19.3
Number of individuals 9.11 0.0006 ab 475
Soil invertebrates
Springtails 3.64 0.03 ab 67.8
Beetles 0.6 0.70 16.5
Centipedes 2 0.34 US)
Slugs 0.8 0.52 4.0
Earthworms 8.8 0.002 a 54.5
Isopods ae) 0.005 a 127.3
(Table 1). Springtail abundance increased with greater
litter cover (22.4% of variation explained; F = 5.2,
P =0.04). Earthworm abundance was negatively cor-
related with percent conifer cover (65.7% explained
variance) and positively correlated with number of logs
(10%; F = 34.4, P < 0.001). Isopod abundance was
negatively related to percent conifer cover (62.4% of
variation explained; F = 29.9, P < 0.001; Table 1). In
contrast, beetles, centipedes, and slugs were relatively
evenly distributed across forest types and their abun-
dance was not significantly related to forest charac-
teristics (not shown in Table 1).
Discussion
Our findings are consistent with the view that diver-
sity is greater in the most common habitat within a
varied landscape, such as a mixed-wood boreal forest
(<80 y) and is often characterised by intermediate
productivity and disturbance. Simpson’s and Shannon’s
Indices of Diversity explained similar amounts of vari-
ation in the pattern of diversity of soil invertebrates
with forest characteristics. Both found percent herba-
ceous cover the most important environmental factor
explaining the pattern of soil invertebrate diversity
among forest habitats. Also, both indices showed simi-
lar correlations, in magnitude and direction, such that
Forest types
Lowland Shrub Conifer Conifer-
hardwood grass
(n = 2) (n=4) (n=6) (n= 2)
a 16.0 b 4.3 ab 7.5 b 5.5
a 15.0 o23 be 2.7 c 2.0
a 1.4 c 0.0 c 0.1 c 0.0
a 69.5 b 34.3 a 65.7 ab 54.5
ab 54.5 a 77.8 ab 66.3 ab 56.0
ab 68.5 be 56.8 c 32.8 b 65.5
cb 14.0 b 31.8 a 64.2 cb 21.5
b 0.5 b 3.5 bee, a 13.0
b 26.0 ab 36.0 a 55.8 a 53.0
ab 1.99 ads Lif; a 2.19 b 1.90
b 0.155 b 0.147 b 0.142 a 0.228
ab 17.0 ab 16.3 ab 14.5 b 14.0
a 723 be 313 c 190 c 179
a 120.5 ab 65.0 b 46.2 ab 76.5
10.0 eS, 16.5 4.5
10.5 12.0 6.5 20.0
6.0 3:3 6.3 6.0
a 116.5 ab 32.3 b 21.0 b 14.0
ab 96.5 ab 64.5 b 25.3 b 14.5
as diversity increased the percentage of herbaceous
cover decreased. In contrast to our findings, soil inver-
tebrates from 27 orders did not differ significantly
among five different landscapes (with the exception
of earthworms) (Kalisz and Powell 2000).
We found a negative relation of soil invertebrate
diversity with increasing composition of conifer veg-
etation. Few herbs and more litter are present under
the conifer cover due to greater soil acidity (Kimmins
1997). Numbers of invertebrates were greater under
herbaceous cover but diversity was reduced. Other
studies have found invertebrates occurring in greater
numbers under deciduous and herbaceous cover rela-
tive to conifer litter (Wallwork 1983; Paquin and
Coderre 1997; Hammond 1997; Marra and Edmonds
1998). Within varied forest landscapes, the greatest
diversity of soil invertebrates likely occurs for the most
common (in time and space) successional community.
In northern boreal forests this is likely for older conifer
stands with greater overstorey and reduced ground veg-
etation understorey. Removal of conifers by natural
disturbance or forest harvesting likely results in lower
initial diversity with increasing diversity over time as
other plants colonize the habitat (i.e., succession). We
found greater invertebrate density under herbaceous
cover associated with hardwood forest, but diversity
392
was lower relative to the conifer forest. More research
is required to explain these differences.
There are some limitations to the sampling method-
ology used in this study. Taxonomic levels lower than
the one used here to identify invertebrates would cer-
tainly provide more detailed results though sampling
efficiency would be reduced. Sampling was done
around mid-day, which limits sampling to invertebrate
groups that are active during the day (Eisenbeis and
Wichard 1987). Results are limited to the invertebrates
visually observed (i.e., >1 mm which may exclude
arthropods such as small mites) found under boxes
whereas smaller individuals and groups found in deep-
er soil are under-represented. Another potential con-
cern is that ants, due to their clumped distribution and
significant effects on community structure, may obscure
patterns among other invertebrate groups (Madden
and Fox 1997).
Diversity indices respond to both changes in species
richness estimates and changes in species evenness.
For example, the mesic lowland hardwood site record-
ed few RTU but high total density. Among those com-
mon taxa associated with the mesic lowland sites are
springtails, earthworms, and isopods, which might be
expected to be more abundant in moist soils. As a result,
one problem with interpretation of diversity results is
the possible relationship between measures of richness
and diversity relative to measures of density. Both
Shannon’s and Simpson’s indices are expected to be
lowest when richness and evenness are low and to
increase with richness and evenness. Shannon’s index
is more sensitive to richness and is impacted by the
inclusion of rare taxa, while Simpson’s index is more
sensitive to evenness of the more common taxa. The
result is usually that the two are generally correlated,
although the relative ranking of sites may differ some-
what. Among the five forest types reported in Table 2,
the two hardwood sites had the highest numbers of
individuals. Both Shannon’s and Simpson’s indices are
reported as moderate for these sites with higher esti-
mates for both in the upland sites. The two conifer-
grass sites yielded the lowest number of individuals.
The Shannon’s estimate is the lowest of the five sites
while the Simpson’s is the highest. Between the other
two sites, which recorded somewhat higher numbers
of individuals, the Shannon’s estimates are the two
highest while the Simpson’s estimates are the two low-
est. The net effect is that across all five habitat types
the correlation coefficient between the Shannon and
Simpson estimates for the forest stands arranged along
a moisture gradient had a negative slope, although not
significant, contrary to expectations. However, both
indices were negatively correlated with % herb cover
and positively correlated with each other. Greater repli-
cates are required in various forest stands along envi-
ronmental gradients to account for forest characteris-
tics that covary.
Although increasing plant diversity significantly
increases invertebrate diversity, local herbivore diversi-
THE CANADIAN FIELD-NATURALIST
Vol. 118
ty is also maintained by a diversity of parasites (e.g.,
flies and nematodes) and predators (Siemann et al.
1998; Ferguson 2001). A community-level prediction
is that invertebrate diversity increases with increasing
plant species diversity, as many invertebrates forage
on the leaves and litter of herbaceous plants (Symstad
et al. 2000). However, if an entire functional group of
plants, such as conifers, is absent from a habitat, then
a landscape-level decrease in soil invertebrate diver-
sity would occur, as many taxa are associated with the
acidic soil and fungal hyphae characteristic of conif-
erous forest floors (Lattin 1993; Butterfield 1999).
Alternatively, diversity is hypothesized to increase and
decrease across the two dimensions of productivity and
disturbance, respectively (Kondoh 2001). Our results
conform to this view, as conifer cover had the highest
diversity at the late successional stage but the lowest
measure of diversity at the early conifer-grass stage.
In contrast, more constant mesic hardwood habitats
had high productivity and low disturbance, and showed
intermediate indices of invertebrate diversity. Appar-
ently, the pattern of invertebrate community diversity
varied among habitat types according to productivity
and disturbance gradients.
The decrease in soil invertebrate diversity with
increasing grass cover may be due to the low nutri-
tive value of grass and the microhabitat conditions of
grassy areas. Low moisture, associated with dry grassy
areas, has been found to have an adverse effect on soil
invertebrate abundance due to a reduced oxygen level
that degrades soil composition, increases erosion, and
mobilizes carbohydrates and nutrients (Marra and
Edmonds 1998). The majority of soil invertebrates are
best suited to moderate moisture levels, as some spe-
cies have little or no exoskeleton (e.g., earthworms) to
protect against high and low soil moisture (Schaefer
1995; Ferguson 2004).
Soil invertebrate diversity was not significantly
related to many of the forest characteristics. Still, the
considerable diversity of invertebrates ensures that
some species are adapted to many of the diverse con-
ditions. For example, soil invertebrates did not show
a relationship to the number of downed logs. This
lack of a relationship with logs may have been relat-
ed to the experimental technique of providing a simi-
lar microhabitat using boxes. Many soil invertebrates
are known to depend on cover provided by coarse
woody debris, such as downed logs, due to their pro-
vision of nutrients and protection from predators and
stability of microclimatic conditions (Lattin 1993;
Ferguson and Joly 2002). Slugs showed few relation-
ships with forest characteristics and were found in a
diversity of habitats. Slugs forage on larvae of bee-
tles and flies and on cellulose and other plant poly-
saccharides (Port and Port 1986). Earthworms bur-
row in moist rich soil and feed on decaying organic
matter from fallen leaves and vegetation (Edwards
and Bohlen 1996). Earthworms were found to be
positively associated with herbaceous cover, nega-
2004
tively associated with conifer cover, and positively
associated with soil moisture. The major food items
of centipedes are earthworms and small arthropods
(Formanowicz and Bradley 1987). Although cen-
tipedes have been found to prefer moist habitats
(Corey and Stout 1992), such as under logs, no sig-
nificant relationships were found with the forest
characteristics measured in this study.
Springtails are abundant in soil, and consume
decomposing plant material and fungal hyphae (Hop-
kin 1997). Their abundance was negatively associat-
ed with litter cover, perhaps because it is living annu-
al plants that provide the overwinter dead material
that fungal hyphae provide as springtail food. The
non-significant correlation (P = 0.06) of springtail
abundance with herbaceous cover and the negative
association with conifer composition contradicts
other studies (Butterfield 1999; Paquin and Coderre
1997). A possible explanation for these differences is
the differing sampling methodologies used whereby
surface-dwelling springtails were sampled here, in
contrast to sub-surface sampling from other studies.
Beetles showed little dependence on any of the
measured forest characteristics in this study, in con-
trast to another study that found habitat dependencies
(Fournier and Loreau 2001). Beetles are adapted to a
wide range of environments partly due to their
exoskeleton enabling life in a variety of moisture
conditions (Eisenbeis and Wichard 1987). Isopods
occur in greater abundance under stones and in damp
environments (Sutton 1980), which is confirmed in
this study by the positive association with relative
soil moisture. Also, isopods were positively associat-
ed with herbaceous versus conifer cover, which is
related to intolerance to acidic conditions of conifer
soils and the greater food availability in deciduous
and herbaceous forest cover (David et al. 2001).
These findings differ with previous research that
found isopod abundance unrelated to forest attributes
(Bolger et al. 2000).
Forest management, with the goal of preserving
forest biodiversity that includes soil invertebrates,
needs to consider the requirements of individual taxa
in boreal ecosystems by providing varied landscapes
within a mosaic of forest stands. For example, cli-
mate change may profoundly influence boreal forest
ecosystems and their management, via increased
temperature and altered precipitation regimes (e.g.,
fires, etc.; Parker et al. 2000). In the boreal forest
area studied here, conifer habitat had the highest
diversity, although abundance and RTU richness
were lower. However, our results need to be guarded-
ly interpreted as they are based upon observations of
a partly artificial system and our invertebrate diversi-
ty results are not sufficiently comprehensive to draw
management conclusions. Still, monitoring soil
invertebrate diversity can provide a means to assess
changes in forest environments with climate warm-
FERGUSON and BERUBE: INVERTEBRATE DIVERSITY 393
ing as well as forest management practices that
include silvicultural interventions to maintain forest
health.
Acknowledgments
Students in the “Fish and Wildlife Practice” 4" year
course offered at Lakehead University participated in
data analysis. Financial support was provided by post-
doctoral (SHF) and postgraduate (DKAB) funding from
NSERC (Natural Sciences and Engineering Research
Council) and Bowater Pulp and Paper Inc., Thunder
Bay Woodlands Division.
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Received 16 April 2003
Accepted 23 November 2004
Observations of Habitat Use by Polar Bears, Ursus maritimus, in the
Alaskan Beaufort, Chukchi, and Northern Bering Seas
DONALD J. HANSEN
U.S. Department of the Interior, Minerals Management Service, 949 E. 36'" Avenue, Anchorage, Alaska 99504 USA
Hansen, Donald J. 2004. Observations of habitat use by Polar Bears, Ursus maritimus, in the Alaskan Beaufort, Chukchi,
and northern Bering Seas. Canadian Field-Naturalist 118(3): 395-399.
A total of 1 112 Polar Bears (Ursus maritimus) at 482 sightings were recorded during aerial surveys in the Beaufort, Chukchi,
and northern Bering Seas conducted primarily during September and October from 1979-1999. Of these bears, 784 were
observed offshore at 400 sightings. The surveys were conducted by the Naval Ocean Systems Center and Minerals Manage-
ment Service; they were designed to monitor the fall Bowhead Whale (Balaena mysticetus) migration. Over the 20-year
period, 1 096 620 kilometers of surveys were flown. The majority of the offshore Polar Bears, 595 bears at 290 sightings,
and most of the kill sites and polar bear tracks were recorded in 80-100% ice cover. The number of bears per kilometer
increased substantially in >24% ice cover, with the highest number observed in 80-100% ice cover. This habitat use proba-
bly is related to the availability of seals, their primary prey. There were 328 bears (83 sightings) recorded on land, and most
of them were associated with whale carcasses and bowhead whale subsistence harvest sites along the Alaskan Beaufort Sea coast.
Key Words: Polar Bear, Ursus maritimus, habitat, Beaufort Sea, Chukchi Sea, Northern Bering Sea, Alaska.
The preference of Polar Bears for extensive ice
habitats is well documented (Stirling et al. 1993; Stir-
ling and Derocher 1993; Amstrup 1995). Polar Bears
need an ice platform to hunt successfully for seals,
their primary prey (Stirling, Andriashek, and Calvert
1993). The bears select ice habitats that increase ac-
cessibility (availability) of seals. Ferguson et al. (2000)
compared ice-habitat use by Polar Bears of the Cana-
dian Arctic Archipelago and Baffin Bay. They found
ice-habitat use to be similar for the two regions. How-
ever, Baffin Bay bears had more limited access to
Ringed Seals (Phoca hispida) because of the complete
absence of ice cover during the summer season. The
Canadian Arctic Archipelago had more consistent sea-
sonal ice cover, which provided the bears with reli-
able access to the seals. Although the Baffin Bay region
had a much higher density of Ringed Seals (1.4-2.1
seals/square kilometer: Finley et al. 1983; Stirling and
Oritsland 1995) than the Arctic Archipelago region
(0.28-0.97seals/square kilometer: Kingsley, Stirling,
and Calvert 1985), both regions had very similar Polar
Bear densities. Ferguson et al. (2000) concluded that
Polar Bear abundance is not always proportional to prey
density because of differences in Polar Bear access to
seals (i.e., availability of prey).
During September and October (open-water season),
the Alaskan Beaufort Sea has great variability in ice
coverage from year to year (Figures la and 1b). Like
Baffin Bay, the Arctic coast of Alaska during light ice
years is free of ice during the open-water season, when
the pack ice is more than 100 miles from the coast (see
Figure la). During the absence of ice in coastal Beau-
fort Sea habitats, bears that occur along the coast either
scavenge on animal carcasses that wash ashore, feed
on the remains of whale carcasses at subsistence whale
harvest sites, or fast until shorefast ice forms and seals
become available (United States Department of the
Interior, Fish and Wildlife Service 1995).
During heavy ice years, the pack ice remains on
the continental shelf; ice floes are common in coastal
waters, and shorefast ice remains or forms early dur-
ing the fall (Figure 1b). These varying ice conditions
affected the movements and distribution of Polar Bears
in the Beaufort and Chukchi seas (Amstrup 2000).
Methods and Materials
From 1979-1999, the Naval Ocean Systems Center
under contract with the Bureau of Land Management
(1979-1982) and Minerals Management Service (1982-
1999) under the Bowhead Whale Aerial Survey Project
has conducted aerial surveys in the Beaufort, Chukchi,
and Bering seas (Ljungblad et al. 1986; Moore and
Clarke 1992; Treacy 2000) to monitor the fall migration
(late August through October) of endangered whales
(Treacy 2000). Information on Polar Bears and sea-ice
coverage was acquired mostly from these aerial surveys.
Surveys were flown primarily at 1500 feet (458 meters),
weather permitting, or at a minimum of 1000 feet
(305 meters) to avoid disturbing marine mammals. The
aircraft used was a de Havilland Twin Otter Series 300
with bubble windows on both sides of the plane. Earlier
flights (1979-1991) over the northern Bering, Chukchi,
and western Beaufort seas used a Grumman Turbo
Goose model G21G (Ljungblad et al. 1986; Moore
and Clarke 1992).
Information also was used from aerial whale sur-
veys conducted during the spring and summer (April
through August) in the northern Bering Sea as well
395
396
Arctic North Slope of Alaska
THE CANADIAN FIELD-NATURALIST
Maximum Retreat of the Pack Ice on 2 October 1998
Vol. 118
“600 Miles
Ficure la. Light Ice Year Information derived from the National Naval Ice Center (http://www.natice.noaa.gov/westarct1.htm).
Maximum Retreat of the Pack Ice on 18 September 1983
Beaufort Sea
Arctic North Slope of Alaska
Maximum Retreat of the Pack Ice on September 18, 1983
ak.
Ficure 1b. Heavy Ice Year information derived from the National Naval Ice Center (http://www.natice.noaa.gov/westarct1.htm).
as in the Chukchi and Beaufort seas (Ljungblad et al.
1986; Moore and Clarke 1992). Incidental sightings
of Polar Bears and their behavior were recorded along
north-south transects and off transects along the re-
mainder of the flight tracks (Figure 2). Information
was recorded on percent ice coverage within about 1-
2 kilometers of the aircraft at each position update
(once about every 5 minutes) and at each sighting loca-
|
1
2004
ioe.
Chukchi Sea
Alaska
Bering Sea
&
HANSEN: HABITAT USE BY POLAR BEARS
397
Polar Bear Sightings
Survey Track
FiGure 2. Study are with survey tracks and Polar Bear sightings.
tion. Position updates, sighting locations, and ice-
coverage data were recorded on an onboard comput-
er system connected to a Global Positioning System
receiver in the aircraft. These records included infor-
mation on numbers of Polar Bears per sighting and
ice cover within about 1-2 kilometers of the aircraft.
Polar Bear tracks and kill sites also were recorded dur-
ing September and October from 1987 through 1999.
Survey effort in the Beaufort Sea focused primarily
along the coast, continental shelf, and shelf break, while
surveys in the northern Bering and eastern Chukchi seas
extended from the coast to the International Date Line
(Figure 2). The Polar Bear sightings, kill sites, locations
of bear tracks, and ice-coverage data were converted
into database files and analyzed with Arcview Geo-
graphic Information System Program 3.2a (devel-
oped by ESRI in Redland, Calif.). Tables and graphs
were created in Microsoft Word and Microsoft Excel
(Windows 2000) to compare bear numbers and sight-
ings with ice coverage (Table | and Figure 3) and kill
sites and bear tracks with ice cover (Figures 4 and 5).
The number of bear sightings and the survey effort
(kilometers flown) were plotted by ice category to com-
pare ice-cover use (Figure 2). This analysis is provid-
ing useful information on habitat use by Polar Bears
occurring in Alaskan waters.
Results and Discussion
Table 1 shows the number of Polar Bears and num-
ber of sightings recorded offshore by ice cover and
on the mainland or on barrier islands. Figure 4 shows
the number of Polar Bear kill sites and ice coverage
recorded at the kill locations. Figure 5 shows the num-
bers of Polar Bear tracks recorded and ice coverage
at their locations.
Over the 20-year period and the 1 096 620 kilome-
ters of surveys flown, 1112 Polar Bears at 482 sightings
were recorded in the Beaufort, Chukchi, and Bering
398
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE |. Number of Polar Bears and Number of Sightings (Recorded Per Year) by Ice Coverage and Number Recorded on
Land.
Year 80-100% Ice 50-79% 25-49%
Ice Ice Ice
1979 15 (8)
1980 29 (2) ayy) iy, <6)
1981 S005) Sii(Q) Dale)
1982 16.3) 4 (4) ives)
1983 165 365) 14 (11) Brn)
1984 23)a- 1 CLS) (2) Sy)
1985 5 (3) ihe (Cb)
1986 9 (6) 3y2@)
1987 4 (2) i eo Gh)
1988 69 (43) 1G) PEO)
1989 155) 0) a= 9A) One®)
1990 52 (40) Perth)
1991 DD ran 3) Aa (2) Gd)
1992 LOS Gib) Sie G2)
1993 Sh aC)
1994 26°, (12) PO) 32)
1995 Disi(eld)
1996 9 (7) ta)
1997 53 (8) 1) ED)
1998 15 (6) 9 (4) 1b Gb)
1999 2 (2) 1b)
Totals: 5957 1(290) 91 (52) 45 (23)
Polar Bear Sightings/Kilometer
@ bear/km
79-50% 49-25% — 24-1% 0%
Ranges of Ice Coverage
100-80%
Ficure 3. Polar Bear sightings per kilometer recorded from
April 1979 through October 1999 in the Beaufort,
Chukchi and Bering Seas.
Ice Coverages at Kill Sites
1
{
77)
o
=
2)
S
-
)
_
o
Q
=
3
rs
100% 99-95% 94-90% 89-80% 79-70% 69-50% 49-40%
Percent Ice Coverage
39-1%
FiGuRE 4. Number of kill sites and ice coveage recorded at
each site.
1-24%
Ice No Ice
Total Number of
On Land Bears and Sightings
51) 20 (10)
(29)
(20)
1 (1) 22 (19)
93 (49)
3-7(2) et) S50 1@2)
6 (4)
(10)
356)
72 (46)
(25)
53 (41)
(18)
(48)
Sp (@)
(16)
2 @)
10 (8)
LL @) 65 (11)
217 (57) 247 (73)
33 (19) 39 (25)
328 (83) 1112 (482)
67 (5)
8 (5)
S13)
28 17) 25, (7)
seas from 1979-1999 (Table 1). Of these bears, 784
were observed offshore at 400 sightings. Figure 2
shows the number of Polar Bears per kilometer of
survey effort over ranges of ice coverage. The num-
ber of bears per kilometer increased substantially in
>24% ice cover, with the highest number observed in
80-100% ice cover. These observations suggest that
Polar Bears may use 80-100% ice cover more often
than lower percentages of ice cover. This habitat use
probably is related to the availability of seals, their pri-
mary prey. Table | lists the number of bears and sight-
ings seen offshore in other ice concentrations. Thirty-
five kill sites and 769 Polar Bear track sightings were
recorded, mostly in 80-100% ice cover (Figures 3 and
4, respectively). Tracks with zero ice cover were record-
ed on land or barrier islands.
A total of 328 bears (at 83 sightings) were recorded
on the mainland or on barrier islands (Table 1). Most
of these bears were associated with whale carcasses
and bowhead whale subsistence harvest sites along
the Beaufort Sea coast. The large numbers of bears
were recorded on land in 1992 (67 bears) and 1998
(217 bears), when repeat sightings were made of sever-
al bears feeding on whale carcasses along the Beau-
fort Sea coast (Table 1).
Studies of radio- and satellite-tagged Polar Bears
have provided useful information on the movements
and habitat use of individual Polar Bears (Arthur et
al. 1996; Ferguson et al. 1998; Amstrup et al. 2001;
Durner et al. 2004). These studies recorded Polar Bear
locations and compared them with satellite-derived,
2004
Number of Polar Bear Tracks
nm
a
ao
nm
o
n
x
rs)
£
(=
°
-
o
a
=
Ss
z
100 99-95 94-90 89-80 79-70 69-60 59-50 49-40 39-30 29-20 19-1% 0
Percent Ice Coverage
FiGurE 5. Number of Polar Bear tracks and ice coverage
recorded at each site.
digitized maps of ice types and ice concentrations in
_ the general areas where the bears were located. These
remote-sensing techniques provide general informa-
tion on habitat use by Polar Bears throughout the
year. Aerial surveys in this study recorded ice types
and ice concentrations within 1-2 kilometers of the
aircraft along the flight track and at the specific loca-
tions where Polar Bears were observed. Both tech-
niques record information on habitat use. Aerial sur-
veys provide real-time information on habitat use at
the actual locations where the bears were observed,
_ while remote-sensing techniques provide valuable
information on bear movements and general informa-
tion on habitat use over time.
Many aerial surveys conducted specifically for
Polar Bears are flown at lower altitudes than the 1500
foot surveys conducted in this study. Aerial surveys
that are conducted at very low altitudes (200-300 feet)
are very likely to disturb Polar Bears and other wild-
life. Our surveys were conducted at 1500 feet to avoid
disturbing marine mammals. Even at 1500 feet some
_ of the bears observed reacted to the aircraft by run-
ning away when the aircraft past overhead. Polar Bears
are quite visible on the ice at 1500 feet because their
tracks are very detectable. Other marine mammals of
comparable size to Polar Bears, such as Beluga Whales,
are easily detected at 1500 feet.
_ Acknowledgments
This study was funded by the U.S. Department of
the Interior, Minerals Management Service, as part
of its Alaska Environmental Studies Program. As the
Principal Investigator, I would like to thank Stephen
Treacy, Project Manager for the Minerals Manage-
ment Service Bowhead Whale Aerial Survey Project,
for providing the survey data on Polar Bears and ice
coverage along the survey tracks from 1979 through
2000, and for his comments on the draft manuscript.
I also would like to thank Elinore M. Anker, who edited
the manuscript.
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HANSEN: HABITAT USE BY POLAR BEARS
399
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Received 23 April 2003
Accepted 16 August 2004
New Records for the Arctic Shrew, Sorex arcticus and the Newly
Recognized Maritime Shrew, Sorex maritimensis
Nett D. Perry!, DONALD T. STEWART?, ELIZABETH M. MADDEN®, and THOMAS J. MAIER*
'Department of Wildlife and Fisheries Science, Texas A&M University, 210 Nagle Hall, College Station, Texas, 77843-2258
USA. Corresponding author.
“Department of Biology, Acadia University, Wolfville, Nova Scotia, B4P 2R6 Canada
‘U.S. Fish and Wildlife Service, Medicine Lake National Wildlife Refuge, 223 North Shore Road, Medicine Lake, Montana
59247 USA
USDA Forest Service, Northeastern Research Station, University of Massachusetts, Amherst, Massachusetts 01003-9285
USA
Perry, Neil D., Donald T. Stewart, Elizabeth M. Madden, and Thomas J. Maier. 2004. New records for the Arctic Shrew, Sorex
arcticus, and the newly recognized Maritime Shrew, Sorex maritimensis. Canadian Field-Naturalist 118(3): 400-404.
We report the first record for the Arctic Shrew (Sorex arcticus) in the state of Montana, USA. We also report range extensions
for the closely related Maritime Shrew (Sorex maritimensis) in New Brunswick and Nova Scotia, Canada. These collections
augment our limited knowledge of the ranges and habitat associations of these rarely collected shrews, and highlight the
need for a careful assessment of the status of S. maritimensis in Canada.
Key Words: Arctic Shrew, Sorex arcticus, Maritime Shrew, Sorex maritimensis, range, state record, Montana, New Brunswick,
Nova Scotia, Quebec.
Approximately 38 species of shrews (genus Sorex)
are currently recognized in North America (Hall 1981;
Jones et al. 1986; George 1988; Wolsan and Hutterer
1998; Fumagalli et al. 1999). Most North American
shrews belong to the subgenus Otisorex, which is pri-
marily restricted to this continent. Until recently, the
only two recognized members of the subgenus Sorex
found in North America were the Tundra Shrew (Sorex
tundrensis) and the Arctic Shrew (Sorex arcticus) (van
Zyll de Jong 1983a), the latter species documented
throughout much of the boreal forest region of North
America. Recent molecular work, however, has support-
ed the recognition of the Maritime Shrew (Sorex mari-
timensis, previously S$. arcticus maritimensis) as a
distinct species (Stewart et al. 2002). The range of the
Maritime Shrew is limited to the eastern portion of
New Brunswick and Nova Scotia.
Sorex arcticus and S. maritimensis are infrequently
observed or collected. Both species exhibit a preference
for grass-sedge meadows and wetland edges (Wrigley
et al. 1979; van Zyll de Jong 1983b; Kirkland and
Schmidt 1996). Although there are limited studies which
include estimates of density (Buckner 1966), both spe-
cies appear to exist at lower population densities than
other common mammal species of the boreal region
(e.g., Masked Shrew [Sorex cinereus] and Meadow
Vole [Microtus pennsylvanicus]), although they may
be locally common in appropriate habitat (Wrigley et
al. 1979). Sorex maritimensis, because of its limited
range and restriction to areas of grass-sedges, is con-
sidered rare (van Zyll de Jong 1983b). This may be a
result of competitive exclusion by similar sized Smoky
Shrews (Sorex fumeus) which exhibit a preference for
less mesic, wooded habitats (van Zyll de Jong 1983a).
Herein we report the first record of S. arcticus in
Montana and range extensions of S. maritimensis in
New Brunswick and Nova Scotia, and provide addi-
tional data on habitat associations in these locations.
We also report a collection of S. arcticus in Sept Hes,
Quebec, one of only six records within the province
(Peterson 1966; van Zyll de Jong 1983b). In the follow-
ing sections, we detail trapping methods and results
for each collection.
Methods
Montana, USA. Between 22 and 27 July 2001 we
conducted small mammal baseline surveys on wet
meadow habitats at Medicine Lake National Wildlife
Refuge, Sheridan County, northeast Montana (48°30'N,
104°20'W; Figure 1). The refuge is located in the gla-
cially influenced prairie pothole region, noted for its
gentle rolling plains with occasional shallow depres-
sions—host to vast wetlands and seasonally flooded
meadows.
We set two 150 m transects, each with 10 trap sta-
tions set 15 m apart for five consecutive nights. Each
station included three different Victor® snap-traps:
one mouse trap, one museum special trap, and one rat
trap (300 trap nights). Nearby pitfall traps consisted of
two 5-m fences (aluminum flashing) with 5-L paint
buckets (dry, not baited) at either end (40 trap nights;
each night a bucket was open was considered a trap
night). The transects were located in the Lake Creek
flood plain, an area seasonally inundated with water
during spring run-off and early summer rains (Stuart
and Kantrud 1971). The plant community was herba-
ceous, dominated by sedges (Carex spp.), grasses (Agro-
pyron spp. and Spartina spp.), and rushes (Juncus
400
2004
PERRY, STEWART, MADDEN, and MAIER: ARCTIC AND MARINE SHREWS
40]
FicurE 1. Suggested range for Sorex arcticus. Includes extensions presented herein and ranges suggested by Peterson
(1966) and van Zyll de Jong (1983b). Insets: A + Indicates location of Montana S. arcticus collections, Medicine
Lake National Wildlife Refuge. @ Indicates location of nearest known record, Lostwood National Wildlife Refuge,
North Dakota. B. o Indicates the location of the Quebec S. arcticus collection, other points (@) indicate location of
historical collections in Quebec.
spp.), with a variety of wetland forbs interspersed. Iden-
tical survey efforts were conducted in two additional
habitat types on the refuge: native prairie and planted
perennial grasslands. Total combined effort for all three
habitat types was 900 snap trap nights and 120 pitfall
nights.
Quebec, Canada. One hundred pitfall traps (800 trap
nights) were set at each of two sites, 17-21 July 1990
(Figure 1). Sites were 8 km north and 8 km east of Sépt
Iles, Quebec (50°12'N, 66°23'W) in coniferous wood-
land near the edge of a marsh and in an old grassy field
next to a road, respectively. The coniferous woodland/
marsh was characterized by White Spruce (Picea
glauca), Balsam Fir (Abies balsamea) and sedges
(Carex spp.).
New Brunswick, Canada. A total of 175 non-baited
pitfall traps (525 trap nights) were set 3 km southeast
of St. George, near L’Etete, New Brunswick (45°8'N,
66°50'W), 3-7 August 1990 (Figure 2). Traps were set
in thickets of predominantly alder (Alnus sp.) with some
mixed conifer growth and some grasses. A small brook
(0.5 m wide) transected the site, maintaining relatively
moist soils.
Nova Scotia, Canada. [Method information is not
available]
Results
Montana, USA. Six S. arcticus, the first confirma-
tion of this species in Montana (Foresman 2001), were
collected in wet meadows at Medicine Lake National
Wildlife Refuge (Figure 1). The nearest known previous
collection was at Lostwood National Wildlife Refuge,
Burke and Mountrail counties, North Dakota, approx-
imately 190 km to the east (R. Murphy, personal com-
munication).
402
THE CANADIAN FIELD-NATURALIST
Vol. 118
200 Kilometers
_
FiGureE 2. Suggested range of Sorex maritimensis, including collections described herein. A indicates the location of the St.
George collection, New Brunswick. B indicates location of the Belle Isle collection, Nova Scotia. Historic locations,
indicated by solid dots, were taken from van Zyll de Jong (1983b). We found no extralimital collections since that
publication.
These specimens were captured using Victor® Mu-
seum Specials (n = 5) and Victor® rat traps (n = 1)
baited with a mixture of peanut butter, oatmeal, flour,
and black sunflower seeds. No S. arcticus were col-
lected in either pitfall traps or smaller Victor® mouse-
traps. Although identical survey efforts were conduct-
ed in native prairie and planted perennial grasslands,
S. arcticus were collected only in wet meadow habi-
tats. Other species collected from wet meadow sites
included: Meadow Vole (n = 19), Deer Mouse (Pero-
myscus maniculatus, n = 1), and Masked Shrew (n = 8).
All specimens were confirmed as S. arcticus; how-
ever, they were collected on the periphery of the S. a.
arcticus and S. a. laricorum ranges, and identification
to subspecies is difficult. These specimens are cata-
logued at the Philip L. Wright Zoological Museum at
the University of Montana, Missoula (catalog numbers
UMZM 18554 — 18559).
Quebec, Canada. Two Arctic Shrews (S. a. arcticus;
Royal Ontario Museum [ROM] catalogue numbers
110254 and 110255) were collected by D.T-.S. near
Sept Iles, Quebec (50°12'N, 66°23'W), 17-21 July 1990
(Figure 1). This is the sixth reported collection of S.
arcticus in this province (Peterson 1966; van Zyll de
Jong 1983b). Both specimens were collected from the
grassy site east of Sept Iles. Other species collected
during this effort were Masked Shrew (n = 7), Pygmy
Shrew (Sorex hoyi; n = 1), and Meadow Vole (n = 1).
This record is as far north along the immediate
coast of the St. Lawrence River as S. arcticus have
previously been reported. The last specimen in this
general area, near Moisie River, just north of Sept
Iles, was trapped in 1937 (van Zyll de Jong 1983b).
Though little trapping has been conducted in this
region, van Zyll de Jong (1983b) speculates that the
species is distributed further north in Quebec and
Labrador throughout the boreal forest, which includes
extensive marshy habitats.
New Brunswick, Canada. Three Maritime Shrews
(originally identified as S. a. maritimensis; ROM cata-
logue numbers 110314, 110315, 110331) were col-
lected 3 km southeast of St. George, near L’Etete, New
Brunswick (45°8'N, 66°50'W), 3-7 August 1990 (Fig-
ure 2). This collection extends the known range of S.
maritimensis ca. 100 km south. Other species collected
from this effort were Masked Shrew (n = 21) and
Northern Short-tailed Shrew (Blarina brevicauda;
e—1))'
Nova Scotia, Canada. On 4 October 1992, a single
specimen of Sorex maritimensis (originally identified
as §. a. maritimensis) was collected at Belle Isle,
Nova Scotia (Tom Herman, personal communication).
The specimen, collected in a marshy area dominated
by the sedge Scirpus cyperinus, represents a provin-
cial range extension of this species by ca.100 km
(Figure 2).
2004
Discussion
Sorex arcticus. The range of the Arctic Shrew is
strongly associated with the boreal forest region of
North America. Southward range expansions of four
other boreal species, Masked Shrew, Meadow Vole,
Meadow Jumping Mouse (Zapus hudsonius), and the
Least Weasel (Mustela nivalis), have been correlated
with contemporary cool, mesic climate patterns in the
Great Plains region (Frey 1992). Jannett and Huber
(1994) speculate that a recent southward extension of
S. arcticus in Minnesota is associated with these cool-
ing climate patterns. Indeed, this southwestward exten-
sion of S. arcticus into Montana could be correlated
with this phenomenon.
Nevertheless, few small mammal surveys have been
conducted in northeastern Montana (D. Flath, person-
al communication); it is possible this has prevented
earlier detection in the state. Similar wet meadow
habitat exists approximately 40 km to the south as
the Big Muddy Creek feeds into the Missouri River.
Thus, it is plausible that the range of S. arcticus ex-
tends further into Montana.
All Montana S. arcticus specimens were sexually
inactive young-of-year. Clough (1963) observed that
over-wintering S. arcticus captured between February
and July were reproductively active. Also, the char-
acteristic tri-colored pelage for adults of this species
was indistinct in these specimens, further supporting
our designation of these shrews as young-of-year,
products of early season breeding by the previous
year’s cohort (Clough 1963; Baird et al. 1983). These
specimens were collected in two groups of three,
each group approximately 3 km apart and separated
by a small perennial stream. Given their inactive re-
productive status and that individuals from each group
were collected no greater than 15 m apart, group mem-
bers might have been litter-mates. As such, a viable
population of S. arcticus likely exists at Medicine
Lake National Wildlife Refuge.
Sorex maritimensis. The Maritime Shrew was pre-
viously considered restricted to the north and east of
the St. John River system, with the nearest previous
collection for this species near Saint John, New Bruns-
wick (Peterson 1966; van Zyll de Jong 1983b). The
collection of S$. maritimensis near L’ Etete, New Bruns-
wick, brings this species within 30 km of the Maine
border. Maine and New Brunswick are separated in
this area by the St. Croix River which could be a bar-
rier to shrew dispersal. There is suitable habitat for S.
maritimensis on the U.S. side of the border and it is
possible they will be found there; however, to date there
is no record of S. maritimensis in Maine (J. Albright,
R. Boone, and L. Master, personal communications).
S. maritimensis is currently recognized as one of only
four mammals endemic to Canada (the others are the
Varying Lemmings /Dicrostonyx hudsonius D. richard-
soni], the Gaspé Shrew [Sorex gaspensis], and the
Vancouver Marmot [Marmota vancouverensis]).
PERRY, STEWART, MADDEN, and MAIER: ARCTIC AND MARINE SHREWS
403
The Nova Scotia and New Brunswick collections of
the newly recognized S. maritimensis imply a greater
range, extending inland and likely including the entire-
ty of mainland Nova Scotia. Stewart et al. (2002)
speculate that recent glacial encroachment (ca. 20 000
y) may have isolated this species on the coastal flood
plain of Nova Scotia. These recent collections may
either provide evidence that S. maritimensis is re-
colonizing former range, following the reestablish-
ment of the boreal forest after the last ice age, or may
reflect the paucity of efforts to collect S. maritimensis
within suitable habitats in these provinces. These col-
lections also support a hypothesis that this species is
limited to moist grasslands and bogs associated with
the boreal forest, competitively excluded from habitats
occupied by the Smokey Shrew, a closely related wood-
land associate. This limited distribution and restriction
to fragile wet meadow habitats suggests this species
may warrant conservation concern.
These collections offer some data regarding the range
and niche characteristics of these shrews. Given that
S. arcticus and S$. maritimensis have been the focus
of very few research efforts, more research targeting
specific life history traits are necessary to better under-
stand the habitat associations and range restrictions
of these shrew species.
Acknowledgments
We particularly thank Tom Herman for providing
data on his specimen of S. maritimensis collected in
Nova Scotia and Kerry Foresman for facilitating the
processing and accession of Montana specimens into
the University of Montana mammal collection. We also
thank the staff at Medicine Lake National Wildlife
Refuge for funding and support of small mammal col-
lections on the refuge. We thank D. Flath and R. Mur-
phy for insight into the status of S. arcticus in Mon-
tana and North Dakota. DTS thanks S. Hindocha and
H. Russell for assistance in the field; and J. Albright,
R. Boone, and L. Master for comments on the status
of S. maritimensis in Maine. The research program of
DTS is supported by an NSERC Discovery grant.
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Clough, G. C. 1963. Biology of the Arctic Shrew, Sorex
arcticus. American Midland Naturalist 69: 69-81.
Foresman, K. R. 2001. The wild mammals of Montana.
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Frey, J. K. 1992. Response of a mammalian faunal element
to climatic changes. Journal of Mammalogy 73: 43-50.
Fumagalli, L., P. Taberlet, D. T. Stewart, L. Gielly, J.
Hausser, and P. Vogel. 1999. Molecular phylogeny and
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from mitochondrial DNA sequence data. Molecular and
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George, S. B. 1988. Systematics, historical biogeography, and
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2™4 edition. John Wiley and Sons, New York. 690 pages.
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first holocene record of the arctic shrew, Sorex arcticus,
from the driftless area, southeastern Minnesota. Canadian
Field-Naturalist 108: 226-228.
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Hoffmann, D. W. Rice, and C. Jones. 1986. Revised
checklist of North American mammals north of Mexico,
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Kirkland, G. L. Jr., and D. F. Schmidt. 1996. Sorex arcticus.
Mammalian Species (524): 1-5.
Peterson, R. L. 1966. The mammals of eastern Canada.
Oxford University Press, Toronto. 465 pages.
Stewart, D. T., N. D. Perry, and L. Fumagalli. 2002. The
Maritime Shrew, Sorex maritimensis (Soricidae: Insecti-
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special consideration of the taxonomic status of S. a.
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Received 12 May 2003
Accepted 21 December 2004
Lichen Zonation on Coastal Rocks in Gwaii Haanas National Park
Reserve, Haida Gwaii (Queen Charlotte Islands), British Columbia
IRWIN M. Bropo! and Norm A. SLOAN2
‘Canadian Museum of Nature, P. O. Box 3443 Station D, Ottawa, Ontario K1P 6P4 Canada
> Parks Canada, Gwaii Haanas National Park Reserve and Haida Heritage Site, P. O. Box 37, Queen Charlotte City, British
Columbia VOT 1SO Canada
Brodo, Irwin M., and Norm A. Sloan. 2004. Lichen zonation on coastal rocks in Gwaii Haanas National Park Reserve. Haida
Gwaii (Queen Charlotte Islands), British Columbia. Canadian Field-Naturalist 118(3): 405-424.
The occurrence of 43 marine lichen species on intertidal rocky shores of southern Haida Gwaii (Queen Charlotte Islands),
British Columbia is described and related particularly to elevation on the shore (duration of seawater immersion) and
exposure to waves. In the area of Gwaii Haanas National Park Reserve and Haida Heritage Site on Moresby Island, rock-
dwelling marine lichens are distributed in zones much as they are elsewhere in the world, although some species found
abundantly only in Haida Gwaii give the local shores a unique appearance. In common with other areas, there is a
conspicuous black band of Verrucaria species (in this case, nine species plus other black lichens) at the upper edge of the
intertidal zone. A conspicuous white band of Coccotrema maritimum above the black band is a unique feature of this flora.
The unusually large percentage of endemic, near-endemic or disjunct lichen species and their phytogeography suggest that at
least the headland rocks along the west coast were refugia during the last glacial maximum. Verrucaria striatula and V.
sandstedei are reported for the first time from British Columbia.
Key Words: Maritime lichens, zonation, Haida Gwaii, Pacific Northwest, British Columbia.
Lichens form a dominant, yet often overlooked,
component of the maritime vegetation along rocky sea-
shores. They create distinct bands along such shores
from polar to tropical seas with maximum abundance,
and the most studies, in north-temperate regions (Flet-
cher 1980; Little and Kitching 1996). The species res-
ponsible for these bands in the northeast Pacific (1.e.,
the Pacific Northwest of North America; see the cover
photo, and Plate 64 in Brodo et. al. 2001: 77), however,
have rarely been investigated.
The shoreline lichen vegetation of Gwaii Haanas
National Park Reserve and Haida Heritage Site can be
understood in the context of the total lichen flora of
Haida Gwaii, British Columbia. Five field trips by the
senior author to Haida Gwaii since 1967 have revealed
a diverse lichen flora of about 580 species with more
than 25 new to science (Brodo 1995). Many of the spe-
cies are rare worldwide, and more than a dozen are en-
demic to Haida Gwaii or are known only from a few
nearby localities in southeast Alaska and Vancouver
Island. Further, many species are disjuncts, having their
nearest additional locality thousands of kilometres dis-
tant, often in western Europe, Asia or the southern
hemisphere (Brodo 1992).
With the establishment of Gwaii Haanas as a Na-
tional Park Reserve, there is a need to develop a base-
line inventory of lichen species for various uses, for
example, to facilitate the conservation of lichen bio-
diversity (Hunter and Webb 2002), to track human and
natural perturbations, to assist in nature interpretation,
and to aid studies of shoreline ecology. Lichens are
well-known indicators of environmental health in use
world-wide (Nimis et al. 2002). Regionally, they have
been used for air quality monitoring in the Tongass
National Forest in southeast Alaska (Geiser et el. 1994*).
In addition, lichen studies have been made to evaluate
the effects of oil spills and post-spill cleaning on marine
ecosystems (Lallemant and Van Haluwyn 1981; Flet-
cher and Crump 2002). A knowledge of maritime lich-
ens is clearly relevant to the prospect of oil and gas
development in the Hecate Strait separating Haida
Gwaii from the British Columbia mainland (Anony-
mous 2002*).
It is important to know if the shoreline lichens of
Haida Gwaii differ from those found elsewhere on the
west coast of North America. The only other detailed
study of Pacific Northwest marine lichen zonation was
done by Ryan (1988a, 1988b) in Washington State, al-
though some observations on shoreline lichens from
southern British Columbia were presented by Noble
(1982).
We report here on the distribution of lichen species
in the upper rocky intertidal zone landward into the salt
spray zone in the Gwaii Haanas area. Because splash
patterns and exposure affect establishment and growth
of shoreline lichens, we examined rocky shores with a
range of exposures to wave action from “protected” to
“very exposed” to reveal species occurrence patterns.
Finally, we compared the rock-dwelling marine lichen
flora and zonation of southern Haida Gwaii with the
flora and patterns seen in other regions.
Study Area
Haida Gwaii, known also as the Queen Charlotte
Islands, is an archipelago of about 138 islands in the
hypermaritime zone of the Pacific Northwest, lying
405
406
about 80 km off the mainland British Columbia coast
between Vancouver Island and southeast Alaska (Fig-
ure |). Its geography, climate and vegetation were des-
cribed in some detail in Brodo (1995).
The two largest land masses of Haida Gwaii are
Graham Island to the north and Moresby Island to the
south. The lower elevations of Graham Island (the
eastern two-thirds) and Moresby Island (the northern
third) have been disturbed by intensive logging activ-
ities, but the southern two-thirds of Moresby Island
were set aside in 1988 as a National Park Reserve
called Gwaii Haanas lying roughly between 52° and
53°N longitude (Figure 2) covering ca. 1470 km? of
land and ca. 1700 km of shoreline (Sloan and Bartier
2000). The lichen studies described here mainly centre
on the extreme southern end of the Park Reserve, at
the tip of Moresby Island and on Kunghit Island (Fig-
ures 2 and 3).
Methods
To characterize our sample locations, we used Gwaii
Haanas’ shoreline classification system (Harper et al.
1994*). This is in the park’s geographic information sys-
tem (GIS) and is based largely upon substrate type,
texture and exposure to wave action. This system was
first developed in Gwaii Haanas and has since become
the standard physical shoreline classification system of
British Columbia (Howes et al. 1994*) and Washington
State [http://www2.wadnr.gov/nearshore/index.asp].
The system has a biological zoning component in
which visible lichens are coarsely grouped into a
“Verrucaria band” (Searing et al. 1995). The British
Columbia scheme has been used in broad-scale region-
al studies of intertidal species diversity (Zacharias and
Roff 2001).
In Harper et al. (1994*), lichens are mentioned as
forming conspicuous shoreline bands. There are refer-
ences to the “Verrucaria zone” and the “white lichen
zone,” but the diversity of species is overlooked. For
example, it is not made clear that the Verrucaria zone
consists of nine black Verrucaria species and other
dark lichens (Brodo and Santesson 1997), and that the
white zone is caused by the dominance of Coccotrema
maritimum, a species described from Haida Gwaii,
whose closest relatives are in Asia and the southern
hemisphere. It is rare in the Pacific Northwest outside
Haida Gwaii and adjacent coastal regions (Brodo
1973). Other lichens of intertidal rocks also proved to
be new to science and generally restricted to Haida
Gwaii and nearby coastal localities. These include
Caloplaca litoricola, Fuscidea thomsonii, Verrucaria
schofieldii, V. epimaura, and Porina pacifica (Brodo
1984: Brodo and Wirth 1998; Brodo and Santesson
1997; Brodo 2004). Several other novelties remain to
be formally described.
Fourteen locations within Gwaii Haanas and one on
Limestone Island were sampled (Figures 2, 3). At each
location, one to three transects were laid out for a total
of 18 transects. A 12 m tape measure was deployed
THE CANADIAN FIELD-NATURALIST
Vol. 117
conforming closely to the rock surface and perpendi-
cular to the high tide line. Transects usually began at
the upper limit of the rockweed (Fucus gardneri) and
barnacle (Balanus and Semibalanus spp.) zone (the
“FB zone,” approximating the mean high water level
[MHW)]) and ran landward to the point at which terres-
trial vascular plants or mosses began. This distance
was divided into eight or nine equal sections to give
approximately nine to ten quadrat points. Because ex-
posed, wave-splashed beaches and shallow slopes pro-
duced longer transects than those on protected, rela-
tively steep shores, the increments of height above the
FB zone from quadrat to quadrat were not uniform,
nor were the distances between quadrats.
At each quadrat point, a 10 x 10 cm grid on trans-
parent plastic with a hundred 1-cm? squares, was cen-
tered on the transect tape. All lichen species under the
grid were recorded together with their coverage in
percent (each square representing 1% coverage). For
smooth rocks, the coverage readings were fairly accu-
rate, but with increasing surface roughness, the esti-
mates were correspondingly approximate. After the
quadrats were sampled and the lichen data recorded,
the vertical height of each quadrat above the starting
point in the FB zone was recorded.
Results
The 18 transects were sorted and analyzed accord-
ing to degree of shoreline exposure from Protected to
Very Exposed, based on Harper et al. (1994*), as listed
in Table 1. Two locations had multiple transects, there
were no transects for localities 6 or 10, and transect
11 had incomplete data and was excluded. Limestone
transects are indicated (L) and all other transects were
over mixed volcanic and fine-grained sedimentary rocks
characteristic of the region’s shoreline (Sutherland
Brown and Yorath 1989).
The transects in Gwaii Haanas yielded 43 lichen
species. Sixty-seven rock-dwelling species occurring
on maritime rocks are currently known from Haida
Gwaii as a whole. An annotated list of all shoreline
species in Haida Gwaii is presented as an Appendix.
This updates the list in Sloan and Bartier (2000; Ap-
pendix B, Part 2) compiled by the senior author based
on specimens at the National Herbarium of Canada
(CANL), Ottawa. The zones indicated in Sloan and
Bartier (2000) were assigned tentatively, based on
label data, and have been corrected in this study. Two
of the lichens from our transects (Verrucaria striatula
and V. sandstedei) are new lichens for Haida Gwaii
(and British Columbia), and ten others were not includ-
ed in the Sloan and Bartier (2000) list because they
were not regarded to be maritime. These are: Adelole-
cia kolaensis, Gyalecta jenensis, Opegrapha gyro-
carpa, Parmelia saxatilis, Placopsis lambii, Porpidia
contraponenda, P. speirea and P. thomsonii. Many rela-
tively common maritime and marine lichens found
elsewhere in Haida Gwaii were not seen in the Gwaii
Haanas transects. These include Caloplaca inconspecta,
2003 BRODO AND SLOAN: LICHEN ZONATION ON COASTAL ROCKS 407
Langara 1327 'W
Island Dixon Entrance
Canada
Masset
e
f , British
A Columbia
| + ak
Graham
Island
Hecate
Queen
Charlotte :
Citys. Skidegate Strait
® Sandspit
Louise
Island
Moresby
Island
GD
Gwaii Haanas Burnaby
A Island
National Park Reserve
and Haida Heritage Site /
proposed National Marine
Conservation Area
SGaang
Gwaii Kunghit
Island
Queen
100 Km Cape Charlotte
St. James Sound
FicurE 1. Location of Gwaii Haanas within Haida Gwaii (Queen Charlotte Islands) including some of the larger islands.
408
132°W
Louise
Island
va
Moresby
Island
Gwaii Haanas
National Park Reserve
and Haida Heritage Site
and proposed
National Marine
Conservation Area
THE CANADIAN FIELD-NATURALIST
Vol. 117
131°W
Ron
18 Limestone
Island
Lyell Hecate
Island eunah
Strait
Burnaby
Island
Inset 2
17
Kunghit Treat Bay
Island
GOON
50 Kilometres
132°W
131°W
FIGURE 2. Map of the Gwaii Haanas area showing Limestone Island (location 18) to the north and Treat Bay (location 17)
to the south of the insets (see Figure 3 for insets).
Catillaria calybeia, Rhizocarpon hensseniae and Rino-
dina gennari. At least one lichen (Porina pacifica) was
found growing abundantly just outside the quadrats
on a protected shore.
The frequency of occurrence (%) of each species
in each transect is listed according to shore exposure
class in Table 2. Verrucaria maura occurred in all tran-
sects on all shores. Among the eight most abundant
lichens (frequencies exceeding 50% in all transects),
four are endemic or nearly endemic to Haida Gwaii:
Caloplaca litoricola, Coccotrema maritimum, Verru-
caria epimaura and V. schofieldii; and one is endemic
to the coastal Pacific Northwest (Herteliana alasken-
sis). The semi-exposed shores had the most species and
the most exposed shores yielded the fewest species.
The results of the transect observations, expressed as
metres above the FB (Fucus/barnacle) zone, are given
in Tables 3 and 4 organized according to the degree of
2003 BRODO AND SLOAN: LICHEN ZONATION ON COASTAL ROCKS
; Ee
; F bY e TS phelican Foint Tnset
pre
wie, eas
Skincuttle han
i 4 ; ee : Hecate
: \ # &. a Ka
Strait
ns Gamenten 8 7 - Ingraham Point
Bay ray
¢
5 Kilometres
Houston Stewart
Channel
Islands
4 Kilometres
SSS
Ficure 3. Inset maps from Figure 2 showing lichen sampling locations 1-16 within Gwaii Haanas (see Table 1).
409
410
THE CANADIAN FIELD-NATURALIST
Vol. 117
TABLE 1. Locations of shore lichen transects in the Gwaii Haanas area grouped according to the shore exposure classification
of Harper et al. (1994).
Exposure Class Location Name
Transect No.*
Latitude (°N) Longitude (°W)
Protected Carpenter Bay 9 131.1660 52.2312
SGaang Gwaii 13 13022511 S2a1015
Limestone Island 18(L>) 131.6170 52.9086
Semi-protected Ellen Island 1 131.0918 52.1544
Orion Point 5) 131.0231 52.1229
Semi-exposed Gordon Islands 2-1, 2-2, 2-3 131.1443 52.0967
Orion Point + 131.0217 52.1241
Pelican Point 14 (L’) 131.2615 52.3472
Pelican Point 15 131.2618 52.3458
Houston-Stewart Channel 16-1, 16-2 131.1261 21258
Treat Bay ity) 131.0080 52.0659
Exposed Ingraham Point 7 131.0325 32.232)
Ingraham Point 8 131.0331 52.2319
Very exposed Gordon Islands 3 131.1493 52.0965
SGaang Gwaii 1 131.2330 52.1021
4 Two locations (2 and 16) had multiple transects, locations 6 and 10 had no transects, the transect at location 11 was in-
complete and excluded.
>L = limestone rock
exposure of each shore. These data are graphed Figures
in 4 and 5, with the ordination based on average mini-
mum values (the base of the thick black line). Because
the values for all shore exposures except “Very Ex-
posed” appear to largely overlap with respect to the
height above the FB zone, the data are pooled in Table
3 and Figure 4; Table 4 and Figure 5 shows the data
only for Very Exposed shores. The data for Quadrat
Position (Table 5), being relative, are not greatly affect-
ed by shore exposure, so all shores are considered
together. The results of all transects with 8-10 quadrats
per transect are shown in Figure 6. (Transects having
only 6 or 7 quadrats cannot be compared with those
having 8-10 transects.)
Translating the continuum of species position into a
zonal scheme with names that correspond with previ-
ous North American or European studies proved to be
challenging. The graphs presented in Figures 4 and 5
based on metres above the upper limit of the FB zone
(Tables 3 and 4) were compared to Figure 6 showing
the species according to their quadrat placement along
the transects (Table 5) with the aim of finding natural
breaks in the continua. This was only partially suc-
cessful. Thus, in Table 6, which presents a summary of
the zones, their position and their dominant lichens, a
few species are listed twice, in different zonal cate-
gories, according to height above the Fucus-barnacle
limit versus their relative quadrat position. Our zonal
terminology basically follows the British System, es-
pecially Fletcher (1973a, 1973b) who, in agreement
with Lewis (1961), argued that the zones are best
described and defined on biological criteria, not on
physical (i.e., tidal) criteria. Lewis (1961) recommend-
ed adopting “Littoral Fringe” in place of “Supralit-
toral Fringe” used by Stephenson and Stephenson
(1949) because it better describes the community that
inhabits the upper fringe of the intertidal zone, washed
by most tides in relatively protected shorelines. We
replace Mesic, Submesic and Xeric subdivisions of the
Supralittoral Zone with the more easily understood
terms Lower, Middle and Upper, respectively. In addi-
tion, we find that the term “xeric,” even taken in its
relative sense, is not an accurate description of a shore-
line habitat. Ryan (1988b) used a numbering system
for his zones, but they basically followed the British
scheme following the distribution of shoreline organ-
isms. O’Clair et al. (1996) used a simplified system
based on wave exposure, and this was adopted by Sloan
and Bartier (2000). Some zonal synonymy, discussed
in detail by Ryan (1988b), is given in the first column
of Table 6.
In the Gwaii Haanas area, Verrucaria mucosa and
Pyrenocollema halodytes are the most abundant spe-
cies at the upper edge of the intertidal zone; i.e., the
lowest point on our transects, where rockweed or bar-
nacles occur (Lower Littoral Fringe; quadrat 1). They
grow there together with some of the smaller and rarer
species of Verrucaria such as V. sandstedei and V. stri-
atula. These are generally too small, thin, and scattered
to create a black zone and, therefore, are hard to find.
The black zone begins with the appearance of the
blacker, thicker species of Verrucaria: V. erichsenii,
V. maura, V. epimaura and V. schofieldii, all of which
can have broad coverage (Table 7) in the Upper Lit-
toral Fringe (quadrats 2-4). Although V. maura con-
tinues to be important well up on the shoreline, the
community changes its character and color with the
appearance of the gray-brown, gray, and orange species
such as Herteliana alaskensis, Arthonia phaeobaea,
and the near-endemic but abundant Haida Gwaii lichen,
Caloplaca litoricola, in the Lower Supralittoral Zone
(quadrats 5-7). Also in this zone is Adelolecia kolaensis
and the cyanophilic lichen Spilonema revertens. Above
this is a poorly defined orange zone (Middle Supra-
EE qC“eer_
2003
BRODO AND SLOAN: LICHEN ZONATION ON COASTAL ROCKS
41]
TABLE 2. Percentage occurrence of shoreline lichen species at locations according to shore exposure classification of Harper et al.
(1994) in the Gwaii Haanas area. P = protected; SP = semi-protected; SE = semi-exposed; E = exposed; VE = very exposed.
% occurrence according to shore exposure class %
Lichen species P (3) SP (2)
Verrucaria maura 100 100
Spilonema revertens 67 100
Caloplaca litoricola 33 100
Coccotrema maritimum 67 50
Verrucaria epimaura 0 100
Herteliana alaskensis 67 100
Pyrenocollema halodytes 67 0
Verrucaria schofieldii 67 100
Arthonia phaeobaea 33 50
Verrucaria amphibia 100 0
Lecidella stigmatea 67 100
Rhizocarpon geminatum 33 50
Xanthoria candelaria 0 50
Amandinea coniops 0 100
Physcia caesia 33 50
Porpidia speirea 0
Verrucaria erichsenii 0
Verrucaria mucosa 67
Caloplaca flavogranulosa 33
Collema fecundum 33
Fuscidea thomsonii
Adelolecia kolaensis
Verrucaria degelii
Verrucaria sandstedei
Lecanora muralis
Ochrolechia subplicans
Parmelia saxatilis
Placopsis lambii
Porpidia thomsonii
Rhizocarpon haidensis ined.
Aspicilia caesiocinerea
Caloplaca citrina
Caloplaca rosei
Caloplaca verruculifera
Candelariella sp.
Fuscopannaria maritima
Gyalecta jenensis
Lecanora sp. #2
Lecanora sp. #1
Lecanora straminea
Opegrapha gyrocarpa
Opegrapha sp.
Porina pacifica
Porpidia carlottiana
Porpidia contraponenda
Rhizocarpon hochstetteri s. str
Verrucaria sp. #5
Verrucaria striatula
i>)
Sees
Nn
Nn
Nn Nn
SESS nO SIS OSS 2 OS 2 SEO OES TOO So. OrO rr Orr Oo Orr
WwW
SrOL ISTO Dru iOrO LOO OS OOS Os OOS O20 FSGS
nn nN
ies)
nn
Oo
—
\o
i)
Total lichen species
littoral Zone; quadrats 7-8) with Caloplaca flavogran-
ulosa, C. rosei (both west coast endemics) and the
widespread Xanthoria candelaria, as well as the in-
conspicuous crust, Rhizocarpon “haidensis.” The
Upper Supralittoral Zone (quadrats 8 — 9) almost at
the upper edge of the beach is well marked by the dom-
inance of the pinkish white lichen, Coccotrema mari-
(number of transects) occurrence in
SE (9) E (2) VE (2) all transects
100 100 100 100
56 100 50 67
56 100 50 61
67 100 0 61
67 50 100 61
33 100 50 56
56 50 100 56
56 0 0 50
33 100 50 44
33 50 0 39
0 0 100 33
22, 0 50 28
22 0 100 28
22 0 0 22
22 0 0 22
44 0 0 22
33 0 50 22
yp) 0 0 22
22, 0 0 17
11 50 0 17
22 50 0 17
0 50 0 17
33 0 0 17
33 0 0 17
0 0 50 11
11 50 0 11
11 50 0 11
22 0 0 11
11 50 0 11
22 0 0 11
0) 0 0) 6
11 0 0 6
0 0 0 6
0 0 50 6
0) 0 0) 6
11 0 0 6
11 0 0 6
0 0 0 6
0 0 0 6
0 0 50 6
0 0 0 6
11 0 0 6
0 0 0 6
0 0 0 6
11 0 0 6
0 0 0 6
11 0 0 6
0 0 50 6
33 15 15
timum, which forms a conspicuous white band on the
coastal rocks of Haida Gwaii, especially on the Pacific
side, although it is less common outside of the archi-
pelago. Accompanying the Coccotrema are such wide-
spread lichens as Placopsis lambii, various species of
Rhizocarpon, and rarer west coast species such as Och-
rolechia subplicans. Higher on the shore and influ-
412
THE CANADIAN FIELD-NATURALIST
Vol. 117
TABLE 3. Summary data for Protected to Exposed shores, metres above Fucus/barnacle zone (16 quadrats).
Species # Extreme
quadrants minimum
Adelolecia kolaensis 3 135
Arthonia phaeobaea 7 0.55
Aspicilia caesiocinerea 1 2.05
Caloplaca citrina 1 1.05
Caloplaca flavogranulosa 3 1.24
Caloplaca litoricola 10 0.55
Caloplaca rosei 1 2.05
Candelariella sp. 1 2.65,
Coccotrema maritimum 11 1.10
Collema fecundum 3} 0.80
Fuscidea thomsonii 3 2.20
Fuscopannaria maritima 1 2.40
Gyalecta jenensis 1 0.90
Herteliana (Bacidia) alaskensis 9 0.60
Lecanora muralis 2 2.65
Lecanora sp. no.1 1 0.55
Lecanora sp. no.2 1 0.90
Lecidella stigmatea 4 0.60
Ochrolechia subplicans 2 1.80
Opegrapha gyrocarpa 1 1.83
Opegrapha sp. 1 1.80
Parmelia saxatilis 2 2.00
Physcia caesia 4 1.00
Placopsis lambii p) 1.85
Porina pacifica if 2.70
Porpidia carlottiana 1 1.50
Porpidia contraponenda 1 1.60
Porpidia speirea + 1.10
Porpidia thomsonii 2 2.00
Pyrenocollema halodytes 8 -0.20
Rhizocarpon geminatum 4 1.70
Rhizocarpon haidensis y) E25)
Rhizocarpon hochstetteri s. str 1 1.30
Spilonema revertens 11 0.60
Verrucaria amphibia 7 0.20
Verrucaria degelii 3 0.30
Verrucaria epimaura 9 0.25
Verrucaria erichsenii 3 0.00
Verrucaria maura 16 -0.20
Verrucaria mucosa 4 -0.20
Verrucaria sandstedei 3 0.00
Verrucaria schofieldii 9 -0.15
Verrucaria sp. #5 1 0.90
Xanthoria candelaria 3 1.40
enced only by intermittent salt spray, is the Terrestrial
Zone (quadrats 9-10), characterized by widespread non-
maritime but salt-tolerant species such as Parmelia
saxatilis as well a Haida Gwaii endemic, Fuscidea
thomsonii, and a few lichens restricted to the Pacific
Northwest, such as Fuscopannaria maritima and Por-
pidia carlottiana. The bird rock community (ornitho-
coprophilous lichens), including Lecanora straminea,
L. muralis, and Caloplaca verruculifera, also occurs
in this zone.
In comparing the graph showing zonation on Pro-
tected to Exposed shores (Figure 4) with the graph deal-
ing with Very Exposed shores (Figure 5), it is imme-
diately apparent that on very exposed shorelines, most
Average Average Extreme
minimum (m) maximum (m) maximum (m)
1.43 2.03 BES
1.04 1.34 2.40
2.05 3.15 3.15
1.05 1.05 1.05
1.85 1.85 2.20
1.07 1.43 Balls
2.05 2.65 2.65
2.65 2.65 2.65
2.05 239) 3.60
1.40 1.50 1.90
2.73 D213. 3.60
2.40 2.40 2.40
0.90 0.90 0.90
1.08 1.20 2.45
2.65 2.65 2.65
0.55 0.55 0.55
0.90 0.90 0.90
25 1.30 2.05
2.10 2.40 2.40
1.83 1.83 1.83
1.80 2.30 2.30
2.20 2.20 2.40
1.11 1.99 Sul
1.93 Pil} 2.40
2.70 3.60 3.60
1.50 1.50 1.50
1.60 1.60 1.60
2.28 2.44 3.60
2.05 2.05 2.10
0.00 0.00 0.35
2S 2.61 Bulld
2.08 DSS 2.90
1.30 1.30 1.30
1.65 2.21 3.60
0.44 0.61 0.69
0.32 0.32 0.35
0.45 0.81 DDS
0.35 0.87 0.90
0.45 1.93 3.60
-0.05 0.08 0.20
0.20 0.33 0.35
0.62 0.78 1.50
0.90 1.05 1.05
1.97 233 3.65
of the lichen species are much higher on the shore, the
zones themselves are much broader (reflecting the
height of wave splash), and not all species are in the
same relative quadrat position. For example, the cyano-
bacterial lichen, Spilonema revertens, which mainly
occurs in the central section of the transects (Middle
Suppralittoral) on Protected to Exposed shores, is found
at the top of the transects (Terrestrial) on Very Exposed
shores. Verrucaria maura begins to invade the rock
over a metre above the Fucus/barnacle limit, and other
shoreline lichens are proportionally higher on the
shore. The five species at the top of the transects are
terrestrial, but salt-tolerant, lichens, not really mari-
time. Also unique to the Very Exposed shores are the
2003
BRODO AND SLOAN: LICHEN ZONATION ON COASTAL ROCKS
413
TABLE 4. Summary data for Very Exposed shores, metres above Fucus/barnacle zone (2 transects).
Species # Extreme
quadrants minimum
Arthonia phaeobaea | 2.05
Caloplaca litoricola | 2.05
Caloplaca verruculifera I 3.65
Herteliana alaskensis I 3.65
Lecanora muralis | 6.70
Lecanora straminea | 3.65
Lecidella stigmatea 2, Poet fe)
Pyrenocollema halodytes 2 0.00
Rhizocarpon geminatum 1 6.70
Spilonema revertens | 5.70
Verrucaria epimaura 2 1-75
Verrucaria erichsenii ] 0.70
Verrucaria maura 2 1.10
Verrucaria schofieldii I 1.10
Verrucaria striatula | 0.00
Xanthoria candelaria 2 3.65
large areas of uncolonized rock (bare of lichens as
well as barnacles or marine algae).
The relative zonal position of some lichen species
on protected shores differs when comparing relative
quadrat position and actual distance above the FB zone
(compare Figures 4 and 6). This may be due to the
ability of these species to occupy broader zones than
others, coupled with the method of averaging mini-
mum and maximum values to draw the charts. The
species included in more than one zonal category are
marked with an asterisk (*) or exclamation (!) in
Table 6.
Species richness (diversity) appears to be greatest
on Semi-exposed shores (33 species) but, since this
category of exposure has the largest number of tran-
sects (9), the significance of this number is difficult to
evaluate. If one combines the lists in Table 2 for Pro-
tected and Semi-protected shores (5 transects) and
those of Exposed and Very Exposed shores (4 tran-
sects), the numbers of species are closer: P+SP: 29
species; SE: 33 species; E+VE: 23 species. Interest-
ingly, the Very Exposed shores, with only 16 species,
include 3 species found in no other exposure type,
Verrucaria striatula, Caloplaca verruculifera and
Lecanora straminea.
One indication of species importance along the
rocky shores is the ability of each species to form large
patches, 1.e., with high coverage values. Table 7 sum-
marizes the coverage classes of all the species that
appeared in quadrats in this study. Some species, and
even species groups, are clearly able to cover larger
areas than others. Almost all the black Verrucaria spe-
cies, for example, are able to cover over 50% of the
100 cm? quadrats, which is why they form a conspic-
uous black belt on the shore. Similarly, Coccotrema
maritimum forms large patches as does Caloplaca
litoricola and Ochrolechia subplicans. Some species
never dominate their zones, however, always occur-
ring in small patches even if they are frequently en-
Extreme
maximum (m)
Average
minimum (m)
Average
maximum (m)
2.05 2.05 2.05
2.05 3.65 3.65
3.65 3.65 3.65
3.65 3.65 3.65
6.70 6.70 6.70
3.65 3.65 3.65
4.73 4.83 6.70
0.00 0.00 0.00
6.70 6.70 6.70
5.70 6.70 6.70
2:23 2.38 2.70
0.70 1.70 1.70
1.40 4.83 6.70
1.10 1.10 1.10
0.00 0.00 0.00
5.18 5.18 6.70
countered. Examples are Spilonema revertens, Pyreno-
collema halodytes, Herteliana alaskensis and Arthonia
phaeobaea.
Rock type generally has a major influence on spe-
cies composition in lichen communities, but some spe-
cies are more tolerant of varying rock type than others.
Verrucaria mucosa was especially abundant on lime-
stone although present on siliceous rock as well. Some
lichens found only, or most commonly, on the lime-
stone transects were Verrucaria amphibia, V. species
number 5, Caloplaca citrina and Gyalecta jenensis.
Pyrenocollema halodytes occurs on limestone rocks as
well as on barnacles (both rich in calcium carbonate).
On the other hand, many common lichens; e.g., Cocco-
trema maritimum, Caloplaca litoricola, Verrucaria
epimaura, Herteliana alaskensis and Collema fecun-
dum, were found only on siliceous rock. Species appar-
ently oblivious to rock chemistry include Verrucaria
maura and V. schofieldii.
Discussion
Marine and maritime lichens distribute themselves
on rocky shorelines in response to many factors, with
the dominant influences being wave exposure and,
particularly, immersion duration (Southward 1958;
Fletcher 1973a; Taylor 1982). Fletcher (1973a) said
that lichens such as Verrucaria mucosa and V. striatula,
which grow among the barnacles in the upper inter-
tidal zone, require 52% submergence per year, the
highest amount for any lichen. There is experimental
evidence (Ramkaer 1977) that spore germination and
hyphal growth at young stages of development are
influenced by salt concentrations, and that the ability
of different lichens to become established in shoreline
habitats is positively correlated with their position on
shoreline rocks. Those lowest on the shore (longest
immersion duration) are the species that have best
germination and hyphal growth under moderate or
even high concentrations of seawater. Mature thalli
414
THE CANADIAN FIELD-NATURALIST
Table 5. Summary data for relative quadrat position for all transects with 8-10 quadrats (15 transects).
Species # Extreme
quadrants minimum
Adelolecia kolaensis 3 4.00
Amandinea coniops 4 6.00
Arthonia phaeobaea 7 4.00
Aspicilia caesiocinerea 1 6.00
Caloplaca flavogranulosa 3 6.00
Caloplaca litoricola 10 4.00
Caloplaca rosei 1 7.00
Caloplaca verruculifera 1 9.00
Candelariella sp. 1 7.00
Coccotrema maritimum 9 6.00
Collema fecundum 3 5.00
Fuscidea thomsonii 3 9.00
Fuscopannaria maritima 1 9.00
Herteliana alaskensis 10 3.00
Lecanora muralis 2 7.00
Lecanora straminea 1 9.00
Lecanora sp. no.1 1 4.00
Lecanora sp. no.2 1 3.00
Lecidella stigmatea 6 4.00
Ochrolechia subplicans 2 7.00
Opegrapha gyrocarpa 1 8.00
Parmelia saxatilis 2 6.00
Physcia caesia 3 6.00
Placopsis lambii 2 8.00
Porina pacifica 1 7.00
Porpidia carlottiana 1 9.00
Porpidia speirea 3 6.00
Porpidia thomsonii 2 8.00
Pyrenocollema halodytes 9 1.00
Rhizocarpon geminatum 5 5.00
Rhizocarpon haidensis 2 7.00
Rhizocarpon hochstetteri s. str 1 8.00
Spilonema revertens 11 5.00
Verrucaria amphibia =) 1.00
Verrucaria degelii 2 1.00
Verrucaria epimaura 10 2.00
Verrucaria erichsenii 4 1.00
Verrucaria maura 15 1.00
Verrucaria mucosa 2 1.00
Verrucaria sandstedei 3 1.00
Verrucaria schofieldii 8 1.00
Verrucaria striatula 1 1.00
Xanthoria candelaria 5 6.00
might be affected by osmotic problems, acidity (sea
water has a relatively high pH), and other seawater
minerals. Other factors that influence zonation include
degree of wetness and seepage of acidic fresh water
from the land above the shore (Fletcher 1973b; Ryan
1988b) and excess heating or freezing (Southward
1958). Verrucaria maura occurs far up on exposed
shores in depressions or shaded nooks indicating a
requirement for moisture. This was noted by European
workers, including Fletcher (1973b), who nevertheless
regards V. maura as one of the more drought-tolerant
of the marine Verrucaria species. Fletcher (1973a)
found that V. maura actually has no requirement for
submergence in sea water at all. It can survive with
Vol. 117
Average Average Extreme
minimum (m) maximum (m) maximum (m)
5.67 7.00 8.00
6.50 6.50 7.00
6.00 6.57 9.00
6.00 8.00 8.00
7.33 N33 8.00
4.80 6.30 9.00
7.00 7.00 7.00
9.00 9.00 9.00
7.00 7.00 7.00
8.00 9.00 10.00
6.00 6.67 7.00
9.33 9.33 10.00
9.00 9.00 9.00
4.80 5.30 9.00
7.50 7.50 8.00
9.00 9.00 9.00
4.00 4.00 4.00
3.00 3.00 3.00
6.17 6.67 8.00
8.00 9.00 9.00
8.00 8.00 8.00
8.50 9.00 9.00
6.00 7.00 8.00
8.00 8.50 9.00
7.00 8.00 8.00
9.00 9.00 9.00
8.00 8.67 10.00
8.00 8.00 8.00
1.00 1.00 1.00
7.80 8.00 9.00
7.00 9.50 10.00
8.00 8.00 8.00
6.27 7.73 10.00
2.40 2.60 4.00
1.00 1.00 1.00
2.90 3.90 5.00
DIDS 4.50 7.00
2.47 UAL 10.00
1.00 1.50 2.00
1.00 1.67 3.00
325 4.00 7.00
1.00 1.00 1.00
7.20 7.60 8.00
only sea spray. Competition with algae and grazing
animals (such as limpets and snails) is regarded to be
a significant factor by some observers (Southward
1958; Ryan 1988b) and minimal by others (Fletcher
1973a). We did not see much evidence of grazing on
the lichens of Gwaii Haanas.
As noted by Fletcher (1980), the lichen bands can
be characterized by life form as well as species. In the
Littoral Fringe, all lichens are anatomically unstratified
(i.e., without a differentiated cortex, algal layer and
medulla) and almost all open by an ostiole rather than
having a discoid apothecium. An exception in Gwaii
Haanas is Herteliana alaskensis, a lichen with bia-
torine apothecia found in the Lower Supralittoral Zone
a
2003 BRODO AND SLOAN: LICHEN ZONATION ON COASTAL ROCKS 415
TABLE 6. Zones formed by lichens on maritime rocks in Gwaii Hanaas. The names of equivalent zones in O’ Clair et al. (1996)
and Ryan (1988b) are also given. For species listed twice under “Characteristic lichens,” an asterisk (*) indicates the lichen’s
zonal position according to its occurrence in the quadrat series (see Figure 6); an exclamation (!) indicates its zonal position
according to its height above the Fucus-barnacle (FB) zone (see Figure 4). P to E = protected to exposed shores; VE = very
exposed shores.
Quad series m above
Zone Type Quadrat FB zone
Terrestrial (Halophilic) 9-10 2.3-3.6
O’Clair: upper salt spray
Ryan: Zones 2A- 2B
Upper Supralittoral Zone 8-9 2.1-2.6
O’Clair: mid salt spray
Ryan: Zone 2C-2D
Middle Supralittoral Zone 7-8 1.4-2.3
O’Clair: low salt spray
Ryan: Zone 2D
Lower Supralittoral Zone 5-7 0.8-1.5
O’ Clair: splash zone
Ryan: Zone 2E
Littoral Fringe, Upper 2-4 0.3-0.8
O’Clair : high intertidal (p.p.)
Ryan: Zone 3-2E
Littoral Fringe, Lower 1-2 -0.3-0.3
O’Clair: high intertidal (p.p.)
Ryan: Zone 4A-3
occasionally in the company of black species of Ver-
rucaria. Lichens with apothecia, also having somewhat
stratified crustose thalli, first appear in the Lower Su-
pralittoral Zone. Higher still, in the Middle and Upper
Supralittoral Zones, the stratified foliose lichens appear.
The biological reasons for this phenomenon are fairly
easy to surmise. Lichens that are submerged frequently
have no need for a loosely organized medulla with air
Characteristic lichens
PtoE VE
Parmelia saxatilis
Fuscidea thomsonii
Fuscopannaria maritima
Rhizocarpon geminatum!
Lecanora muralis!
Porina pacifica
Caloplaca verruculifera*
Lecanora straminea*
Porpidea speirea!
Rhizocarpon geminatum
Lecanora muralis
Spilonema revertens
Coccotrema maratimum
Placopsis lambii
Ochrolechia subplicans
Xanthoria candelaria!
Porpidia thomsonii
Aspicilia caesiocinerea
Rhizocarpon “haidensis”!
Caloplaca rosei!
Porpidea speirea*
Rhizocarpon geminatum*
Lecidella stigmatea
Xanthoria candelaria
Caloplaca flavogranulosa
Caloplaca rosei*
Rhizocarpon “haidensis” *
Lecanora muralis*
Xanthoria candelaria*
Adelolecia kolaensis!
Spilonema revertens!
Caloplaca verruculifera
Herteliana alaskensis
Lecanora straminea
Herteliana alaskensis
Caloplaca litoricola
Arthonia phaeobaea
Physcia caesia
Collema fecundum
Adelolecia kolaensis*
Spilonema revertens*
Caloplaca litoricola
Arthonia phaeobaea
Verrucaria maura
V.epimaura
Verrucaria maura
Verrucaria epimaura
Verrucaria erichsenii
Verrucaria schofieldii
Verrucaria amphibia
Verrucaria erichseniti
V. schofieldii
Pyrenocollema halodytes
Verrucaria striatula
Verrucaria mucosa
Verrucaria sandstedei
Pyrenocollema halodytes
Verrucaria striatula
spaces for gas exchange, and their spores are better
distributed by oozing out of an ostiole than being shot
into the air as would occur from an apothecial disk.
Stratified apothecial lichens are adapted for a basically
terrestrial life style.
The shift in relative position in the zonation by
Spilonema revertens on Very Exposed (where it is
Terrestrial) as compared to less exposed shorelines
Vol. 117
Metres above Fucus/barnacles
THE CANADIAN FIELD-NATURALIST
416
4.00
3.50 -
3.00
2.50
2.00
1.50
1.00
0.50
0.00
-0.50
2 2 O@ Sf & © oN DS 3 V © O © Ww @ Oo HS So © © @ oe & dS @ a > & > © © & / Oo &
os os e) os ee © is & SES Oe” ss CLE SX o* SELES ES é es yy Sos eS
LE COE EFC FEF BOE GF SEF OB EE ESE SF EEF EB E EP EE EES ES oF oF F EEF ESE
@ as fs a” -® eo” SS @ 2S ee & S s Ra eS S oe @ SEOe PF oe & & 5 & Pes < Ss & & > we @ & os & eS
PS eS SF FS SS SF PD GS FP OS SF SF So Pie Fe S ee & & P° QPS LY EF oF
F : Oe 7 0 or 2
oo “<. RS ws Rs Fo oe ae es Fe & 3 & Fee ss ror & QP x eS RO is) Ko s e ¢ x ES eg Z S
SF WANA RO w CN SC SS Se ie oe
Ke ak es) 0 & ee PF ¥ of
SS es Co we < ge
x < «
e €
The thick line is the range of average values. The thin lines represent the total range (extreme maximum and
FicureE 4. Zonation of maritime lichens on Protected to Exposed shores, ordered by metres above the Fucus-barnacle zone.
minimum) values.
2003 BRODO AND SLOAN: LICHEN ZONATION ON COASTAL ROCKS 417
ecies etres above Fucus/barnacles
mn Sp Metres above Fucus/barnacl
“%
Ge)
%
@
y ° A I) 7) rN on fo) Ni 00
°% ° ° r=) ° ° ° ° ° ro)
Pe ro) ro) ro) } ro) rs) ro) } }
FiGuRE 5. Zonation of maritime lichens on Very Exposed shores, ordered by metres above the Fucus-barnacle zone. The
thick line is the range of average values. The thin lines represent the total range (extreme maximum and minimum)
values.
418 THE CANADIAN FIELD-NATURALIST Vola?
Species 4 Quadrant
%,
%e
ke es y ° Nn h a oo S =a
j=) S S
beh ro) ros) ro) ) ) 8 S
FiGcuRE 6. Zonation of maritime lichens on Protected to Very Exposed shores, ordered by relative quadrat position. The
thick line is the range of average values. The thin lines represent the total range (extreme maximum and minimum)
values.
2003
BRODO AND SLOAN: LICHEN ZONATION ON COASTAL ROCKS
419
TABLE 7. The number of quadrats sampled in which lichen species are represented, according to percentage coverage category.
Coverage category (%)
Lichen species 1-5 6-10 11-20
Adelolecia kolaensis 4 | 2
Amandinea coniops 3
Arthonia phaeobaea 5 | |
Aspicilia caesiocinerea | ]
Caloplaca citrina
Caloplaca flavogranulosa 1
Caloplaca litoricola 6 4 3
Caloplaca rosei 2
Caloplaca verruculifera 1
Candelariella sp. |
Coccotrema maritimum 1 4 2
Collema fecundum
Fuscidea thomsonii 3
Fuscopannaria maritima 1
Gyalecta jenensis 1
Herteliana alaskensis 7 4 3
Lecanora muralis 2
Lecanora straminea 1
Lecanora sp. #1
Lecanora sp. #2
Lecidella stigmatea 4
Ochrolechia subplicans 1
Opegrapha gyrocarpa
Opegrapha sp.
Parmelia saxatilis
Physcia caesia 1
Placopsis lambii 2 1
Porina pacifica
Porpidia carlottiana
Porpidia contraponenda
Porpidia speirea 4
Porpidia thomsonii 1
Pyrenocollema halodytes 10
3
2
—
Sas a
—
i)
BRNNRK eK
—
Rhizocarpon geminatum
Rhizocarpon haidensis ined.
Rhizocarpon hochstetteri s. str 1
Spilonema revertens 17
Verrucaria amphibia 2
Verrucaria degelii
Verrucaria epimaura 2
Verrucaria erichsenti 1
Verrucaria maura 11
Verrucaria mucosa
Verrucaria sandstedei
Verrucaria schofieldii Z 2 2
Verrucaria striatula
Verrucaria sp. #5
Xanthoria candelaria +
i
[id )
SN Oe
aN
—
me
(where it is Middle Supralittoral) may be due, in part,
to the species’ sensitivity to excessive inundation by
tidal splash. More likely, it is due to its inability to
physically withstand the pounding of waves on highly
exposed headland rocks. Spilonema is a microfruticose
lichen and is attached to the rock relatively loosely
compared to its crustose neighbours. A similar shift
in the distribution of the fruticose Lichina pygmaea
occurs on European shores (Fletcher 1973a). Spilo-
21-30
31-40 41-50 51-60 61-70 71-80 81-90 91-100
w
See nNWe
oo
tS
—
iT)
NCO
nema revertens is not a particularly maritime lichen,
however, being frequently found in inland areas (Brodo
et al. 2001).
The species diversity on protected and semiprotect-
ed Gwaii Haanas shores is not significantly lower than
that of more exposed shores. Chu et al. (2000) found
the opposite on Hong Kong shores. They hypothesized
that wave-exposed shores have more microhabitats to
be exploited than do quiet bays. Our data do not sup-
420
port Chu’s observations, but our data suffer from un-
even sampling in the various exposure categories and
may not be as reliable.
Light influences species composition especially on
the more terrestrial shoreline habitats (Fletcher 1973a).
For example, Caloplaca and Xanthoria species are
almost entirely restricted to sunny rocks in Gwaii
Haanas. Fletcher (1973a) found that most lichens in
the Littoral Fringe and even the Lower Supralittoral
Zone are largely indifferent to light conditions, but
Ryan (1988b) reported that Verrucaria mucosa only
occurs in shaded habitats. This species was found in
both unshaded and shaded sites in Gwaii Haanas,
although it was more abundant on shaded limestone.
Since exposure to sun affects moisture availability and
retention, some correlation of species distribution ac-
cording to shade conditions is to be expected. Shaded
shores are almost always also protected shores, so it
is difficult to separate the two factors in explaining
differences in lichen vegetation.
Shoreline rocks are frequently subject to manuring
by sea birds, increasing the nitrogen load (urea and
ammonia) and raising the pH of the rock surface, and
this affects the composition of the saxicolous lichen
communities, especially in the salt spray zone. Orni-
thocoprophilous lichens that prefer such habitats in-
clude Lecanora straminea, Caloplaca verruculifera,
Physcia caesia and Xanthoria candelaria, all present
on the shores of Gwaii Haanas wherever the conditions
are suitable.
The relative position of the marine and maritime
species in Gwaii Haanas agree closely with observa-
tions made by others, in so far as there are species in
common, e.g., Verrucaria mucosa, V. striatula, Pyreno-
collema halodytes occur in the upper edges of the in-
tertidal zone; V. maura appears higher and has a broad
distribution; Xanthoria candelaria, Physcia caesia and
Caloplaca verruculifera are associated with bird rocks;
etc. (Eliasson 1965; Ryan 1988b; Sheard and Ferry
1967; Sheard 1968; Fletcher 1973a; Fletcher 1973b).
The west coast endemics, and especially the mari-
time lichens closely restricted to Haida Gwaii, com-
prise 17 of the 67 species listed in the Appendix. It is
useful to examine these species to see what their eco-
logical and taxonomic equivalents would be elsewhere
in the world. We will begin with ecological relation-
ships.
Caloplaca litoricola, a Haida Gwaii specialty, is in
the Supralittoral Caloplaca zone as one would expect,
but, since it is grey rather than yellow, it does not help
to create an orange zone as other species of Caloplaca
do in Europe or even eastern North America. On the
other hand, the Pacific Northwest endemics C. rosei
and C. inconspecta, and especially Caloplaca flavo-
granulosa, are the ecological equivalents of the similar
European C. marina (also in western North America
from California to Vancouver Island, but not reaching
Haida Gwaii; Arup 1992), which is part of the “orange
zone” of European shores. Instead of the fruticose
THE CANADIAN FIELD-NATURALIST
Vol. 117
cyanophilic lichen, Lichina pygmaea, common in the
British Isles (and rare on the American east coast),
we have Spilonema revertens, a microfruticose cyano-
philic lichen in Gwaii Haanas, although it tends to be
higher in the transects than Lichina would appear. In-
stead of species like the orange foliose lichen, Xan-
thoria parietina (common in both Europe and along
the east coast of North America) in the Middle to
Upper Supralittoral Zone, Haida Gwaii has the white
crustose lichen Coccotrema maritimum, resulting in
a conspicuous white zone replacing the orange zone
seen in Europe. We have no ecological equivalent for
their maritime saxicolous fruticose lichen, Ramalina
siliquosa, but instead of Fuscidea cyathoides, Haida
Gwaii has the narrowly endemic F: thomsonii in the
Terrestrial zone (Brodo and Wirth 1998).
The distribution of geographically or ecologically
separated, closely related taxa (vicariants) with respect
to these endemics or near-endemics is especially in-
teresting. The categories of relationships and the taxa
involved are summarized below, in most cases, with
references to discussions already published.
High Mountain connections
The following species either have close relatives in
the arctic-alpine flora, or have populations/subspecies
that are found only on maritime and alpine rocks, not
in between.
Caloplaca litoricola: C. exsecuta (Ny1.) Dalla Torre
& Sarnth. (Brodo 1984)
Ochrolechia subplicans: subsp. hultenii 1s on shore-
line rocks; subsp. subplicans grows in the alpine zone
from Haida Gwaii to Alaska (Brodo 1988).
Porpidia carlottiana: populations on Haida Gwaii
either on shore or in mountains; close to P. glauco-
phaea (Korber) Hertel & Knoph in Hertel, an ocean-
ic species (Gowan 1989).
Southern Hemisphere connections
These species are closely related to species common
in the southern hemisphere, either in South America
or Australasia.
Coccotrema maritimum: C. cucurbitula common on
trees in Chile, etc. as well as in other parts of the Paci-
fic Basin, e.g., Japan (Brodo 1973)
Collema fecundum: C. novozelandicum Degel., on
calcareous non-maritime and maritime rocks and soil,
South Island, New Zealand (Degelius 1974, 1979)
Verrucaria epimaura: V. durietzii 1. M. Lamb, mari-
time lichen from the Aukland Islands (Brodo and
Santesson 1997)
Kohlmeyera complicatula: the same or related spe-
cies are On maritime rocks in western South America.
(Brodo 1976)
Related to widespread maritime species
These species are most closely related to other mari-
time lichens.
Lecanora species number 1: L. actophila, L. heli-
copsis This undescribed Lecanora with a thick, white,
xanthone-containing thallus will be discussed in a pub-
2003
lication in preparation. It is clearly related to other
species in the L. dispersa aggregate such as those
listed above.
L. poliophaea (undescribed subspecies): subsp.
poliophaea. The Haida Gwaii populations of L.
poliophaea differ in some respects from European
populations and are probably deserve taxonomic
recognition. This will be discussed in the publication
in preparation mentioned above.
Verrucaria. schofieldii: V. erichsenii, a widespread
supralittoral species (Brodo and Santesson 1997).
Related to widespread non-maritime species
The following species have their closest relatives
as Temperate or Boreal, non-maritime lichens.
Fuscidea thomsonii: F. intercincta (Nyl.) Poelt, F:
atlantica (H. Magn) P. James & Poelt, both are Euro-
pean species found in regions with an oceanic climate
(Brodo and Wirth 1998; Oberhollenzer and Wirth 1984).
Fuscopannaria maritima: F. thiersii P. M. J@rg., a
Pacific Northwest species on iron-rich moist rocks
(Jérgensen 2000); and F: leucostictoides Ohlsson, a
western American corticolous species (Jorgensen 1978).
Porina pacifica: Porina chlorotica (Ach.) Miill. Arg.,
widespread northern species on shaded rock faces
(Brodo 2004).
Rhizocarpon maritimum ined: R. cinereovirens is a
Temperate species on shaded and exposed rocks, B. C.,
Black Hills, Long Island, N.Y. (The species, which will
be described in a forthcoming paper, is closely related
to R. cinereovirens (Fryday 2002: 463).
These phytogeographic relationships of the endemic
or near-endemic maritime lichens of Haida Gwaii and
their vicariant taxa suggest survival in the area during
the Pleistocene glaciations. Relationships with montane
species may indicate, as has been suggested (Clague
1989; Heusser 1989), that during the several glacial
advances of the Pleistocene, some coastal areas and
the highest mountain peaks of Haida Gwaii remained
exposed. They would, therefore, have been available
for colonization by lichens. It is possible that species
that evolved at sea level from montane ancestors were
highly restricted to coastal rocks and never were able to
reinvade the intervening elevations although the highly
exposed and harsh seacoast environment has much in
common with alpine habitats and often shares the same
or related species. It is probably significant that the
closest relative of Coccotrema maritimum, a rock-
dwelling species, is C. cucubitula, primarily a corti-
colous species throughout its range. A glacial relic
would, of course, have to survive on non-arboreal sub-
strates. Schofield (1989) notes that all the Haida Gwaii
endemics among the bryoflora occur on rock or soil.
Many organisms are distributed around the Pacific
Rim, or are disjunct from regions thousands of kilo-
metres away. Plants and animals showing these pat-
terns usually are related at the genus level or above,
but these relationships show up at the species level in
lichens and sometimes bryophytes (Schofield 1989).
BRODO AND SLOAN: LICHEN ZONATION ON COASTAL ROCKS
The fact that the land mass of Haida Gwaii represents
a crustal plate fragment (terrane) that originated off the
coast of Peru and and started its northward migration
approximately 230 million years ago (Sutherland-
Brown and Yorath 1989) provides a possible way for
the species to have been transported (assuming the spe-
cies had evolved by that time), although long distance
dispersal is another means. Similar patterns are known
from bryophytes; e.g., the moss Polytrichadelphus
lyellii Mitt, which is known from British Columbia
to California. The other 20 species of the genus are
from South America, New Zealand and Australia
(Persson, H. 1968. The possible migration routes of
the species with southern hemisphere affinities are
discussed by Brodo (1973).
Maritime lichens on Haida Gwaii that are disjunct
with western Europe or even eastern North America
probably reveal ancient, probably Tertiary, distribu-
tion patterns that were at first continuous but became
dissected by climatic and geological events over the
past 10-20 million years leaving the Haida Gwaii
populations clinging to their outposts in microclimat-
ically suitable habitats. Equivalent patterns among
the mosses are common (Schofield 1984).
Conclusions
Rock-dwelling marine lichens of Gwaii Haanas are
distributed in zones much as they are elsewhere in the
world, although some species found abundantly only in
Haida Gwaii create a unique appearance of these zones,
such as the white Coccotrema zone, as compared with
other regions. The unusually large percentage of en-
demic, near-endemic or disjunct species suggests that
at least the headland rocks along the west coast were
refugia during the last glacial maximum.
Acknowledgments
We thank Gwaii Haanas (Parks Canada) for fund-
ing the summer 2000 fieldwork and Doug Burles and
Lee Edenshaw for field assistance. Dr. Fenja Brodo
made numerous helpful suggestions on early drafts and
assisted with some quadrat studies when not execut-
ing her own Gwaii Haanas inventory project. IMB,
now retired from the Canadian Museum of Nature,
thanks the Museum for appointing him as a Research
Associate and providing him with space and facilities
for his lichen research. We dedicate this paper to the
memory of Bruce Ryan, who first studied the maritime
zonation of lichens in the Pacific Northwest and did
it so well.
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Received 30 June 2003
Accepted 17 February 2004
424
THE CANADIAN FIELD-NATURALIST
Volany
Appendix: Lichens of Haida Gwaii Found on Maritime Rocks
Note: Many of the lichens listed below are non-maritime lichens that, on occasion, are found growing in the maritime
zone thereby demonstrating a tolerance for salt spray. Species not found in Gwaii Haanas National Park Reserve are marked
with an asterisk (*). Those new to British Columbia are in boldface. Voucher specimens of all these records can be found in
the Canadian Museum of Nature (CANL).
Adelolecia koalensis (Ny1.) Hertel & Rambold (Syn. Lecidea
conferenda Nyl.) This was first reported for British Col-
umbia in Brodo (1995).
*Amandinea coniops (Wahlenb. in Ach.) M. Choisy ex Scheid.
& H. Mayrh.
Arthonia phaeobaea (Norman) Norman
Aspicilia caesiocinerea (Nyl. ex Malbr.) Arn.
*A spicilia supertegens Arn. This is not normally a maritime
species. The single voucher specimen requires further study.
*Bacidina inundata (Fr.) Vézda. This species was also found
in streams in Haida Gwaii.
*Caloplaca chlorina (Flotow) H. Olivier. The voucher speci-
men was verified by both T. Tonsberg and C. M. Wetmore.
Caloplaca citrina (Hoffm.) Th. Fr.
Caloplaca flavogranulosa Arup
*Caloplaca inconspecta Arup
Caloplaca litoricola Brodo
Caloplaca rosei Hasse
Caloplaca verruculifera (Vainio) Zahlbr.
*Catillaria chalybeia (Borrer) Massal.
*Cliostomum griffithii (Sm.) Coppins
Coccotrema maritimum Brodo
Collema fecundum Degel.
*Ephebe lanata (L.) Vainio
*Fuscidea mollis (Wahlenb.) V. Wirth & Vézda. The voucher
specimen is not typical of the species, so this record is
questionable.
Fuscidea thomsonii Brodo & V. Wirth
Fuscopannaria maritima (P. M. Jorg.) P. M. Jorg.
Gyalecta jenensis (Batsch) Zahlbr.
Herteliana alaskensis (Nyl.) Zahlbr.
*Kohlmeyera complicatula (Nyl.) Schatz
Lecanora muralis (Schreber) Rabenh.
*Lecanora poliophaea (Wahlenb.in Ach.) Ach. s. lat.
Lecanora straminea Wahlenb. ex Ach.
*Lecanora tenera (Nyl.) Cromb.
Lecanora sp. number 1. This is a xanthone-containing. mari-
time, saxicolous member of the Lecanora dispersa group
and almost certainly is undescribed.
Lecanora sp. number 5. This lichen is similar in many respects
with L. contractula Ny\l.
*Lecidella scabra (Taylor) Hertel & Leuckert
Lecidella stigmatea (Ach.) Hertel & Leuckert f. stigmatea
Ochrolechia subplicans (Ny1.) Brodo subsp. hultenii (Erichs.)
Brodo
Opegrapha gyrocarpa Flotow
Opegrapha sp. This is a sorediate species containing roccel-
lic acid, with 3-septate spores and lirelliform ascomata
unlike those of O. gyrocarpa. It may be undescribed.
Parmelia saxatilis (L.) Ach.
Physcia caesia (Hoffm.) Fiirnr.
Placopsis lambii Hertel & Wirth. There is a single record of
P. gelida (L.) Lindsay s. str. on a rock in a tidal marsh, but
otherwise the species is only known on Haida Gwaii from
inland localities, usually on roadsides and fresh rock
exposures.
*Polychidium muscicola (Sw.) S. F. Gray
Porina pacifica Brodo. This species, which superficially
resembles P. chlorotica (Ach.) Miill. Arg., was only recent-
ly described (Brodo 2004)
Porpidia carlottiana Gowan
Porpidia contraponenda (Arnold) Knoph & Hertel
Porpidia speirea (Ach.) Kremp.
Porpidia thomsonii Gowan
*Punctelia stictica (Duby) Krog
Pyrenocollema halodytes (Nyl.) R. C. Harris s. lat. We have in-
cluded specimens with sunken perithecia as well as those
with sessile perithecia under this name if the perithecia
were under 0.3 mm in diameter. The much larger P. sub-
litorale (Leighton) R. C. Harris ex Fletcher in Coppins,
P. James & D. Hawksw. has not yet been found in Haida
Gwail.
Rhizocarpon geminatum Korber
Rhizocarpon “haidensis” Brodo, ined. This species is closely
related to R. cinereovirens (Miill. Arg.) Vainio (Fryday
2002). Its description is being prepared for publication.
*Rhizocarpon hensseniae Brodo
Rhizocarpon hochstetteri (K6rber) Vainio s. str. A detailed
discussion of this species is provided by Fryday (2002).
*Rinodina gennarii Bag}.
Spilonema revertens Ny.
*Tephromela atra (Hudson) Hafellner in Kalb
*Tylothallia biformigera P. James & R. Kilias in R. Kilias
Verrucaria amphibia Clemente
Verrucaria degelii R. Sant.
Verrucaria epimaura Brodo
Verrucaria erichsenii Zsch.
*Verrucaria halizoa Leighton
Verrucaria maura Wahlenb. in Ach.
Verrucaria mucosa Wahlenb. in Ach.
Verrucaria sandstedei de Lesd. This species, like V. striatula
listed below, was reported from coastal rocks in Fildago
Island, Washington, by Ryan (1988a, b).
Verrucaria schofieldii Brodo
*Verrucaria Silicicola Fink
Verrucaria striatula Wahlenb. See comment under V. sand-
stedel.
Verrucaria sp. number 5 (dry rock at edge of beach)
Xanthoria candelaria (L.) Th. Fr.
Predaceous Water Beetles (Coleoptera: Adephaga: Dytiscidae, Gyrinidae)
Collected Along the Horton and Thelon Rivers in the Arctic Central
Barrens of Canada
HELENA V. SHAVERDO! and DONNA J. GIBERSON?
‘Department of Entomology, 213 Animal Science/Entomology Building, University of Manitoba, Winnipeg, Manitoba R3T 2N2
Canada
"Department of Biology, University of Prince Edward Island, Charlottetown, Prince Edward Island C1A 4P3 Canada
Shaverdo, Helena V., and Donna J. Giberson. Predaceous water beetles (Coleoptera: Adephaga: Dytiscidae, Gyrinidae) col-
lected along the Horton and Thelon rivers in the Arctic Central Barrens of Canada. Canadian Field-Naturalist
118(3): 425-433.
Predaceous water beetles were collected during expeditions along two northern Canadian rivers during 2000 and 2002.
Twelve species of Dytiscidae (including 11 named species and one additional genus identified from a larva) and one species of
Gyrinidae are recorded from 20 sites along the Horton and Thelon rivers in the Central Barrens area of the Canadian Arctic.
These records represent an extension of the distributions of four species to the northeast in the Northwest Territories (NWT),
and two species to the northwest in Nunavut (NU). Oreodytes sanmarkii is reported for NWT and for the mainland of NU
for the first time. //ybius erichsoni, Hydroporus geniculatus, and Gyrinus opacus are reported for NU for the first time. Five
species were recorded for the first time from the Southern Arctic ecozone, and one from the Taiga Shield ecozone. The
majority of specimens were collected in habitats that were consistent with those previously known for each species.
Key Words: Insecta, Coleoptera, Adephaga, Dytiscidae, Gyrinidae, predaceous water beetles, faunistics, river, Northwest
Territories, Nunavut, Arctic Central Barrens.
The Central Barrens area of the Canadian Arctic is
a vast and very sparsely populated area dominated by
arctic tundra, scattered clumps of taiga vegetation,
large lakes, and rivers. The inaccessibility of the region
has meant that the area has been poorly collected for
all insect groups (Currie et al. 2000), including preda-
ceous water beetles. Only three surveys have been con-
ducted on aquatic Adephaga in the Yukon, Alaska,
and the eastern Canadian Arctic (Alarie and Maire
1991; Larson 1991, 1997), though data on this group
of Coleoptera in arctic and subarctic regions can also
be found in Larson and Roughley (1991), Roughley
(1991), Anderson (1997), and Larson et al. (2000).
Recently a series of expeditions were mounted to ex-
plore the aquatic insect fauna along large river systems
on the treeless barrens of the mainland Canadian Arc-
tic zone (Currie et al. 2000, 2002). The objective of
this paper is to report on the predaceous water beetles
collected from habitats in and near the Horton River
Northwest Territories (NWT) and the Thelon River,
NWT and Nunavut (NU), and present faunistic and
habitat data from the collections.
Methods
Two expeditions were made by DJG and colleagues
from various institutions to northern Canadian rivers
during 2000 and 2002 (Figure 1). Expedition mem-
bers flew in to upstream sections of the Horton and
Thelon rivers in NWT and travelled downriver by
canoe, stopping frequently to sample habitats along the
linear corridor of each river. Aquatic sampling was
carried out using a D-frame kick net with a 200 um
mesh. In flowing water habitats, the net was placed
into the stream and the substrate disturbed by kicking
or by moving rocks by hand, and the dislodged insects
were carried into the net by the current. In areas with
little or no flow, the substrate was disturbed as above,
and then the net was drawn through the water by
hand to catch any dislodged insects. Insects were
sorted alive from the substrate materials on site, and
preserved in 80% ethanol. Predaceous water beetles
were not specifically targeted in the study, but those
that were collected (61 adults and 6 larvae) were exam-
ined by HVS. Collection records were compared to the
maps and distribution table in Larson et al. (2000) to
determine whether any of them represented range ex-
tensions among the provinces and ecozones. The doc-
ument A National Ecological Framework for Canada
(Ecological Stratification Working Group 1995) was
consulted for the classification of Canada’s ecological
regions. Collecting Permits were obtained from the
Aurora Research Institute (Inuvik, NWT) and the
Nunavut Research Institute (Iqaluit, NU) to carry out
the research. Voucher specimens have been deposited
in the collections of the Wallace Museum (University
of Manitoba) and the Royal Ontario Museum, and in
the private collection of D. J. G.
Study Site and Sampling Regime
The Horton River begins west of Horton Lake, which
is located north of Great Bear Lake in the Northwest
Terriories of Canada (Figure 1). The river, which has
425
426
THE CANADIAN FIELD-NATURALIST
Vol. 118
Horton River
68°.
127° Tanptalase 123° 121°
Thelon River
Thelon Game"
* Sanctuary \
ynaeunn
_souloyuse| ISOMYYON
105°W 100°W
FiGureE 1. Location of study area (A), including the Horton River (B) and Thelon River (C) showing sample sites. The fine
dashed line indicates the watershed boundary upstream of the lowest sampled site for both watersheds. The grey
border on the Thelon Watershed map indicates the boundaries of the Thelon Game Sanctuary. Site co-ordinates are
given in Table 1.
a drainage basin area of approximately 26 680 km?
and a total length of = 800 km, runs entirely in the
Southern Arctic Ecozone. Expedition members col-
lected over a 700 km stretch of the river from Horton
Lake to the Arctic Ocean. The river flows over lime-
stone-dominated substrates in its upper reaches, where
it is characterized by relatively high pH (>8.0) and spe-
cific conductance (>150 uS/cm). In its lower reaches,
the river flows through the Smoking Hills, a region
containing lignite and magnesium deposits which spon-
taneously ignite when exposed to air (for example,
during bank slumping during summer). These result
in “smoke holes” as smoke pours from places where
the coal is burning underground, and the water drain-
ing these sites is profoundly affected by the geology.
Tributaries and ponds in this region were highly acidic
(some with pH values < 2.5), and acid runoff in this
area resulted in a decline in river pH to approximately
neutral values. The river is clear and swift-flowing for
most of its length, but becomes muddy and meander-
ing in its lower portion. Sampling was carried out in
37 sites on or near the river between 17 July and 8 Au-
gust 2000. Predaceous water beetles were collected
from 5 of the 37 sites along the river, corresponding to
sampling sites 8, 11, 14, 18, and 23 of the larger Hor-
ton River survey; all were located in the middle sec-
tion, which was clear and swift-moving (Figures 1b,
2; see Table 1 for descriptions of each site).
The Thelon River begins near Lynx Lake, to the
east of Great Slave Lake (Figure 1). The river flows
= 900 km from Lynx Lake to Baker Lake (which exits
via Chesterfield Inlet to northern Hudson Bay to the
east) and drains a total area of = 240 000 km?. The
upper portions of the Thelon River are in the Taiga
Shield ecozone, then the river flows into the Southern
Arctic ecozone. Expedition members flew into the
junction of the Hanbury and Thelon rivers, and col-
lected along a 300 km stretch of the Thelon River
located within the bounds of the Thelon Game Sanc-
tuary (Figure Ic). The part of the river covered in this
survey (i.e., upstream of Beverly Lake, NU) drains
an area of 71 470 km. The river corridor upstream of
the study area consists of large numbers of lakes, water-
falls, and rapids, but in the study area itself, the river
meanders over an ancient glacial lake bottom. At this
point, the river is wide and slow moving and dominat-
ed by sandy or sand/silt-embedded cobble substrates.
Surrounding relief is very low except in a few spots,
2004
Horton Site 8
one
SHAVERDO and GIBERSON: PREDACEOUS WATER BEETLES IN ARCTIC
Horton Site 11
FIGURE 2. Study sites along the Horton River where predaceous water beetles were collected, July/August 2000 (compare to
Figure 1B for site locations).
where low hills, boulders, and more rapid flow can be
found. Most of the river flows through open tundra,
but a small stretch in the upper third of the study area
(= 65 km) is located in a remnant spruce and larch
forest known as the “Thelon Oasis”. The pH and spe-
cific conductance values were quite low, especially in
comparison with the Horton River, with pH values gen-
erally around 6.0, and specific conductance values
= 10 uS/cm for main river sites. pH and conductivity
values for tributaries and tundra pools were more
variable, however. Sampling was carried out at 34 sites
on or near the river between between 29 June and 11
July 2002. Predaceous water beetles were collected
from 15 of the 34 sites, representing a combination
of river and pool sites corresponding to sites 1, 3, 4,
Gy TS OMI lor slSeil9) 22-26::27.) 50and 32-oftthe
larger Thelon River survey (Figures Ic, 3; see Table
1 for descriptions of each site).
Results and Discussion
Oreodytes laevis (Kirby) and O. sanmarkii (Sahlberg)
were the two most common species found in our north-
em rivers survey, and were also the only species found
in both rivers (Table 1). Oreodytes laevis accounted
for 26 of the 61 adults collected (> 40%) and was found
in eight of the 20 sites where water beetles were found.
428 THE CANADIAN FIELD-NATURALIST Vol. 118
_ Thelon Site 7
FiGuRE 3a. Study sites along the upper reaches of the Thelon River where predaceous water beetles were collected, July/
August 2000 (compare to Figure 1C for site locations).
2004 SHAVERDO and GIBERSON: PREDACEOUS WATER BEETLES IN ARCTIC 429
Thelon Site 18 i Thelon Site 19
yA
Thelon Site 30
FIGURE 3b. Study sites along the lower reaches of the Thelon River where predaceous water beetles were collected, July/August
2000 (compare to Figure Ic for site locations).
430
TABLE |. Distribution and abundance of predaceous water beetles collected along the Horton and Thelon Rivers. All species
were collected in the main branch of the rivers except where specifically indicated. All species were in the family Dytisci-
THE CANADIAN FIELD-NATURALIST
dae except Gyrinis opacus which was in the family Gyrinidae.
Site
Coordinates / Date Site Details
Horton River, NWT
8
67°59°24.5"N
123°13°55.5°W
20 July 2000
68°09°29"N
123°22°44.9"W
22 July 2000
68°23°31.5°N
123°38°03.4°W
23 July 2000
68 39°3.18°N
124°08°53.0"W
25 July 2000
68°44’ 19.9"N
124°59°0.8°W
28 July 2000
Thelon River, NWT
1
13
16
18
63 38°04.8"N
104°32°18.6"W
29 June 2002
63 42°04.4”"N
104°25’26.6" W
30 June 2002
63 48’22°N
104°18’21.1"W
30 June 2002
63°49’58.4"N
104°06°20.9"W
1 July 2002
63°55°02.7"N
103°56’59.5°W
1 July 2002
64°02’ 13.2”N
103°51°41.8°W
2 July 2002
64°17°01.8"°N
103°33°22.4”"W
3 July 2002
64°19" 18.6”N
103°19715.7°W
4 July 2002
64°17°56.2”N
102°43°20.6"W
5 July 2002
cobble dominated riffle and shore section,
where river slowed and flowed through a
broad valley; pH: 8.3; conductivity:
150 wS/cm; temp.: 15°C
slow, weedy shoreline area along
the main channel of the river (fill
in from logbook); pH: 8.2;
conductivity: 180 uS/cm; temp.: 10.5°C
backwater zone and a riffle, from a portion
of the river in a narrow valley surrounded
by high limestone cliffs; pH: 8.2;
conductivity: 180 uS/cm; temp.: 12°C
the river is a series of very shallow
flats and riffles; temp.: 12°C
canyon/white-water area of the river, deep
bedrock pools and fast riffles; at camp spot
no obvious riffles though water moving very
fast; sampled from shore; temp.: 17°C
relatively slow and wave washed section near
shore, in silt/sand embedded cobble; pH: 6.2;
conductivity: 10 uS/cm; temp.: 11°C
rocky shore with fairly strong current,
and in backwater pools behind large
boulders; pH: 6.2; conductivity:
10 wS/cm; temp.: 11°C
slow section near shore, with cobble substrate
embedded in sand and silt; pH: 6.2;
conductivity: 10 uS/cm; temp.: 10.5°C
submerged grasses in slow current near
shore, 10 m upstream of a tributary entering
from the south; pH: 6.2; conductivity:
40 uS/cm; temp.: 14°C
cobble and silt substrate near shore where
main river narrowed and became swift
flowing, even near shore; pH: 6.2;
conductivity: 10 uS/cm; temp.: 11°C
at Hornby Point; well embedded cobble
in fast, shallow riffle near shore; pH: 6.1;
conductivity: 10 uS/cm; temp.: 12°C
cobble substrate in fast water in main
channel, plus slower water near shore;
pH: 6.3; conductivity: 30 uS/cm; temp.: 13°C
unnamed tributary entering Thelon River from
forest to the north; riffle with large clean cobble
substrate; pH: 7.6; conductivity: 40 uS/cm;
temp.: 16°C
river wide and lake-like; wave-washed area,
in cobble substrate well embedded in sand;
pH: 6.3; conductivity: 10 uS/cm; temp.: 13.5°C
Species
Oreodytes laevis
(Kirby)
Oreodytes sanmarkii
Sahlberg
Oreodytes sanmarkii
Oreodytes laevis
Oreodytes sanmarkii
Oreodytes sanmarkii
Oreodytes sanmarkii
Oreodytes laevis
Oreodytes sanmarkii
Oreodytes laevis
Oreodytes laevis
Hygrotus novemlineatus
(Stephens)
Oreodytes laevis
Stictotarsus griseostriatus
(DeGeer)
Oreodytes laevis
Stictotarsus griseostriatus
Oreodytes sanmarkii
Oreodytes laevis
Vol. 118
Specimens |
1°
ie)
lo
2c¢c
lo
ilxe}
2c¢c
oil ©
2004
SHAVERDO and GIBERSON: PREDACEOUS WATER BEETLES IN ARCTIC
43]
TABLE | (continued). Distribution and abundance of predaceous water beetles collected along the Horton and Thelon Rivers.
All species were collected in the main branch of the rivers except where specifically indicated. All species were in the fami-
ly Dytiscidae except Gyrinis opacus which was in the family Gyrinidae.
Site
19 64°10°46.1°N
102°36°58.1"W
6 July 2002
23 64°11°05.4"N
102°19°06.9° W
7 July 2002
Thelon River, NU
26 64°19713.2”°N
101°50’11.1°W
8 July 2002
27 64°19’ 13.2”N
101°50°11.1"W
8 July 2002
30 64°26°15°N
101°43°55.1"W
9 July 2002
64°32°25.2”N
101°24°48.9°W
10 July 2002
Coordinates / Date Site Details
small brown-water tundra pools above the
river on north, pools draining to each other
and seeping to the river; overhanging vegetation,
undercut banks, stony bottom; pH: 6.0;
conductivity: 20 uS/cm; temp.: 14°C
unnamed tributary seep entering the river
from the north and small brown-water tundra
pools surrounded by willows, shorelines with
sphagnum and grass; pH: 5.7; conductivity:
50 wS/cm; temp.: 9°C
unnamed tributary entering the river from the
north; cobble substrate in riffle area of the stream;
pH: 6.5; conductivity: 10 uS/cm; temp.: 11°C
small brown-water tundra pond beside site 26;
much submerged and decaying vegetation (grass);
pH: 6.0; conductivity: 10 uS/cm; temp.: 15°C
large tundra pond on southern bank above the
river, with overhanging willows and soft bottom
substrates; pH: 6.0; conductivity: 10 uS/cm;
temp.: 12°C
unnamed small tributary entering the river
from the south - small pools and seeps between
the pools; overhanging vegetation; pH: 6.2;
conductivity: 20 wS/cm; temp.: 14°C
Species Specimens
Hydroporus appalachius 2d¢0
Sherman DIRE)
Agabus confines 499
(Gyllenhal) il bake
Ilybius erichsoni 1E9
(Gemminger
and Harold)
Agabus sp. DES
Oreodytes sanmarkii 1°
Hydroporus geniculatus lo
Thomson
Ilybius erichsoni lo
2IE3e
Stictotarsus griseostriatus lo
Agabus arcticus ls
(Paykull) 6 29
Rhantus sp. WLR
Gyrinus opacus Sahlberg le
Hydroporus morio 3.99
Aubé
Agabus thomsoni IN Gr Ale.
(Sahlberg)
Note: * L3 — larva of third instar; L2 — larva of second instar.
Eleven specimens of Oreodytes sanmarkii were also
found at eight sites. Stictotarsus griseostriatus (De-
Geer) specimens were collected in three of the sites, but
there was only a single specimen in each collection. The
remaining species were all restricted to a single site
each. Although several specimens of individual species
were often found, for example, the sites with Agabus
confinis (Gyllenhal) and A. arcticus (Paykull) (Table 1).
These collections are range extensions among the
provinces and ecozones of Canada for most of the
species collected, and represent a “filling in of gaps” in
the distributions of many northern species. Because of
logistic difficulties in sampling these interior regions
of the arctic barrens, many previously reported species
distributions have appeared disjunctive, or restricted
to coastal areas (e.g., Larson et al. 2000). For example,
the known ranges of Hydroporus appalachius Sher-
man, Oreodytes laevis, and Agabus confinis are extend-
ed to the northeast within the Northwest Territories,
and those of Agabus arcticus and A. thomsoni Salh-
berg are extended to the northwest within Nunavut.
Oreodytes laevis and Hydroporus appalachius are
widespread in the boreal low arctic zone of the Nearc-
tic, so these records represent an extension into the
Tundra zone. With respect to ecozone distribution, O.
laevis, H. appalachius, and A. confinis are recorded
for the first time from the Southern Arctic ecozone,
and A. confinis is now known from all ecozones of
Canada except the prairies. [/ybius erichsonii (Gem-
minger and Harold) is reported for the first time for
Nunavut, and its known range is extended to the north-
east within the Northwest Territories, and into the
Southern Arctic Ecozone. Ilybius erichsonii has now
been reported from all the ecozones of Canada. Hydro-
porus geniculatus Thomson is a Holarctic species
which occurs in the boreal and alpine zones in north-
western North America. In Canada, it is distributed
throughout most of British Columbia and western
Alberta, and north into the Yukon Territory and Alaska
(Larson et al. 2000), and is reported for the first time
in this study in Nunavut and in the Southern Arctic
ecozone. The present record is an extension of its known
432
distribution far to the northeast, and therefore the
range for this species appears disjunctive. However,
H. geniculatus belongs to the poorly studied nigellus-
group, and revision of the group is needed to clarify
its taxonomic position and distribution. We report the
presence of Oreodytes sanmarkii in the Northwest
Territories and in the Taiga Shield ecozone for the first
time, and the collections along the Thelon River also
represent the first record of the species on the Nunavut
mainland. This Holarctic species was previously known
in Canada from a few sites in northern Yukon and a site
on Southampton Island (NU) (Larson et al. 2000).
Hygrotus novemlineatus (Stephens), Hydroporus morio
(Aubé), and Stictotarsus griseostriatus have been
reported in the Canadian Barrens to the east and west
of the sampled areas, but these collections indicate
that their distributions are more continuous across the
north than previous distribution maps might indicate.
Gyrinus opacus (Gyrinidae) is reported for Nunavut
for the first time, and collections on the Thelon River
may represent the most northeasterly record for the
species (Oygur and Wolfe 1991). However, this record
is in need of confirmation since it is based on study
of a single female specimen.
Most of the species were collected in habitats that
matched those that were previously reported for each
species (e.g., Larson et al. 2000). However, this study
has produced some new and additional data on habi-
tat distributions for several species. Oreodytes laevis
and O. sanmarkii have been reported in rivers, streams,
and along exposed shorelines of cold lakes with little or
no submerged vegetation, and with mineral substrates.
These two species dominated in these types of habi-
tat along the Thelon and Horton rivers. According to
Alarie and Maire (1991; as H. hudsonicus) and Larson
et al. (2000), Hygrotus novemlineatus is circumpolar in
the low arctic region and has been collected in Canada
(near Churchill Manitoba, and in Quebec) in brackish
splash pools (rock-pools) along the coast. However,
in our survey it was collected among dense submerged
grass in slow water current along the shore of the
Thelon River. The species may have relatively wide
habitat preferences, since Nilsson and Holmen (1995)
reported it in Fennoscandia from similar habitats to
the Thelon site, as well as from sandy oligotrophic lake
margins and sparsely vegetated ponds. In the southern
parts of its range, Hydroporus appalachius is usually
found in habitats where there is some water movement,
for example in streams, springs, and the margins of
small lakes (Larson et al. 2000). In Labrador, the
species was collected from a protected shoreline of a
large lake (Larson et al. 2000), and it has been found
in inland pools in the Quebec subarctic region (Alar-
ie and Maire 1991). The habitat in the more northern
parts of its range has not previously been described,
and in this survey, it was found in small tundra pools
that drained into each other before spilling into the
Thelon River.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Acknowledgments
We are grateful to Rob Roughley and Lisa Purcell
for their advice and comments on the manuscript.
Financial support for the collections was provided by
an NSERC operating grant, a UPEI Senate Research
Grant, and a Nature Discovery Grant (National Muse-
ums of Canada) to D. J. Giberson. Lisa Purcell helped
to collect the specimens. Support for the study of the
material was provided by NSERC through a 2001
NATO Science Fellowship to H. V. Shaverdo and an
NSERC operating grant to Rob Roughley. Voucher
specimens have been deposited in the J. B. Wallace
Museum of the University of Manitoba, the Royal
Ontario Museum, and in the private collection of
H. V. S. Collecting permits were provided by the terri-
torial governments through the Aurora Research Insti-
tute in the Northwest Territories and the Nunavut
Research Institute in Nunavut.
Literature Cited
Alarie, Y., and A. Maire. 1991. The dytiscid fauna of Québec
Subarctic (Coleoptera: Dytiscidae). Coleopterists Bulletin
45: 350-357.
Anderson, R. S. 1997. An Overview of the Beetles (Coleop-
tera) of the Yukon. Pages 405-444 in Insects of the Yukon.
Edited by H.V. Danks and J.A. Downes. Biological Sur-
vey of Canada. Monograph series (2), Biological Survey
of Canada (Terrestrial Arthropods). Ottawa. Ontario.
Currie, D. C., D. J. Giberson, and B. V. Brown. 2000. Insects
of Keewatin and Mackenzie. Newsletter of the Biological
Survey of Canada (Terrestrial Arthropods) 19: 48-51.
Currie, D. C., D. J. Giberson, and B. V. Brown. 2002. Insect
biodiversity in the Thelon Wildlife Sanctuary. Newsletter
of the Biological Survey of Canada (Terrestrial Arthro-
pods) 21: 59-64.
Ecological Stratification Working Group. 1995. A National
Ecological Framework for Canada. Agriculture and Agri-
Food Canada, Research Branch, Centre for Land and Bio-
logical Resources Research, and Environment Canada, State
of the Environment Directorate, Ecozone Analysis Branch,
Ottawa/Hull. Report and national map at 1:7 500 000
scale.
Larson, D. J. 1991. A new species of Potamonectes Zim-
mermann (Coleoptera: Dytiscidae) from Labrador. Coleop-
terists Bulletin 45: 280-284.
Larson, D. J. 1997. Dytiscid Water Beetles (Coleoptera:
Dytiscidae) of the Yukon. Pages 491-522 in Insects of the
Yukon. Edited by H. V. Danks and J. A. Downes. Biological
Survey of Canada. Monograph series (2), Biological Sur-
vey of Canada (Terrestrial Arthropods). Ottawa. Ontario.
Larson, D. J., and R. E. Roughley. 1991. Family Dytiscidae.
Pages 62-72 in Checklist of beetles of Canada and Alaska.
Edited by Y. Bousquet. Agriculture Canada Publication
1861/E.
Larson, D. J., Y. Alarie, and R. E. Roughley. 2000. Preda-
ceous Diving Beetles (Coleoptera: Dytiscidae) of the Nearc-
tic Region, with emphasis on the fauna of Canada and Alaska.
NRC Research Press, Ottawa, Ontario, Canada. 982 pages.
Nilsson, A. N., and M. Holmen. 1995. The aquatic Adephaga
(Coleoptera) of Fennoscandia and Denmark. II. Dytiscidae.
Fauna Entomologica Scandinavica 32: 1-192.
2004 SHAVERDO and GIBERSON: PREDACEOUS WATER BEETLES IN ARCTIC 433
Oygur, S., and G. W. Wolfe. 1991. Classification, distribution, Roughley, R. EK. 1991. Family Gyrinidae. Pages 72-73 in
and phylogeny of North American (north of Mexico) spe- Checklist of beetles of Canada and Alaska. Edited by Y.
cies of Gyrinus Miiller (Coleoptera: Gyrinidae). Bulletin Bousquet. Agriculture Canada Publication 1861/E.
of the American Museum of Natural History 207: 1-97.
Received 2 June 2003
Accepted 14 July 2004
Notes
Collapsing Burrow Causes Death of a Eurasian Beaver, Castor fiber
Liat R. THOMSEN!, FIONA SHARPE2, and FRANK ROSELL?
' Department of Zoology, University of Aarhus, Denmark
2 School of Biology, University of St Andrews, Fife, Scotland
3 Faculty of Arts and Sciences, Department of Environmental and Health Studies, Telemark University College, N-3800 Bo
i Telemark, Norway
Thomsen, Liat R., Fiona Sharpe, and Frank Rosell. 2004. Collapsing burrow causes death of a Eurasian Beaver, Castor
fiber. Canadian Field-Naturalist 118(3): 434-435.
The death of a Eurasian Beaver Castor fiber caused by a collapsing burrow in southeast Norway is reported. Two days of
heavy rainfall had presumably caused the burrow to collapse, suffocating the animal.
Key Words: Beaver, Castor fiber, collapsing burrow, southeast Norway.
Several causes of death have been reported for
Eurasian Beavers (Castor fiber) (Rosell et al. 1996;
Nolet et al. 1997), but to our knowledge this is the
first report of a beaver killed due to a collapsing bur-
row. The beaver was an adult solitary male (21.5 kg
and 5 years old; age was determined by examining
annual cementum and dentine layers of the first molar
(van Nostrand and Stephenson 1964)). His mate died
two months earlier, probably due to old age (18 years
old). The animal was one of several radio tagged
beavers that were followed during a field study in
spring and summer 2000 in Telemark County, south-
east Norway (59°25'N, 09°03'E) (see Campbell 2000).
On the evening of 14 July 2000 it was noted that the
pulse interval of the radio signal had increased. The
signal is inversely related to the body temperature of
the animal (Alterra 1999), thus a higher pulse interval
indicated that the beaver had died. The dead beaver
was located in the main part of a partly collapsed bur-
row (assessed to be relatively new), which was exca-
vated four days later in order to find and retrieve the
carcass (Figure 1).
Beavers dig burrows where banks are sufficiently
high (Wilsson 1971; Zurowski 1992). A burrow usu-
ally consists of a single living chamber, a water basin,
and a tunnel with exit below the water level (Wilsson
1971). The beaver was lying in the chamber (1 m long
and 70 cm wide) of the collapsed burrow, facing to-
wards the exit. The chamber was situated 210 cm from
the water’s edge, 80 cm below the surface of the
riverbank, and 60 cm above the current water level.
Apparently the ceiling of the chamber had collapsed
on top of the beaver causing the death of the animal,
presumably by suffocation. There was loose sand along
the flanks of and underneath the body of the dead
beaver. The last 10 cm of the beaver’s tail was bent
downwards into the sand and the right hind foot was
crouched as if the beaver had been attempting to dig
with it. The beaver had no external injuries and seemed
to be in good condition.
of a partly collapsed burrow.
The burrow was dug in sandy soil. In the week prior
to the discovery of the beaver there had been two days
with heavy rainfall in the area with 30.8 mm and 24.6
mm of rain, respectively (data from the Norwegian
Meteorological Institute).
We conclude that the combination of heavy rainfall
and a sandy soil had caused the burrow to collapse,
therefore causing the death of the beaver. How preva-
lent this cause of death is in beavers is unknown. How-
ever, we expect that more field studies using radio
telemetry, in areas where beavers dig burrows, could
clarify this issue.
434
2004
Acknowledgments
We thank Frode Bergan for help with excavating
the beaver and Inger Hanssen-Bauer for providing the
weather data. The study was financially supported by
Telemark University College. The experiments comply
with the current Norwegian law, the country in which
they were performed.
Literature Cited
Alterra. 1999. Alterra (IBN/DLO) P.O. Box 23. 6700 AA
Wageningen. Netherlands.
Campbell, R. D. 2000. Territoriality in the European Beaver,
Castor fiber. MSc thesis, School of Biological Sciences,
University of East Anglia, Norwich, England.
Nolet, B. A., S. Broekhuizen, G. M. Dorrestein, and K.
M. Rienks. 1997. Infectious diseases as main factors of
NOTES
435
mortality to beavers Castor fiber after translocation to the
Netherlands. Journal of Zoology, London 241: 35-42.
Rosell, F., H. Parker, and N. B. Kile. 1996. Causes of mor-
tality in beaver (Castor fiber & canadensis). Fauna 49:
34-46 [In Norwegian with English summary].
van Nostrand, F. C., and A. B. Stephenson. 1964. Age deter-
mination for beavers by tooth development. Journal of
Wildlife Management 28: 430-434.
Wilsson, L. 1971. Observations and experiments on the ethol-
ogy of the European beaver (Castor fiber L.). Viltrevy 8:
_ E266:
Zurowski, W. 1992. Building activity of beavers. Acta
Theriologica 37: 403-411.
Received 26 November 2002
Accepted | November 2004
Frequency of Tail Breakage of the Northern Watersnake, Nerodia
sipedon sipedon
KENNETH D. BOWEN! :2
'Department of Biology, Central Michigan University, Mt. Pleasant, MI 48859 USA
Present Address: 709 Ringold Street, Boone, Iowa 50036 USA
Bowen, Kenneth D. 2004. Frequency of tail breakage in the Northern Watersnake, Nerodia sipedon sipedon. Canadian
Field-Naturalist 118(3): 435-437.
I noted the frequency of broken tails of Northern Watersnakes, Nerodia sipedon sipedon, in the Beaver Archipelago of North-
eastern Lake Michigan. Overall, 10% (22 of 220) of captured snakes had broken tails. This value is similar to published values
for closely related snakes but is smaller than those reported for another Nerodia sipedon sipedon population. Unlike some
previously published studies, the frequency of injured tails was not greater for females or lesser for first-year snakes. The mech-
anism behind the injury frequency observed here and the reason for differences between this and other studies are unknown.
Key Words: Beaver Archipelago, Nerodia sipedon sipedon, Northern Watersnake, tail breakage, Michigan.
The frequency of tail injuries in a lizard or snake
population was at one time considered to be a useful
index of the predation pressure on that population be-
cause tail autotomy and breakage (Mendelson 1992)
are thought to be important defense mechanisms (re-
viewed in Arnold 1988). More recently, theoretical and
empirical tests of this hypothesis have led to the asser-
tion that loss or injury of the tail may instead be related
to predator inefficiency or alternative sources of mor-
tality and that careful investigation must be undertaken
to determine the mechanism behind observed injury
frequencies (Schoener 1979; Medel et al. 1988). While
such data must indeed be interpreted with caution, re-
porting the frequency of tail injury in study populations
can be useful when combined with demographic data
(Arnold 1988), for example in forming hypotheses re-
garding sex or size-based differences in anti-predator
mechanisms (Fitch 2003).
Several researchers have reported the frequency of
tail injuries in populations of snakes. Fitch (1999) found
that the frequency of tail breakage increased with the
age/size of individuals in a Kansas population of Nero-
dia s. sipedon, the Northern Watersnake. More specif-
ically, the frequency of female tail breakage ranged
from 21.2 to 44.5%, and the frequency of male tail
breakage ranged from 6.5 to 25% in increasing body
size categories. Willis et al. (1982) reported that fe-
male Eastern Garter Snakes (Thamnophis sirtalis) and
Northern Ribbon Snakes (Thamnophis sauritus) had a
higher incidence of tail loss than males (13% versus
6%, and 12% versus 7%, respectively) and that tail loss
was more prevalent in larger size classes. However, nei-
ther trend was statistically significant in populations
of Butler’s Garter Snake (Thamnophis butleri). Fitch
(2003) found that tail breakage was more common for
female T. sirtalis (16.7%) than for males (10.3%) and
more common for large snakes (13.7%) than for first-
year snakes (2.42%). In general, females and larger
snakes appear more likely to have broken tails.
I studied the frequency of broken tails of the North-
ern Watersnake in the Beaver Archipelago of north-
eastern Lake Michigan during the summers of 2000
and 2001. I captured snakes from Beaver Island
(45°41.26'N, 85°30.34'W), Garden Island (45°48.28'N,
85°29.41'W), High Island (45°43.88'N, 85°39.54'W),
and Hog Island (45°48.39'N, 85°22.15'W). Upon cap-
436
THE CANADIAN FIELD-NATURALIST
TABLE 1. Chi-square contingency table for comparison of the frequency of tail breakage among male, female, and first-year
Nerodia sipedon sipedon in the Beaver Archipelago of Lake Michigan. The calculated x? was 0.23 (critical x7 = 5.99, df =2).
Class Number of Number of
injured snakes uninjured snakes Total % Injured
Male 7 55 62 AES
Female 13 120 133 9.8
First-year 2, 23 25 8.0
Totals 22 198 220 10.0
ture, I brought snakes to the laboratory where I then
measured snout-vent length (SVL) and noted the tail
condition and sex of each individual. I released all
snakes at the point of capture as soon as possible
after processing. I pooled snakes from all islands and
calculated the overall percentage of snakes with tail
breaks. I also compared the frequency of broken tails
among males, females, and unsexed first-year snakes,
and among three capture locations (Beaver Island Lake
Michigan shoreline, Beaver Island interior lake, and
Garden Island Lake Michigan shoreline) within sexes
using Chi-square contingency table analysis. I hypoth-
esized that females would have a higher frequency of
tail breakage than males and that first-year snakes
would have a lower frequency of tail breakage than
both males and females.
Two hundred and twenty snakes were captured from
the four islands. Beaver Island produced 153 snakes,
Garden Island 55, High Island 1, and Hog Island 11
snakes. Captured snakes ranged in size from 149 to
860 mm SVL with a mean of 478.2 mm and a stan-
dard deviation of 164 mm. In all, 10% (22) of the
snakes had broken tails. There was no statistically sig-
nificant difference in the frequency of tail breakage
among males, females, and first-year snakes (x7 = 0.23,
critical y? = 5.99, df = 2; Table 1). Within males, there
was no statistically significant difference in the fre-
quency of tail breakage among capture sites (x? = 0.33,
critical y7 = 5.99, df =2; Table 2). However, females
captured on the Lake Michigan shoreline of Garden
Island had a higher frequency of tail breakage than
those captured elsewhere (x7 = 8.9, critical y? = 5.99,
dfi=2; Table3):
My data do not closely match those of any pre-
vious studies. The overall frequency of tail breakage is
similar to that reported by Willis et al. (1982). How-
ever, unlike the populations of N. s. sipedon and T.
sirtalis studied by Fitch (1999; 2003), and the popu-
lations of T. sirtalis and T. sauritus studied by Willis
et al. (1982), the frequency of broken tails is not great-
er for females in the Beaver Archipelago overall (al-
though it is greater if only Garden Island is consid-
ered). Furthermore, first-year snakes in the Beaver
Archipelago do not appear to have a lower frequency
of tail breakage than larger snakes. The 7. butleri pop-
ulations of Willis et al. (1982) appear to be similar to
my snakes in the lack of common patterns of tail break-
age. The sample size (287) for T. butleri in that study
is similar to my own, while the sample sizes of the 7.
sirtalis, T. sauritus and N. s. sipedon studies are con-
siderably larger. This suggests that the ability to detect
patterns in the frequency of tail injuries in snake pop-
ulations may be dependent upon sample size.
TABLE 2. Chi-square contingency table for comparison of the frequency of tail breakage of male Nerodia sipedon sipedon
among capture sites in the Beaver Archipelago of Lake Michigan. The calculated x? was 0.33 (critical y° = 5.99, df =2).
Capture Number of
site
Beaver Island Lake Michigan shoreline
Beaver Island interior lakes
Garden Island Lake Michigan shoreline
Totals
mee
injured snakes
Number of
uninjured snakes Total % Injured
ils) 17 11.8
20 22 9.1
18 21 14.3
53 60 Hike 7/
TABLE 3. Chi-square contingency table for comparison of the frequency of tail breakage of female Nerodia sipedon sipedon
among capture sites in the Beaver Archipelago of Lake Michigan. The calculated x7 was 8.9 (critical y* = 5.99, df =2).
Capture site Number of
injured snakes
Beaver Island Lake Michigan shoreline
Beaver Island interior lakes
Garden Island Lake Michigan shoreline
Totals
=
wlnony sp
Number of
uninjured snakes Total % Injured
60 64 6.2
34 36 SD)
21 28 25.0
TS 128 10.1
2004
Fitch (2003) suggested that the frequency of tail
breakage should be expected to vary among different
study sites based on the presence of predators and
availability of escape cover. Such factors may explain
the differences in overall frequency of tail breakage
between this and other studies and between islands in
the Beaver Archipelago within females. Fitch (1999)
also suggested that NV. s. sipedon individuals with great-
er mass are more likely to have broken tails because
they whirl repeatedly in an attempt to escape when
grasped by a predator. Greater mass makes tail break-
age more likely when this whirling motion is employed.
The smaller mass of first-year snakes, the smaller mass
of male N. s. sipedon in comparison to females of the
same age (Fitch 1999), and the fact that broken tails
may potentially damage the hemipenes of males all sug-
gest that these groups should have lower frequencies
of tail breakage than large snakes and females, res-
pectively, regardless of locality. These patterns were
not clear in this study or in the populations of 7:
butleri studied by Willis et al. (1982).
Sample size may be the critical factor in the dis-
crepancy between studies. The two studies that did
not show common patterns in tail breakage had rela-
tively small sample sizes. A large sample size may be
necessary for two reasons: (1) the patterns are real
but the categorical nature of the data (break or no
break) requires that large samples be collected for a
pattern to be detectable, or (2) the patterns are not
real but stem from the fact that any difference, no
matter how small, can be statistically significant if
the sample size is large enough (Johnson 1999). The
general similarity of patterns of tail breakage across
studies with large sample sizes suggests that the first
reason may be the case. However, discrepancies among
studies underscore the need for more research in this
area. Researchers should continue to record and
report the frequency of tail breakage in populations
of lizards and snakes, but more carefully designed
studies that attempt to determine the direct causes
and consequences of tail breakage are needed (Medel
et al. 1988). Until such studies are carried out, the
meaning and utility of tail breakage data will remain
speculative.
NOTES
437
Acknowledgements
This research was done as part of a M.S. thesis at
Central Michigan University. I thank my Thesis com-
mittee: James C. Gillingham, Michael J. Hamas, and
David L. Clark. I also thank John W. Rowe for help
and advice in the field and laboratory. E. S. Bowen,
M. F. Haussmann, and two anonymous reviewers pro-
vided valuable comments on earlier drafts. Financial
support was provided by the Central Michigan Uni-
versity Department of Biology, the Central Michigan
University College of Graduate Studies, and the
Central Michigan University Biological Station on
Beaver Island. Animals were collected under MDNR
Cultural and Scientific Collector’s Permit CA 341 is-
sued to J. C. Gillingham. The experimental protocol
was approved by the Central Michigan University In-
stitutional Animal Use and Care Committee (approval
number 02-06).
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Johnson, D. H. 1999. The insignificance of statistical signifi-
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Accepted 4 November 2004
438
THE CANADIAN FIELD-NATURALIST
Vol. 118
The Heather Vole, Genus Phenacomys, in Alaska
S. O. MACDoNALD!:3, AMY M. RUNCK?, and JosEPH A. COOK>*”
1P.O. Box 58, Gila, New Mexico 88038-0058 USA
Biological Sciences Department, Idaho State University, Pocatello, Idaho 83209-8007 USA
3Museum of Southwestern Biology, University of New Mexico, Albuquerque, New Mexico 87131 USA; Corresponding
author, e-mail cookjose @unm.edu
MacDonald, S. O., Amy M. Runck, and Joseph A. Cook. 2004, The heather vole genus Phenacomys, in Alaska. Canadian
Field-Naturalist 118(3): 438-440.
Four specimens of heather vole (genus Phenacomys) collected in the coastal mountains of Southeast Alaska document the
first Recent records of this vole in Alaska. Alternative hypotheses on the relationship of these newly-discovered populations
to extant and historical populations are outlined, and additional studies proposed.
Key Words: Heather vole, Phenacomys sp., Southeast Alaska.
Since publication of a synopsis of the land mammal
fauna of Southeast Alaska (MacDonald and Cook
1996), new field and laboratory studies of the mam-
mals of this region have resulted in new perspectives
on the zoogeography of the North Pacific Coast (Con-
roy et al. 1999; Cook and MacDonald 2001; Cook et
al. 2001). In our 1996 publication, we speculated that
several mammal species found on the eastern side of
the coastal mountains in Canada may occur along the
Alaska coast. One species, the heather vole (Phena-
comys intermedius), had previously been recorded
within 2 km of the southern Alaska border in the sub-
alpine near Salmon Glacier in British Columbia (ap-
proximately 56.17° N, 130.03° W), and Nagorsen and
Jones (1981) reported its occurrence in the Chilkat Pass
north of Haines and Southeast Alaska. Subsequent
trapping efforts in Alaskan mountains near Salmon
Glacier and elsewhere along the mainland coast result-
ed in the capture of four specimens of this vole (Table
1) from two widely separate localities (Figure 1).
These specimens, deposited at the University of Alaska
Museum (UAM), constitute the first documented rec-
ords of extant populations of heather vole in Alaska.
On 11 August 1996, we captured a single heather
vole (UAM 42371) above timberline in the glacially-
isolated Chilkat Range at the northern end of South-
east Alaska near Excursion Inlet, Glacier Bay National
Park (58.41° N, 135.43° W; elevation approximately
900 m). Also recorded in this alpine area were Sorex
monticolus and melanistic Marmota caligata.
In 1999, three heather voles were collected from
the far southern end of mainland Southeast Alaska,
approximately 400 km south of the 1996 Glacier Bay
record. On 23 September 1999, two male (UAM 64239,
UAM 64240) and one female (UAM 50000) heather
voles were found in subalpine habitat along the Titan
Trail in the Reverdy Mountains, approximately 10
km north of Hyder, Alaska (approximately 55.83° N,
130.03° W; elevations between 1128-1220 m). Synap-
tomys borealis was also sampled at this site.
The distribution of the heather vole is poorly known
throughout western North America (Figure 1) and geo-
graphic variation has been little studied (for overviews
see McAllister and Hoffmann 1988; Nagorsen 1990;
Musser and Carleton 1993). Some authorities (Ander-
son 1942; Cowan and Guiguet 1965; Peterson 1966;
Hallett 1999) recognized the distinctiveness of western
populations (P. intermedius of westcentral British
Columbia south to California and New Mexico) and
separated them from P. ungava in the north and east
(southern Yukon Territory and northern British Colum-
bia eastward to Newfoundland) (McAllister and Hoff-
mann 1988; George 1999); others considered all to
comprise a single species (Crowe 1943; Youngman
1975; Honacki et al. 1982; Nagorsen 2004). Hall (1981)
speculated that intermedius may be a composite of two
or three allopatric species (see McAllister and Hoff-
mann 1988), but the lack of specimens from too few
areas has prevented meaningful progress in resolving
the problem. Reluctance of this species to enter traps
may be the primary factor limiting sample size and
study materials (McAllister and Hoffmann 1988).
The taxonomic affinities of newly-discovered popu-
lations of heather vole in Southeast Alaska are not
immediately evident. Based on the map provided by
Hall (1981: 787, as adjusted by McAllister and Hoff-
mann 1988 and Nagorsen 2004), Alaska’s southern-
most heather voles could share close kinship with the
P. i. intermedius group of “western” heather voles
occurring in the coastal mountain ranges of adjacent
British Columbia. Heather voles from northern South-
east Alaska, on the other hand, might possibly have
connection with the “eastern” populations (as P. unga-
va mackenzii) in northwestern British Columbia and
southern Yukon Territory. Both of these scenarios pre-
sume relatively recent colonization from inland pop-
ulations following the (ongoing) retreat of the last
major glaciation from the region. A similar scenario
has been proposed for American Marten (Martes amer-
icana) (Stone et al. 2002) and other mammals (Cook
438
2004 NOTES 439
TABLE |. Summary of specimen data from collection notes and records at the University of Alaska Museum (UAM). Alaska
Frozen Tissue Number refers to the cryogenic collection administered by UAM. Measurements and abbreviations are as
follows: total length-tail length-hind foot-ear from notch (in millimeters)=mass (in grams); t = testes (length and width in
mm), plsc = number of placental scars on right and left uterine horn; F = female, M = male.
Alaska Frozen Tissue Number
UAM Catalog Number
Sex (Reproduction) Measurements
42371 17262
50000 30176
64239 30178
64240 30179
et al. 2001). An alternative hypothesis, however, 1s that
one or more of these populations are remnants of a
former coastal population whose origin in the region
preceded the last glacial advance (MacDonald and
Cook 1996; Fleming and Cook 2002).
The discovery of late Pleistocene fossil remains of
Phenacomys in limestone cave deposits in the Alex-
ander Archipelago of Southeast Alaska has added his-
torical dimension to these hypotheses. Preliminary
Chilkat River
Gulf
of Alaska
LOCALITY KEY
@ Chilkat Range
@ Reverdy Mts.
On Your Knees
Cave fossil site
M (t=2X3) 120-31-19-11=19
F (plsc: 4R, OL) 156-37-18-14=33.9
M (t=3X2) 129-32-17-13=22.8
M (t=3X2) 115-26-16-10=14.6
analyses of thousands of rodent teeth recovered from
On Your Knees Cave at the extreme northwest corner
of Prince of Wales Island in Southeast Alaska (Figure
1) (Heaton 1995, 2004*; Heaton and Grady 2003) in-
dicate that Heather Voles had been present in the vicin-
ity of this site during the Middle Wisconsin up to the
start of, but not during or following, the last glacial
maximum (between about 24 000 to 13 000 years
ago) (Heaton 2004*; Heaton and Grady 2003). Other
% CANADA
Sc
,
Za
4p
Stikine River
Unuk River
Ficure 1: Localities of specimens of Phenacomys in Southeastern Alaska from Recent and Late Pleistocene sites. Inset range
map modified according to McAllister and Hoffman (1988) following subspecific designations suggested by George
(1999) and Hallett (1999).
440
rodent remains discovered in these same pre-glacial
deposits were Brown Lemming, Lemmus trimucro-
natus, a species thought absent from the region but
recently discovered by UAM in the mountains near
Haines, and the Hoary Marmot, Marmota caligata, a
species now restricted to mainland localities.
How the new records of Phenacomys from South-
east Alaska relate to extant and historical populations
has yet to be determined. Analyses of samples using
modern molecular and morphological techniques could
help clarify these relationships and provide a test of
alternate hypotheses on the origin and dynamics of
the region’s biota. Clearly, more samples from more
localities are needed. An expanded effort to excavate
fossils throughout the region, along with a continua-
tion of survey efforts to further define the current
distribution of Phenacomys and other mammals that
share a deep history in the region (e.g., Lemmus,
Marmota), as well as provide adequate samples for
assessment, are needed. The alpine zone of Southeast
Alaska is virtually unexplored and future inventories
need to target sites above treeline along the mainland
as well as on the more mountainous islands in the
Alexander Archipelago.
Acknowledgments
A number of individuals assisted with field work
that led to these new records including C. T. Seaton,
Able Duffy, Joni Reese, Mike Brown, Guillermo D’Eha,
and John Chythlook. Brandy Jacobsen, Gordon Jarrell,
and Dusty McDonald of the University of Alaska Mu-
seum provided specimen information. Thanks also to
David Nagorsen for reviewing an early draft of this
paper. This research was funded by the United States
Fish and Wildlife Service, United States Department of
Agriculture Forest Service, Alaska Cooperative Fish
and Wildlife Research Unit, and the National Science
Foundation (DEB0196095 & DEB9981915).
Documents Cited [marked * in text citations]
Heaton, T. H. 2004. Ice Age paleontology of Southeast Al-
aska. http://www.usd.edu/esci/alaska/index.html. 3 Decem-
ber 2004.
Literature Cited
Anderson, R. M. 1942. Canadian voles of the genus Phena-
comys with description of two new Canadian subspecies.
Canadian Field-Naturalist 56: 56-60.
Conroy, C. J., J. R. Demboski, and J. A. Cook. 1999.
Mammalian biogeography of the Alexander Archipelago
of Alaska: a north temperate nested fauna. Journal of
Biogeography 26: 343-352.
Cook, J. A., and S. O. MacDonald. 2001. Should endemism
be a focus of conservation efforts along the North Pacific
Coast of North America? Biological Conservation 97:
207-213.
Cook, J. A., A. L. Bidlack, C. J. Conroy, J. R. Demboski,
M. A. Fleming, A. M. Runck, K. D. Stone, and S. O.
MacDonald. 2001. A phylogeographic perspective on
endemism in the Alexander Archipelago of southeast
Alaska. Biological Conservation 97: 215-227.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Cowan, I. M., and C. J. Guiguet. 1965. The mammals of
British Columbia. British Columbia Provincial Museum,
Handbook No. 11, 24 edition: 1-414.
Crowe, P. E. 1943. Notes on some mammals of the southern
Canadian Rocky Mountains. Bulletin of the American
Museum of Natural History 80: 391-410.
Fleming, M. A., and J. A. Cook. 2002. Phylogeography of
endemic ermine (Mustela erminea) in southeast Alaska.
Molecular Ecology 11: 795-808.
George, S. B. 1999. Eastern heather vole, Phenacomys un-
gava. Pages 618-619 in The Smithsonian book of North
American mammals. Edited by D. E. Wilson and S. Ruff.
Smithsonian Institution Press, Washington, D.C., in asso-
ciation with the American Society of Mammalogists. 750
pages.
Hall, E. R. 1981. The mammals of North America. Wiley-
Interscience, New York. 1181 pages.
Hallett, J. G. 1999. Western heather vole, Phenacomys inter-
medius. Pages 617-618 in The Smithsonian book of North
American mammals. Edited by D. E. Wilson and S. Ruff.
Smithsonian Institution Press, Washington, D.C., in associa-
tion with the American Society of Mammalogists. 750 pages.
Heaton, T. H. 1995. Middle Wisconsin bear and rodent re-
mains discovered on Prince of Wales Island, Alaska. Cur-
rent Research in the Pleistocene 12: 92-94.
Heaton, T. H., and F. Grady. 2003. The Late Wisconsin verte-
brate history of Prince of Wales Island, Southeast Alaska.
Pages 17-53 in Ice Cave Faunas of North America. Edited
by B. W. Schubert, J. I. Mead, and R. W. Graham. Indiana
University Press. 400 pages.
Honacki, J. H., K. E. Kinman, and J. W. Koeppl. Editors.
1982. Mammal species of the world: a taxonomic and geo-
graphic reference. Allen Press, Inc. and The Association
of Systematics Collections, Lawrence, Kansas. 694 pages.
MacDonald, S. O., and J. A. Cook. 1996. The land mammal
fauna of southeast Alaska. Canadian Field-Naturalist
110: 571-599.
McAllister, J. A., and R. S. Hoffmann. 1988. Phenacomys
intermedius. Mammalian Species 305: 1-8.
Musser, G. G., and M. D. Carleton. 1993. Family Muridae.
Pages 501-756 in Mammal species of the world: a taxo-
nomic and geographic reference. Edited by D. E. Wilson
and D. M. Reeder. Second Edition. Smithsonian Institution
Press, Washington. 1206 pages.
Nagorsen, D. W. 1990. The mammals of British Columbia:
a taxonomic catalogue. Memoir Number 4, Royal British
Columbia Museum. 140 pages.
Nagorsen, D. W. 2004. The rodents and lagomorphs of Brit-
ish Columbia. Royal British Columbia Museum Hand-
book, Volume 4. University of British Columbia Press,
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Nagorsen, D. W., and D. M. Jones. 1981. First records of
the Tundra Shrew (Sorex tundrensis) in British
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Peterson, R. L. 1966. The mammals of eastern Canada.
Oxford University Press, Toronto. 465 pages.
Stone, K., R. Flynn, and J. Cook. 2002. Post-glacial coloni-
zation of northwestern North America by the forest associ-
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National Museum of Natural History, Publications in
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Received 26 November 2002
Accepted 30 December 2004
2004 NOTES 44]
Extension de l’aire de distribution connue de la Musaraigne fuligineuse,
Sorex fumeus, dans le nord-est du Québec
JEAN-FRANCOIS DESROCHES! et ISABELLE PICARD
' Collége de Sherbrooke, Département des Techniques d’écologie appliquée, 475 du Parc, Sherbrooke, Québec JIK 4K]
Canada
Desroches, Jean-Francois, et Isabelle Picard. 2004. Extension de l’aire de distribution connue de Ja Musaraigne fuligineuse,
Sorex fumeus, dans le nord-est du Québec. Canadian Field-Naturalist 118(3) : 441-442.
La Musaraigne fuligineuse (Sorex fumeus) figure sur la liste des especes de la faune vertébrée susceptibles d’étre désignées
menacées ou vulnérables au Québec. Le 7 juin 1999, nous avons récolté un individu mort en bordure de la riviére Saint-Nicolas,
a Godbout, dans la région de la Céte Nord. Cette observation constitue une extension de l’aire de répartition connue de |’ espéce
d’ environ 200 km vers le nord-est.
Mots-clés : Musaraigne fuligineuse, Sorex fumeus, aire de distribution, Québec.
La Musaraigne fuligineuse (Sorex fumeus) est pré-
sente dans le nord-est de 1’ Amérique du Nord, des
Great Smokies des Carolines au sud jusqu’au centre
de l’Ontario et aux Maritimes vers le nord (Banfield
1977). Au Québec, la mention la plus nordique de
Pespéce se situe a Val-Jalbert, aux abords du lac Saint-
Jean (van Zyll de Jong 1983). Sa répartition connue vers
le nord-est, sur la rive nord du fleuve Saint-Laurent, ne
dépasse guére la riviére Saguenay (van Zyll de Jong
1983; Banfield 1977). Cette musaraigne figure sur la
liste des espéces de vertébrés susceptibles d’étre désig-
nées menacées ou vulnérables au Québec (Beaulieu
1992). Les chercheurs contactés en 1989 n’avaient pas
rapporté de capture récente au Québec (Beaulieu 1992)
mais depuis, elle a été capturée a divers endroits notam-
ment dans le sud de la province (G. Lupien, commu-
nication personnelle).
Le 7 juin 1999, nous avons trouvé un spécimen de la
Musaraigne fuligineuse mort, probablement noyé, en
bordure de la riviére Saint-Nicolas, a environ 100 métres
au sud de la route 138 a Godbout (49°19'10"N,
67°47'24"0), dans la région de la Cote Nord. Lhabitat
a cet endroit est une aulnaie, bordée par une sapiniere
a Bouleau blanc. Aucun autre micromammifere n’y a
été observé. Le spécimen de Musaraigne fuligineuse
a été récolté pour identification. Les mesures ont été
prises sur le spécimen a l’aide d’un vernier a cou-
lisse, par J-F. D. et S. Houde, et elles correspondent a
celles de la Musaraigne fuligineuse (tableau 1). Au
Québec, la Musaraigne fuligineuse peut étre con-
fondue avec la Musaraigne cendrée (Sorex cinereus),
ayant toutes deux de quatre a cing dents unicuspides
visibles, la limite postérieure du foramen infraorbi-
taire antérieure ou prés de la limite entre les molaires
1 et 2, le trou mentonnier situé a la hauteur du proto-
conide de la moiaire 1, et la mandibule dépourvue de
foramen postmandibulaire (Maisonneuve et al. 1997).
Elle s’en distingue toutefois par certaines mesures du
crane et du corps (tableau 1). Le spécimen a malheu-
reusement été perdu quelques jours plus tard, jeté par
erreur avec d’autres micromammiferes morts, mais les
mesures prises confirment son identification.
Cette observation constitue une extension d’aire de —
Vespece de 200 km vers le nord-est, soit a partir de
V’embouchure de la riviére Saguenay (van Zyll de Jong
1983). La Musaraigne cendrée (Sorex cinereus), une
espece plus commune au Québec (observation per-
sonnelle), a une distribution qui s’étend bien plus au
TABLEAU |. Mesures comparées du spécimen de musaraigne trouvé sur la Cote Nord, de la Musaraigne fuligineuse et de la
Musaraigne cendrée.
Longueur Largeur du Longueur Longueur de
Espéce du crane (mm) maxillaire (mm) totale (mm) la queue (mm)
Spécimen de la Céte Nord WET 4.8 111,4 47,8
Musaraigne fuligineuse 17,5 a 18,8? 4,8 45,4? 1104127! 40 452!
SIS? >4,6° 104 a 1252 42 a 54?
Musaraigne cendrée 15,2 a 16,92 3.8 44,32 924110! 37 a 46!
<173 <4,6° Ta le52 28 a 507
' Banfield 1977
> van Zyll de Jong 1983
3 Maisonneuve et al. 1997
441
442
nord (van Zyll de Jong 1983; Banfield 1977). La dé-
couverte de la Musaraigne fuligineuse 4 Godbout in-
dique que la distribution de certaines espéces de petits
mammiféres est encore mal connue. En ce sens, il est
permis de croire que de futures découvertes seront
faites et permettront de mieux connaitre les habitats
fréquentés par ces espéces et de préciser leur aire de
distribution dans le nord de la province. II est a noter
que cette mention de la Musaraigne fuligineuse figure
dans |’Atlas des micromammiféres du Québec, sans
documentation publié en 2002 (Desrosiers et al. 2002).
Remerciements
Nous tenons a remercier Mme Stéphanie Houde,
technicienne de la faune, pour la vérification de l’iden-
tification du spécimen de méme que M. Gilles Lupien,
technicien de la faune a la Société de la Faune et des
Parcs du Québec, pour ses commentaires sur les cap-
tures de l’espéce au Québec. Nous remercions égale-
ment le comité ZIP de l’estuaire du Saint-Laurent, qui a
permis la réalisation de |’inventaire duquel la présente
découverte de la Musaraigne fuligineuse a été faite.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Littérature citée
Banfield, A. W. F. 1977. Les Mammiféres du Canada. Les
Presses de l’ Université Laval et University of Toronto Press.
Publié par le Musée national des Sciences naturelles,
Musées nationaux du Canada. Ottawa, Canada. 406 pages.
Beaulieu, H. 1992. Liste des espéces de la faune vertébrée
susceptibles d’étre désignées menacées ou vulnérables au
Québec. Ministére du Loisir, de la Chasse et de la Péche.
Québec. 107 pages.
Desrosiers, N., R. Morin, et J. Jutras. 2002. Atlas des
micromammiféres du Québec. Société de la faune et des
parcs du Québec et Fondation de la Faune du Québec. 92
pages.
Maisonneuve, C., R. Mc Nicoll, S. St-Onge, et A. Des-
rosiers. 1997. Clé d’identification des micromammiferes
du Québec. Ministére de 1’ Environnement et de la Faune,
Québec. 19 pages.
van Zyll de Jong, C. G. 1983. Traité des Mammiféres du
Canada, volume | : Les Marsupiaux et les Insectivores. Mu-
sée national des Sciences naturelles, Musées nationaux du
Canada. Ottawa, Canada. 217 pages.
Recu 28 octobre 2001
Acceptée 15 janvier 2005
Gulls, Larus spp., Foraging at Pink Salmon, Oncorhynchus gorbuscha,
Spawning Runs
Mary FE. WILLSON
5230 Terrace Place, Juneau, Alaska 99801 USA; e-mail mwillson@ gci.net
Willson, Mary F. 2004. Gulls, (Larus spp.), foraging at Pink Salmon, Oncorhynchus gorbuscha, spawning runs. Canadian
Field-Naturalist 118(3): 442-443.
Small and immature gulls foraged more often on drifting salmon eggs than did large and mature gulls, and large and mature
gulls foraged more often on salmon carcasses, at streams in Southeast Alaska. These differences may be related to body size
via physical strength and dominance status, as well as foraging experience.
Key Words: Gulls, Larus spp., Pink Salmon, Oncorhynchus gorbuscha, Southeast Alaska.
Salmon spawning runs attract many foraging birds
and mammals (Willson and Halupka 1995) and are
clearly an important food resource for wildlife in late
summer and fall. Gulls (Larus spp.) are among the most
numerous predators and scavengers at salmon runs,
sometimes occurring in the thousands (Isleib and Kes-
sel 1973). Here I report how four species of gull ex-
ploited runs of Pink Salmon (Oncorhynchus gor-
buscha) at the mouths of streams in Juneau, Alaska.
Study Area and Methods
Most of these observations were made at the mouths
of Salmon Creek and Sheep Creek (less than 12 km
apart), with some supplementary observations at four
other small, nearby streams, within the city and bor-
ough of Juneau in Southeast Alaska (ca. 58°30'N,
133°30'W). I observed four species of gulls foraging
at or near low tides, usually in the morning, from 27
August to 6 September 2002 (>6 hrs of observation).
At any one time, many dozens of gulls were present
at the two primary study locations. At low tide, these
creeks flow over intertidal deltas, often with several
shallow channels used by incoming salmon. I scanned
these deltas with spotting scope and binoculars, noting
the foraging activities of the gulls and counting the
individuals engaged in several distinctive foraging ac-
tivities. Birds shifted position frequently, using different
parts of the deltas; many individuals of the three larger
species also changed foraging activity as I watched.
Most scans were made at different locations on differ-
ent days; if more than one scan occurred on the same
day and stream delta, they were separated in time by
about 30 min. I recorded foraging observations in three
categories: foraging on salmon eggs (drifting eggs are
common because later spawners often disturb the grav-
els over the nests of earlier spawners, foot-paddling
by gulls also stirs up poorly buried eggs), foraging on
salmon carcasses (including some extraction of eggs
from living or dead fish), and searching for inverte-
brates in Fucus mats (where amphipods and isopods
were common) and tide pools.
2004 NoTes 443
TABLE |. Foraging activity of four species of gull at salmon spawning runs in southeast Alaska.
Species/age class Eggs Salmon Invertebrates N (observations)
Bonaparte’s Gull 82% - 18% 353
Mew Gull adults 33% 1% 66% 232
Herring Gull adults* 31% 58% 11% 26
Herring Gull immatures 80% 20% - 15
Glaucous-wing adults* 11% 87% 2% 362
Glaucous-wing immatures 44% 55% 1% 222
‘Frequency distributions for adults and immatures were significantly different (y’, = 88.5 and 7.1, for the two species
respectively; p < 0.05 in both cases).
Results
Foraging behavior of each species was very con-
sistent among the observed streams, but there were
marked differences in foraging among species and
age classes (Table 1). The small (ca. 190 g, Sibley
2000) Bonaparte’s Gull (L. philadelphia) foraged for
salmon eggs chiefly by hovering over the streams and
plunge-diving for drifting eggs, but they occasionally
sought invertebrates in Fucus mats or tide pools.
Most birds were in nonbreeding plumage, and adults
were not distinguished from immatures.
Mew Gulls (L. canus), of intermediate size (ca.
420 g, Sibley 2000), waded in the shallows, searching
for drift eggs, or hunted invertebrates in Fucus mats.
They seldom foraged on fish carcasses and then only
if no large gulls were nearby. Too few immatures were
present for adequate sampling, so all observations per-
tain to adults.
Both Herring (L. argentatus) and Glaucous-winged
(L. glaucescens) gulls (body mass about 1000-1100 g
for both species, Sibley 2000) foraged chiefly on car-
casses and on eggs, only rarely visiting the Fucus mats
on these deltas. Eggs were commonly obtained while
wading, occasionally by foot-paddling. Glaucous-wing
adults sometimes pulled live salmon from the stream,
poking initially at eyes and at the vent area to force egg
extrusion. Immatures of both species foraged more
often on eggs than did adults, while adults foraged more
often on carcasses. Both of these larger gulls often
examined very old, bleached and decayed, carcasses
that appeared to offer little or nothing edible.
Discussion
Salmon eggs are rich in lipids (Gende et al. 2001,
2004), offering an easily captured and high-calorie
food, and brightly colored, so they are easy to see as
they drift downstream. Bonaparte’s Gulls, Mew Gulls,
and immatures of the larger species foraged heavily
on eggs. The demands of imminent fall migration for
the smaller gulls may provide added impetus for
rapid energy acquisition; most Bonaparte’s Gulls left
the area before the Pink Salmon runs were completely
over. The immatures are less experienced foragers than
adults, and eggs may be more easily accessed than
carcasses. Carcasses are probably less accessible to
smaller gulls because the skin is tough and hard to
breach and also because the larger gulls (and ravens
and eagles) can easily dominate the smaller birds.
Glaucous-winged Gulls selectively killed and eviscer-
ated female Sockeye Salmon (O. nerka) in shallow
streams in westem Alaska (Mossman 1958). The forag-
ing differences among gull species here are similar to
the observations of Moyle (1966) elsewhere in Alaska.
Other species of wildlife also favor salmon eggs.
Bears (Ursus spp.) often feed selectively on eggs (and
other high-lipid body parts) from live-caught fish
(Gende et al. 2001). American Dipper (Cinclus mexi-
canus) chicks, juveniles, and adults feed on drift eggs
(Obermeyer et al. 1999; K. E. Obermeyer and M. F.
Willson, unpublished observations). Foraging: on drift
eggs by wildlife has no significant effect on salmon
populations, because drift eggs do not survive outside
the nesting gravels.
Literature Cited
Gende, S. M., T. P. Quinn, and M. F. Willson. 2001. Con-
sumption choice by bears feeding on salmon. Oecologia
127: 372-382.
Gende, S. M., T. P. Quinn, M. F. Willson, R. Heintz, and
T. M. Scott. 2004. Magnitude and fate of salmon derived
nutrients and energy in a coastal system ecosystem. Journal
of Freshwater Ecology 19: 149-160.
Isleib, M. E., and B. Kessel. 1973. Birds of the north gulf
coast-Prince William Sound region, Alaska. Biological
Papers, University of Alaska 14: 1-149.
Mossman, A. S. 1958. Selective predation of glaucous-winged
gulls upon adult red salmon. Ecology 39: 482-486.
Moyle, P. 1966. Feeding behavior of the glaucous-winged
gull on an Alaska salmon stream. Wilson Bulletin 78:
175-190.
Obermeyer, K. E., A. Hodgson, and M. F. Willson. 1999.
American Dipper, Cinclus mexicanus, foraging on salmon
eggs. Canadian Field-Naturalist 113: 288-290.
Sibley, D. A. 2000. The Sibley guide to birds. Knopf, New
York.
Willson, M. F., and K. C. Halupka. 1995. Anadromous fish
as “keystone” resources in vertebrate communities. Con-
servation Biology 9: 489-497.
Received 26 February 2003
Accepted 22 January 2004
444 THE CANADIAN FIELD-NATURALIST Vol. 118
Sequential Polyandry in Piping Plover, Charadrius melodus, Nesting
in Eastern Canada
DIANE L. AMIRAULT!, JONATHAN KIERSTEAD!, PETER MACDONALD? and LARRY MACDONNELL!
! Canadian Wildlife Service, Environment Canada, P.O. Box 6227, Sackville, New Brunswick E4L 1G6 Canada
? Nova Scotia Department of Natural Resources, P.O. Box 99, Tusket, Nova Scotia BOW 3MO Canada
Amirault, Diane L., Jonathan Kierstead, Peter MacDonald and Larry MacDonnell. 2004. Sequential polyandry in Piping
Plover, Charadrius melodus, nesting in eastern Canada. Canadian Field-Naturalist 118(3): 444-446.
On Cape Sable Island, Nova Scotia, we confirmed that a banded female Piping Plover (Charadrius melodus melodus) produced
two broods of chicks during the 2000 nesting season, the second on a beach approximately 2 km from the first. The female
abandoned her second brood two days after hatching, leaving the male to complete brood rearing.
Key Words: Piping Plover, Charadrius melodus, sequential polyandry, Nova Scotia.
Piping Plovers (Charadrius melodus) generally have
been thought to be monogamous, with males estab-
lishing and defending territories and raising only one
brood per season (Wilcox 1959; Cairns 1982; Haig
and Oring 1988; Haig 1992). Renesting in Piping
Plovers is common if a clutch is lost (Haig 1992) and
occasionally occurs if a brood of chicks is lost (Mac-
Ivor 1990). In Manitoba, Piping Plovers exhibited
sequential polyandrous behavior (Oring 1982; Haig
1992) where some breeding adults had multiple nests
and mates (Haig and Oring 1988) after predation or
storm events caused nest loss.
The best example of polyandry in shorebirds has
been documented in the Spotted Sandpiper (Actitis
macularia) (Oring and Knudson 1973). Within Spotted
Sandpipers, females are larger and more aggressive than
males and establish and defend nesting territories.
Female Spotted Sandpipers lay several clutches of eggs
while different males incubate eggs and complete
brood-rearing tasks for each.
Bottitta et al. (1997) published the first observations
of Piping Plovers successfully fledging two broods in
one nesting season, at Griswold Point in Old Lyme,
Connecticut, and Assateague Island National Seashore,
along the Maryland and Virginia coast. During the
Bottitta et al. (1997) studies (1989-1994), eight Piping
Plover pairs successfully raised two broods each within
a reproductive season. Although not all birds involved
were banded to enable identification of individuals,
mates in most cases were thought to have been re-
tained because of plumage characteristics and proximity
of second nests to locations of first nests.
The potential for Piping Plovers P. m. meliodius to
raise a second brood in eastern Canada is thought to
be small, owing to the later, and therefore shorter, nest-
ing season associated with a more northerly location.
With aid of a banding program, we documented the
production of a second brood by the same female
Piping Plover in southwestern Nova Scotia during
the 2000 nesting season.
Study Area and Methods
Piping Plovers have been closely monitored on two
beaches (Daniels Head beach [43°26'N, 65°36'W] and
Stoney Island beach [43°28'N, 65°34'W]) on Cape
Sable Island in southern Nova Scotia since 1997 (P.
MacDonald, unpublished data). Daniels Head beach
encompasses a 15-90 m (high-low tide) wide stretch
of light-coloured sand extending the full length of the
3.3 km beach, broken by four rocky points and an inlet
to a sandy tidal-flat area. Low vegetated (Ammophila
breviligulata and other grasses) dunes provide a break
between the beach and a brackish inland marsh. Sto-
ney Island is a light-coloured sand beach bordered by
low, densely vegetated dunes (Ammophila breviligulata,
grasses, and shrubs). The 15-75 m (high-low tide)
wide beach extends 1.8 km in a crescent shape from
a rocky point in the south to an embankment in the
north. The beaches are separated by an approximate-
ly 2 km long coastal stretch characterized by rocky
shoreline, a tidal channel, and headland on which a
fish processing plant is located (Boates et al. 1994*).
Daniel’s Head beach supported from three to seven
nesting pairs of Piping Plovers in the 1997 to 2000
period. Conversely, the single pair at Stoney Island
beach was the only successful nesting event since
LOOT:
We trapped and banded birds on several occasions
during May-July 2000. A modified Weller trap was
used to capture adult birds incubating eggs (Weller
1957). A trapped bird was immediately removed from
the trap, banded with a United States Fish and Wildlife
Service numbered metal incoloy band on the lower
right leg (for adult birds) and a Canadian Wildlife
Service bicoloured plastic band on the lower left leg
(specific to province) and released.
Results
On 24 May 2000, we trapped and banded a female
Piping Plover incubating four eggs on Daniels Head
beach. Four chicks hatched from this clutch on 30 May.
The female was not observed with the brood after 13
2004
June, at which time only one chick remained. This
chick was considered fledged on 25 June. The adult
male remained with the juvenile and both were ob-
served together until 5 July. A nest containing three
eggs was discovered on 23 June on Stoney Island
beach. Four eggs were confirmed on 25 June. We
trapped a female bird on this nest on 29 June and her
leg band number confirmed that this individual was
the female banded on 24 May at Daniels Head beach.
This second nesting event appears to have been com-
pleted with a different mate as the male from the first
nest remained with the surviving chick until 5 July,
well after fledging. The second pair hatched four eggs
on 18 July and the female was not observed with the
brood (4 chicks still remained) after 20 July. One
chick from this brood was considered fledged on 13
August, the last day both the juvenile and adult male
were observed. Males from each nest were unbanded,
facilitating identification of which adult (male or
female) was present with the chicks.
Discussion
Although Haig and Oring (1988) documented poly-
andry in Manitoba, their observations included renest-
ing following nest loss but never more than one brood
per nesting season. Our observations represent the first
documented occurrence of a female Piping Plover
relocating to produce a second brood within a nesting
season on Canadian nesting grounds. Bottitta et al.
(1997) were the first to report Piping Plovers raising
more than one brood in a season. However, their oc-
currences were documented in the United States and
on a single nesting beach. Although closely related
species such as Killdeer (Charadrius vociferus) and
Snowy Plover (Charadrius alexandrinus) are known
to produce two broods, this behaviour is thought to
be extremely rare among Piping Plovers (Wilcox 1959;
Cairns 1982; Whyte 1985; Haig and Oring 1988;
Maclvor 1990; Strauss 1990; Loegering 1992). Thus,
most second nest attempts are renests following nest
loss. Presumably, the second nest on Stoney Island
beach was initiated 18-19 June as Piping Plovers aver-
age 6-8 days to complete laying of a full clutch (Haig
1992). The interval between the last sighting of this
female with her first brood (13 June) and the calcu-
lated initiation of her new clutch is brief (5-6 days).
However, Piping Plovers have been known to initiate
renesting after a lost clutch in as few as 4 days
(Whyte 1985; Haig and Oring 1988; MacIvor 1990;
Loegering 1992).
Bottitta et al.’s (1997) long-term study documented
several examples of two broods being produced with-
in a nesting season, all of which were thought to have
been completed with the same mates. That is consis-
tent with renesting Piping Plovers generally retaining
the same mate (Wilcox 1959; Whyte 1985; Haig and
Oring 1988; MaclIvor 1990). However, in southern
Manitoba, renesting birds often chose a new mate in
NOTES
445
cases of high predation and nest loss (Haig and Oring
1988). Our record of intra-year mate switching sug-
gests that switching may occur in cases where nest loss
has not occurred and may increase an individual’s
productivity.
Several studies have indicated that it is not uncom-
mon for one adult, usually the female, to abandon its
brood prior to chicks fledging (Cairns 1977; Whyte
1985; Haig 1987). However, this is the first docu-
mented case of a female plover abandoning its brood
in order to produce another nest. These observations
indicate that a small number of females may leave
early to renest and leave further parental care to the
male.
Previously documented cases of sequential poly-
andry in Piping Plovers have been in circumstances
associated with high predation rates and catastrophic
storm events (Haig and Oring 1988; Maclvor 1990).
Our observations demonstrate that sequential poly-
andry may also occur where there is potential for
increasing productivity. The documentation of a sec-
ond brood produced by one female underscores the
importance of having early nest attempts succeed.
Such success would allow greater chance for a sec-
ond nesting event to occur, resulting in greater prod-
uctivity. Maclvor (1990) reported that more young
fledge from first nest attempts than from renests and
from early versus late nests. MacIvor (1990) suggest-
ed that increased vulnerability of chicks later in the
breeding season (July-August) was due to a greater
human presence on beaches then. Haig and Oring
(1988) reported greater parental care on first nest at-
tempts versus renests; however, no difference in hatch-
ing or fledging rates was noted. Therefore, measures to
enhance nest success such as placing predator exclo-
sures (Bottitta et al. 1997), symbolic fencing, and
beach guardian patrols may be particularly important
for first nest attempts as a successful early nest may
increase reproductive success.
The incidence of producing two broods within a nest-
ing season is thought to be fairly low, but documenta-
tion of one apparent double nesting event by an in-
dividual has significant implications for conducting
population counts of adult Piping Plovers. This event
justifies adherence of any Piping Plover census to a
brief window of time, as in the absence of informa-
tion such as provided by this study, the second nesting
event might have been erroneously recorded as two
additional individuals. Counts within a prescribed time
frame will decrease the potential for double-counting
birds that have relocated to renest or produce a second
brood. In past censuses, observers often have con-
sidered an adult found on a nest or a single adult with
a brood as a nesting pair (i.e., two adult birds), even
if only one adult was observed. Our observations sug-
gest that a small proportion of late-nesting pairs may
actually be successful early nesters on a second nest
attempt. Hence, danger in overestimating numbers
446
exists when counting adult Piping Plovers outside a
census window as our observations indicate not all birds
retain the same mate or beach in a nesting season.
Acknowledgments
The Canadian Wildlife Service funded the Piping
Plover banding and monitoring program during the
2000 season. The Nova Scotia Department of Natural
Resources provided in-kind and logistical support for
the 2000 seasonal effort. Andrew Boyne and Kevin
Davidson provided useful comments on earlier drafts
of the manuscript.
Documents Cited (marked * in text)
Boates, J. S., P. Austin-Smith, G. Dickie, R. Williams, and
D. Sam. 1994. Nova Scotia Piping Plover Atlas. Unpub-
lished Nova Scotia Department of Natural Resources report.
86 pages.
Literature Cited
Bottitta, G. E., A. M. Cole, and B. Lapin. 1997. Piping Plov-
ers produce two broods. Wilson Bulletin 109: 337-339.
Cairns, W. E. 1977. Breeding biology of the piping plover
in southern Nova Scotia. M.Sc. thesis, Dalhousie Univer-
sity, Halifax. 115 pages.
Cairns, W. E. 1982. Biology and behavior of breeding Pip-
ing Plovers. Wilson Bulletin 94: 531-545.
Haig, S. M. 1987. The population biology and life history
patterns of the piping plover. Ph.D. dissertation, University
of North Dakota, Grand Forks. 121 pages.
Haig, S. M. 1992. Piping Plover. Pages 1-18 in The Birds
of North America (2). Edited by A. Poole, P. Stettenheim,
THE CANADIAN FIELD-NATURALIST
Vol. 118
and F. Gill. The Academy of Natural Sciences, Philadel-
phia; The American Ornithologists’ Union, Washington,
Die
Haig, S. M., and L. W. Oring. 1988. Mate, site, and terri-
tory fidelity in Piping Plovers. Auk 105: 268-277.
Loegering, J. P. 1992. Piping Plover breeding biology, forag-
ing ecology and behavior on Assateague Island National
Seashore, Maryland. M.S. thesis, Virginia Polytechnic Insti-
tute and State University, Blacksburg, Virginia.
Maclvor, L. H. 1990. Population dynamics, breeding ecology,
and management of Piping Plovers on outer Cape Cod,
Massachusetts. M.S. thesis, University of Massachusetts,
Amherst, Massachusetts.
Oring, L. W. 1982. Avian mating systems. Pages 1-92 in
Avian Biology. Volume VI. Edited by D. S. Farner and J.
R. King. Academic Press, Inc., New York.
Oring, L. W., and M. L. Knudson. 1973. Monogamy and
polyandry in the spotted sandpiper. Living Bird 11: 59-73.
Strauss, E. 1990. Reproductive success, life history patterns,
and behavioral variation in a population of Piping Plover
subjected to human disturbance. Ph.D. dissertation, Tufts
University, Boston, Massachusetts.
Weller, M. W. 1957. An automatic nest-trap for waterfowl.
Journal of Wildlife Management 21: 456-458.
Whyte, A. J. 1985. Breeding ecology of the Piping Plover
(Charadrius melodus) in central Saskatchewan. M.Sc.
thesis, University of Saskatchewan, Saskatoon, Saskatch-
ewan.
Wilcox, L. 1959. A twenty year banding study of the Piping
Plover. Auk 76: 129-152.
Received 23 May 2003
Accepted 15 November 2004
American Dipper, Cinclus mexicanus, Preys Upon Larval Tailed Frogs,
Ascaphus truei
Curisty A. MorRISSEY!:? AND ROBERTA J. OLENICK?
'Department of Biological Sciences, Simon Fraser University, 8888 University Drive, Burnaby, British Columbia, V5A 1S6
Canada
>Never-Spook-the-Animals Wildlife Photography, 3778 West 13' Avenue, Vancouver, British Columbia, V6R 2S6 Canada
>Corresponding author (current address): Canadian Wildlife Service, Environment Canada, 5421 Robertson Road, RR#1,
Delta, British Columbia V4K 3N2 Canada; email: christy.morrissey @ec.gc.ca or cmorrissey @alumni.stu.ca
Morrissey, Christy A., and Roberta J. Olenick. 2004. American Dipper, Cinclus mexicanus, preys upon larval tailed frogs,
Ascaphus truei. Canadian Field-Naturalist 118(3): 446-448.
The American Dipper (Cinclus mexicanus) is an aquatic songbird that inhabits fast-flowing mountain streams in western
North America. Although dippers are known to feed primarily on aquatic invertebrates, they will also eat juvenile fish and
salmon eggs when available. In 2002, while monitoring and photographing nesting activities of the American dipper, we
observed and photographed adult dippers capturing Tailed Frog (Ascaphus truei) tadpoles and feeding them to their young. This
note is intended to document a rarely observed occurrence and identify interactions between two relatively uncommon species.
Key Words: American Dipper, Cinclus mexicanus, Tailed Frog, Ascaphus truei, feeding, Chilliwack River, British Columbia.
American Dippers (Cinclus mexicanus) are North
America’s only truly aquatic songbirds occupying
mountain streams of western North America from
Alaska south to Mexico (Kingery 1996). Dippers are
known to feed almost exclusively on in stream fauna,
diving underwater and probing among the rocks for
benthic invertebrates and small fish (salmon and trout)
as well as fish eggs (Kingery 1996). To our knowledge,
there have been no previous records in the literature
of dippers feeding on amphibians. However, while
studying and photographing American Dippers in
southwestern British Columbia, we observed dippers
2004
NOTES
447
ni eominstiscgagty em
sa
Creek, British Columbia, in June 2002. Photograph by Roberta Olenick.
on several occasions feeding on Tailed Frog (Ascaphus
truei) larvae.
Field work on the American Dipper was conducted
in the Chilliwack River watershed located in the Cas-
cade Mountains of southwestern British Columbia,
Canada. While observing dipper nests in June and July
2002, we noted at least two different pairs of Ameri-
_ can Dippers, attending separate nests on Tamihi Creek,
_ a tributary of the Chilliwack River (49.02 N, 121.50 W,
Ficure 2: Adult American Dipper delivering Tailed Frog tad-
pole to newly fledged dipper on Tamihi Creek, British
Columbia in July 2002. Photograph by Roberta Olenick.
elevation 545 m) feeding Tailed Frog tadpoles to their
young. Roberta Olenick photographed those dippers
delivering Tailed Frog tadpoles to nestlings or fledg-
lings at each nest site (Figures | and 2).
On one occasion, an adult dipper captured a very
large Tailed Frog tadpole (estimated length 5-6 cm)
and attempted to feed it to one of its fledglings. The
fledgling dipper struggled to swallow the large prey
item without success. Several times, the adult dipper
retrieved the tadpole, knocked it vigorously against a
rock and manipulated the large wide head in its bill.
Eventually, after several minutes of handling by the
adult, the fledgling dipper managed to swallow the
large tadpole whole.
During routine annual benthic invertebrate collec-
tions in April 1999-2002, we infrequently captured
Tailed Frog tadpoles in our Surber samplers using
kick-sampling procedures. Larval Tailed Frogs have
a distinct round mouth, well adapted to use as suction
onto the surface of in stream rocks, making them
relatively easy to identify. Tailed Frog larvae were
found on several tributaries of the Chilliwack River
including Tamihi Creek, Borden Creek, and Chipmunk
Creek. It is worth noting that all of these creeks have
present or past logging activity which is thought to limit
the presence and abundance of Tailed Frogs through
increased water temperatures and siltation (Nussbaum
et al. 1983). No other similar species of amphibians
occupy fast flowing stream habitat in our study area.
There are few known predators of Ascaphus truei.
Tailed Frog tadpoles have been identified as impor-
448
tant prey for larval Pacific Giant (Dicamptodon ensa-
tus) and Cope’s salamanders (Dicamptodon copei) and
Red-legged Frogs (Rana aurora) (Bury 1968; Jones
and Raphael 1998). Observations of garter snakes
(Thamnophis spp.) (Karraker 2001) and Cutthroat
Trout (Salmo clarki) depredating Tailed Frogs have
also been previously reported (Daugherty and Shel-
don 1982). We found only one instance in the litera-
ture where American Dippers were cited as being a
potential predator of Tailed Frogs, in Butler Creek,
Montana (Daugherty and Sheldon 1982). However, it
was not clear whether those authors actually observed
dippers feeding on Tailed Frogs. Given that the Tailed
Frog is a provincially blue-listed (vulnerable) species
in British Columbia and of special concern in the na-
tional COSEWIC listing, documentation of these rare
observations is important.
Tailed Frogs are endemic to the Pacific Northwest.
They range from British Columbia south to Califor-
nia, occupying western mountain streams and humid
forests throughout a 15-20 year lifespan (Daugherty
and Sheldon 1982). Larvae take from | to 4 years to
metamorphose into adults in cool fast streams (Bull
and Carter 1996). Their distribution directly overlaps
that of the American Dipper, which occupies the same
habitat and geographic range. Both species are consid-
ered sensitive to environmental impacts in mountain-
THE CANADIAN FIELD-NATURALIST
Vol. 118
ous watersheds from anthropogenic sources (Nuss-
baum et al. 1983, Kingery 1996). Given that these two
species occupy the same habitat and geographic range,
American Dipper predation of Tailed Frogs may be
more widespread than previously acknowledged.
Literature Cited
Bull, E. L., and B. E. Carter. 1996. Tailed Frogs: Distri-
bution, ecology, and association with timber harvest in
northeastern Oregon. United States Forest Service Re-
search Paper 497: 1-12.
Bury, R. B. 1968. The distribution of Ascaphus truei in Cali-
fornia. Herpetologica 24: 39-46.
Daugherty, C. H., and A. L. Sheldon. 1982. Age determi-
nation, growth, and life history of a Montana population
of the tailed frog. Herpetologica 38: 461-468.
Jones, L. and M. Raphael. 1998. Ascaphus truei (Tailed
Frog) predation. Herpetological Review 29: 39.
Karraker, N. E. 2001. Ascaphus truei predation. Herpeto-
logical Review 32: 100.
Kingery, H. E. 1996. American Dipper (Cinclus mexicanus).
The birds of North America (229): 1-28. Edited by A. Poole
and F. Gill. The Academy of Natural Sciences, Philadelphia,
and American Ornithologists’ Union, Washington, D.C.
Nussbaum, R. A., E. D. Brodie, and R. M. Storm. 1983.
Reptiles and amphibians of the Pacific Northwest. Univer-
sity Press of Idaho, Moscow, Idaho.
Received 28 January 2003
Accepted 6 December 2004
Piping Plover, Charadrius melodus, egg viability after seawater immersion
JULIE McKNiGut!, LINDA THOMAS?, and DIANE L. AMIRAULT?
' Canadian Wildlife Service, Environment Canada, Atlantic Region, 45 Alderney Drive, Dartmouth, Nova Scotia B2Y 2N6
Canada
? Prince Edward Island National Park, Parks Canada, 2 Palmers Lane, Charlottetown, Prince Edward Island C1A 5V6 Canada
3Canadian Wildlife Service, Environment Canada, Atlantic Region, 17 Waterfowl Lane, Sackville, New Brunswick E4L 1G6
Canada
McKnight, Julie, Linda Thomas and Diane L. Amirault. 2004. Piping Plover, Charadrius melodus, egg viability after seawater
immersion. Canadian Field-Naturalist 118(3): 448-450.
Four observed nest histories indicate Piping Plover eggs are able to survive immersion in seawater, but little is known
regarding their hardiness. As Piping Plover nests are often exposed to tidal flooding, their eggs may be relatively resistant to
inundation by seawater. Therefore, we suggest that replacing eggs recently flooded or washed out of-nests is a viable option
for the recovery of individual nests.
Key Words: Piping Plover, Charadrius melodus melodus, flooding, high tide, hatching success, viability, Prince Edward
Island, Nova Scotia.
The Atlantic Coast population of Piping Plover
(Charadrius melodus melodus) is listed as Endan-
gered in Canada and Threatened in the United States
(Goossen et al. 2002: U.S. Fish and Wildlife Service
1996). Nesting Atlantic coast Piping Plovers prefer
flat coastal beaches with sand and pebble substrate
(Boyne and Amirault 1999; Burger 1987; Cairns and
McLaren 1980). The male scrapes a shallow depres-
sion in the substrate between the mean high water mark
and the edge of adjacent dunes or vegetation (Burger
1987; Cairns 1982; Haig 1992). The young hatch
after approximately 28 days and leave the nest within
hours of hatching (Cairns 1982; Haig 1992). Nesting
areas are often flooded by storm-induced overwashes
(Cairns and McLaren 1980) and high water levels des-
troy many plover nests each season (Sylvester 1991).
Four cases in which flooded Piping Plover eggs
remained viable were documented during the course
of regular monitoring at Prince Edward Island National
Park and in southern Nova Scotia. The following nest
2004
histories confirm the viability of flooded eggs.
Case 1. On 29 May 1992, a nest at Cavendish Sand-
spit in Prince Edward Island National Park (46.5036°N,
63.4408°W) was completed with four eggs. On 5 June,
the nest was submerged by a high tide. Both adults
were present but not searching for their eggs or vocal-
ising excessively. Their eggs were removed from the
nest, temporarily replaced with clay eggs and returned
to the nest later that day. The shells that had lined the
nest were covered by wet sand and some water still
remained in the nest. After a brief period, one of the
adults returned to the nest and began to incubate and
the second adult arrived at the site shortly thereafter.
On 24 June, four chicks hatched after 26 days of
incubation. The four chicks were considered to have
fledged on 14 July.
Case 2. On 3 June 1999, a nest at Cavendish Sands-
pit (46.5028°N, 63.4322°W) was completed with four
eggs. On 17 June, this nest was flooded and the eggs
were found approximately | m from the nest in 10 cm
of water. Both adults were present and appeared agi-
tated. The real eggs were removed and clay eggs were
placed in the nest. One severely cracked egg was dis-
carded and the three undamaged eggs were returned
to the nest once the water receded. One chick hatched
on 30 June, and a second was observed on 1 July. The
remaining egg was abandoned. Only one chick sur-
vived to fledge and it was banded on 12 July. This
chick was recaptured as a breeding male on the same
beach in 2001.
Case 3. On 17 June 1999, a nest with three eggs at
Cavendish Sandspit (46.5047°N, 63.4483°W) was
flooded without damage to the eggs. The eggs were
found under 10 cm of water, more than | m from the
nest. They were replaced with clay eggs. An adult was
observed incubating the clay eggs approximately
1.5 hours later. The real eggs were then replaced and
both adults returned within 30 minutes. Only one
adult was observed on subsequent visits and the nest
was considered abandoned on 20 June. The eggs were
collected on 22 June, candled, found to be viable and
placed in an incubator. The eggs were candled again
on 30 June, when further growth and movement was
observed in all 3 eggs. The eggs were successfully
fostered to another Piping Plover pair on 3 July, but
were taken by a predator on 4 July. The eggs from
this nest were not only flooded, but endured a 24-48
hour lapse in incubation without any apparent decrease
in viability.
Case 4. A nest with three eggs was discovered on
12 June 2001 at Sebim Beach in Sand Hills Prov-
incial Park, Nova Scotia (43.5311°N, 65.5580°W),.
The full clutch remained on 25 June, but the high tide
had completely overwashed the nest and the sand
remained wet. Only two eggs remained on 11 July,
and incubation was confirmed on 13 July. One aban-
doned egg remained in the nest on 16 July. On 18
NOTES
449
July, a recently hatched chick (<Sdays of age) and
one adult were observed. The development timeline
indicates a protracted incubation period of at least 32
days. Neither chick nor adults were observed after 18
July, and the rearing period was too short for the chick
to have fledged successfully.
No information is available on the resistance of
Piping Plover eggs to submersion (Haig 1992). Ward
and Burger (1980) found that some embryos of Her-
ring Gull (Larus argentatus) eggs could remain viable
after immersion in cold seawater. As Piping Plover
eggs have long been exposed to selection due to tidal
flooding, they may be relatively resistant to the effects
of inundation (Ward and Burger 1980). Piping Plovers
exhibit strong parental tenacity to incubate and tend
eggs (Prellwitz et al. 1995) and it is likely that their
quick resumption of incubation of eggs after flooding
increases the probability of successful hatching.
These nest histories confirm that some Piping Plover
embryos can survive immersion in seawater, and that
replacing eggs washed out of recently flooded nests
will increase the survival of individual clutches.
Protracted incubation periods due to nest cooling
have been recorded for Piping Plovers and other
shorebirds (Cairns 1982). Therefore, eggs believed to
have been immersed in seawater, but still present in
the nest cup, should not be removed as long as the
adults continue to incubate and the incubation period
is shorter than 40 days.
Acknowledgments
We thank to Peter MacDonald, Amy Marsters, the
field staff at Prince Edward Island National Park,
Scott McBurney, Phil McCabe and Roland McCorm-
ick. Canadian Wildlife Service, Parks Canada and the
Nova Scotia Department of Natural Resources pro-
vided funding and logistical support.
Literature Cited
Boyne, A., and D. Amirault. 1999. Habitat characteristics
of Piping Plover nesting beaches in Nova Scotia, New
Brunswick, and Prince Edward Island. Pages 84-85 in
Proceedings, Piping Plovers and Least Terns of the Great
Plains and nearby. Edited by K. F. Higgins, M. R. Brash-
ier, and C. D. Kruse, South Dakota State University. Brook-
ings, South Dakota, 132 pages.
Burger, J. 1987. Physical and social determinants of nest
site selection in Piping Plover in New Jersey. Condor 89:
811-818.
Cairns, W. E. 1982. Biology and behavior of breeding Pip-
ing Plovers. Wilson Bulletin 94: 531-545.
Cairns, W. E., and I. A. McLaren. 1980. Status of the Pip-
ing Plover on the east coast of North America. American
Birds 34: 206-208.
Goossen, J. P., D. L. Amirault, J. Arndt, R. Bjorge, S. Boates,
J. Brazil, S. Brechtel, R. Chiasson, G. N. Corbett, F.
R. Curley, M. Elderkin, S. P. Flemming, W. Harris, L.
Heyens, D. Hjertaas, M. Huot, B. Johnson, R. Jones,
W. Koonz, P. Laporte, D. McAskill, R. I. G. Morrison,
S. Richard, F. Shaffer, C. Stewart, L. Swanson, and E.
450
Wiltse. 2002. National Recovery Plan for the Piping
Plover (Charadrius melodus). National Recovery Plan
Number. 22. Recovery of Nationally Endangered Wildlife,
Ottawa, 47 pages.
Haig, S. M. 1992. The Piping Plover. Pages 1-18 in The birds
of North America (2). Edited by A. Poole, P. Stettenheim,
and F. Gill, American Ornithologists’ Union, Washington,
Dic:
Prellwitz, D. M., K. M. Erickson, and L. M. Osborne.
1995. Translocation of Piping Plover nests to prevent nest
flooding. Wildlife Society Bulletin 23: 103-106.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Sylvester, J. 1991. Privacy please! People and plovers flock
to P.E.I.’s beaches, keeping them apart is a matter of the
birds’ survival. Canadian Geographic 111(2): 37-40.
United States Fish and Wildlife Service. 1996. Piping
Plover (Charadrius melodus), Atlantic Coast Population,
revised recovery plan. Hadley, Massachusetts. 258 pages.
Ward, L. D., and J. Burger. 1980. Survival of herring gull
and domestic chicken embryos after simulated flooding.
Condor 82: 142-148.
Received 29 May 2003
Accepted 8 November 2004
A Tribute to Loris Shano Russell, 1904-1998
KEVIN L. SEYMOUR
Department of Natural History, Royal Ontario Museum, 100 Queen’s Park, Toronto, Ontario M5S 2C6 Canada; e-mail:
kevins @rom.on.ca
Seymour, Kevin L. 2004. A tribute to Loris Shano Russell. 1904-1998. Canadian Field-Naturalist 118(3): 451-464.
It was somewhat daunting to try to write the story
of a man as accomplished as Loris Shano Russell. On
one hand, it is relatively easy to record or list the
numerous publications and awards. On the other hand,
it is much harder to see through all of the accom-
plishments in order to glimpse something of the man
himself. I got to know Loris only later in his life, as
the one tasked with arranging his weekly visits to the
Royal Ontario Museum (ROM), and so in this report
I have relied on many who knew him earlier, in par-
ticular, John E. Storer.
Russell’s accomplishments were many. He was one
of the last of the “old school” of palaeontologists,
those who studied and published original findings in
geology, stratigraphy, and both fossil invertebrates and
vertebrates: a broad concept rather foreign to most of
us in today’s specialized world. He was extremely
organized, and was meticulous with everything he did,
whether it was science, museology, ham and military
radio operation, or administration. He was unfailingly
polite and dignified, and always came to work wearing
jacket and tie; about the worst name he ever called
anyone in public was “stuffed shirt”, a phrase he
reserved for H. F. Osborn.
Loris died in July 1998, in his 95" year, and was
predeceased by his beloved wife Grace, in March 1998.
Their partnership of 60 years is the stuff of legends.
They did everything together, from hosting museum
dignitaries at their home, to attending antique markets,
to working in the dirt and the heat in the badlands of
Alberta collecting fossils (Figure 1). Grace never did
learn very much about the fossils, but that didn’t matter
to her at all — she was there for, and with, Loris. When
he was hospitalised in 1990, Grace visited several times
a week, as long as the Wheel-Trans vehicles were
available to take her there, as she was then not very
mobile herself. Their separation at this time must have
been very difficult for both of them. Grace was’ an out-
Ficure 1. Grace and Loris Russell, 10 June 1986, in the Red Deer River valley, at the site where the holotype of Edmon-
tosaurus regalis was collected by Levi and C. H. Sternberg in 1912. Photo by Maurice Stefanuk. (Photo courtesy
ROM Archives).
45]
452
spoken fan of her husband, and she was as forthright
with people as he was quiet and formal. Their differ-
ences were marked, yet their partnership flourished.
They had no children, and the topic was never dis-
cussed with others. Many “Grace” stories exist; several
are related in Churcher (2003). Francis Cook passed
on the following story. At the NMC (National Museum
of Canada, now the Canadian Museum of Nature) staff
party for Loris when he was leaving and moving to the
ROM, Grace invited everyone to visit them in their new
quarters in Toronto and to use their swimming pool.
Loris quietly yet respectfully deflected her enthusiasm
by pointing out that they were moving to an apartment
building and he was not sure that it included privileges
for an infinite number of visitors to use the pool.
Loris Shano Russell was born in April 1904, in
Brooklyn, New York. His parents were Matilda Shano
of Newfoundland, and Milan Winslow Russell of New
York. Loris’ middle name came from his mother’s
maiden name, of course, and Loris told me that “Shano”
was an anglicised version of the French “Chenaud”.
As for his unusual first name, Loris told me that his
parents simply were looking for something different
when they picked it; there was no family history to
the name.
In 1908, when Loris was four, his family moved to
Calgary, Alberta, where he grew up. He attended both
public and high school in Calgary, and must have had
a keen early interest in science, judging by early photos
of him (Figures 2 and 3). He attended the University
of Alberta, Edmonton, and graduated with a B.Sc. in
Geology in 1927; however, he had already started pub-
lishing before graduation! He spent some time prospect-
ing the Paskapoo Formation in Alberta near his fami-
ly’s home: his first two reviewed papers (published in
1926) are both on fossils of the Paskapoo. By this time
he must have already encountered the Sternberg family
of dinosaur collecting fame, as there is a 1923 photo
of Loris excavating in the Red Deer River Valley, north
of the Bleriot Ferry (Figure 4). Even at this early point
in his career, his published papers were representative
of his broad-ranging interests: one is on fossil mol-
luscs, and the other on the fossil mammal Catopsalis.
Fossils were not his only early interest, however. Before
his first refereed papers on fossils, he had published a
note on Alberta’s birds in 1923.
At Princeton University, he studied under William
Berryman Scott, the famous geologist and palaeon-
tologist. W. A. Parks, then Head of the Department of
Geology at the University of Toronto (UT), had
wanted him to study at the UT, but Loris thought that
it would be better to study with Scott, one of the very
few European-trained professional vertebrate palaeon-
tologists then teaching in North America. Loris was
awarded his M.A. in 1929, and his Ph.D. in 1930, for
a dissertation entitled “Stratigraphy and Paleontology
of the Uppermost Cretaceous and Lower Tertiary
Formations of Alberta”, a copy of which is in the ROM
THE CANADIAN FIELD-NATURALIST
Vol. 118
FiGure 2. Loris Russell, 1920. Photographer unknown.
(Photo courtesy ROM Archives).
library. By graduation he had published at least a dozen
papers, including papers on subjects as diverse as fossil
pelecypods, gastropods, fish, turtles, dinosaurs, mar-
supials and mammal tracks. These papers may have
partly resulted from his summer work as a student
assistant in 1925-1929 at the Research Council of
Alberta in Edmonton.
After graduating from Princeton in 1930 at the age
of 26, he moved to Ottawa and served as Assistant
Palaeontologist for the Geological Survey of Canada
(GSC) until 1936, and an Assistant Geologist in 1937.
During this period (1930-1937), he published over
two dozen papers, again on a wide variety of topics:
besides the requisite geological and stratigraphic works,
there were a number of papers on fossil mammals
and fresh-water molluscs, with smaller contributions
on turtles, plesiosaurs and dinosaurs. Because of the
utility of molluscs in biostratigraphy, many of his
earlier works concentrated on these fossils. Of course
his interests were not all palaeontological, and he
joined the Ottawa Field-Naturalists’ Club in 1933. He
later became an honorary member of this organization
in 1972, after serving as Vice-President for 1954-1956,
and as President for 1957-1958.
2004 SEYMOUR: TRIBUTE TO LORIS SHANO RUSSELL 453
Ficure 3. Loris Russell, 1922. Photographer unknown.
(Photo courtesy ROM Archives).
During his initial period in Ottawa (1930-1937) Loris
met his future wife and constant companion of 60 years,
Grace. Grace Evelyn LeFeuvre was eight years young-
er than Loris. Her mother was born in Montreal of
Irish stock, and her father had immigrated to Canada
from Jersey, in the Channel Islands. Grace and Loris
had met by arrangement of their mothers. While work-
ing at the GSC in Ottawa, where he could take Grace
out on dates, Loris was offered the position of Assistant
Director of the Vertebrate Section of the then separate
Royal Ontario Museum of Palaeontology (ROMP),
in 1937. This position came about due to the death of
W. A. Parks in 1936, and Parks’ protégé, Madeleine A.
Fritz, simultaneously being appointed Assistant Direc-
tor of the Invertebrate Section of ROMP. He consid-
ered turning down the offer, because he did not want
to be far from Grace. The only solution was marriage,
and his proposal was to the point: “I’m not going there
without you”. It appears he may have, at least briefly,
because he moved to Toronto in 1937, and they were
not married until 1938. Upon their marriage, Grace
had to give up her nursing career, as only one income
per household was allowed during the Depression.
With the Assistant Directorship at the ROMP came
an Assistant Professorship at the UT, in Palaeontology.
However, this work was interrupted by the Second
World War. With his ability as a ham radio operator
(Figure 5), he served from 1942 to 1945 in the Royal
Canadian Signal Corps. He first learned this skill in
1922, an interest that he may have gotten from his father,
who was a telegrapher for the railway (although his
father had died earlier in 1911). At war’s end, he was
Ficure 4. Loris Russell (right) and C. M. Sternberg (left) excavating an Edmontosaurus skeleton in the Red Deer River val-
ley, 1923. Photo by J. E. Thurston. (Photo courtesy ROM Archives).
454
FicurE 5. Loris Russell, circa 1922. Photographer unknown.
(Photo courtesy ROM Archives).
transferred to the Reserve with the rank of Major. He
continued an interest in communications, and collected
early telegraph and other communications equipment,
which since has been donated to the Museum of Sci-
ence and Technology in Ottawa. In 1946 he was appoint-
ed Director of the ROMP and in 1948 Associate Pro-
fessor at the UT. During 1937-1950 he continued his
studies of fossil vertebrates, producing some two dozen
papers on fishes, dinosaurs, creodonts, titanotheres, hors-
es, and mastodons, as well as others on the geology of
Alberta, fossil gastropods, eurypterids and even living
rattlesnakes!
In 1950 came the offer to become Chief of the Zool-
ogy Section at the NMC, an offer he could not resist.
He and Grace returned to Ottawa, and remained there
for the next 13 years. In 1956 he was appointed Direc-
tor of the Natural History Branch of the NMC (Fig-
ure 6), a post that he held until 1963. This time at the
NMC was arguably the single most important part of
his career as a research museum administrator, which
he filled with steady competence, vision and perceptive
guidance of staff activities. He hired several productive
research and curatorial staff, including Wann Langston,
Don McAllister and Arthur Clarke, who shared
Loris’ professional interests in vertebrate palaeontol-
ogy, ichthyology, and malacology, respectively. He
profoundly influenced the direction of the Canadian
natural sciences even outside his own fields of inter-
est. For instance, in 1955 he suggested to invertebrate
zoologist E. L. Bousfield that, as a staff member of a
national institution, he might consider field studies
on the Canadian Pacific coast and break from a previ-
ous eight-year Ph.D. obsession with the Atlantic
coast. This perceptive suggestion led to the discovery
of a diverse, major fauna of amphipod crustaceans of
which, during the next 30+ years, more than 200
species and higher taxa were newly described.
This period (1950-1963) must have been a very busy
time for him, because in addition, in 1958 alone, he
was appointed Acting Director of the Human History
Branch at NMC, President of the Society of Verte-
THE CANADIAN FIELD-NATURALIST
Vol. 118
brate Paleontology, President of Section IV (Geolo-
gy) of the Royal Society of Canada and he received
an honorary LL.D. from the University of Alberta.
He later became the President of the Canadian Muse-
ums Association (CMA) in 1961, and was awarded
the Willet G. Miller Medal from the Royal Society of
Canada (RSC) in 1959. With respect to the RSC, at
the time of his death in 1998 he was the most senior
member (by seven years over three other elderly fel-
lows) of the entire RSC roster of approximately 1500
names, having been elected at the remarkable youth-
ful age of 32 (in 1936), and with 62 years of mostly
active participation in this select group of Canadian
scientists.
While at the NMC, Loris always had the deep respect
of the staff, even though he had a bit of difficulty adjust-
ing to the fact that they were no longer required to
work Saturday mornings, as they had when he joined
the GSC in the 1930s. When the NMC staff complained
in winter about the cold and drafty Victoria Memorial
Museum building where they all had offices, Loris qui-
etly remarked that when Dr. Rand (Chief Zoologist
from 1942-1947 and a very productive staff member)
was there, he just put on an overcoat and went on work-
ing. During 1950-1963, he wrote nearly 60 papers, with
a broad range of topics: geology, eurypterids, molluscs,
fishes, acanthodians, champsosaurs, carnivores, horses,
and rabbits. Also during this time he produced more
synthetic papers that included discussions of mam-
malian migrations, continental zoology of the North
American Pleistocene, the geological record of evolu-
tion, as well as some on museology. These later papers
were unlike anything he had written before, and spoke
of a greater involvement in the museum community.
Examples are several reports on television in museums,
out-of-doors museums, plastics in the museum, and
historical conservation along the St. Lawrence Seaway.
Loris was intrigued by museums and was involved
in the earliest days of the CMA. He was a forward-
thinking museologist, whose central tenet could be
summed up as: “Museums are doing their job when
they are telling stories to the public”. This was not the
prevailing thought in the 1960s, when the object was
supposed to speak for itself, aided by lighting and gadg-
ets, but it seems to be the popular notion once again,
where story-centred galleries are becoming common.
Although Loris may well have had a lifelong interest
in material culture, it was during this period that this
interest blossomed; being the President of the CMA
from 1961-1963 and Acting Director of the Human
History Branch of the NMC no doubt spurred it on.
Constrained by a lack of time to do much palaeonto-
logical research while handling administration, Loris
decided he would try to apply scientific methods to
some research in material history, as an experiment.
He chose oil lamps as a subject for research, perhaps
as a manifestation of industrial development coupled
with social history, and it kept him “occupied and
2004
broke” for years. Loris and Grace visited antique shops
together, often in small towns on their way to do palae-
ontological fieldwork. Some of these adventures are
described in his 1969 Rotunda article. His habit of
meticulously documenting and labelling everything,
plus his deep-seated love of a good story (he claimed
it came from growing up in the “Wild West’), put
him in the position to do ground-breaking research in
material culture. Loris developed a superb collection
of well-documented lamps, which were later kept in
glass display cases in their Toronto apartment; these
have since been donated to the ROM. Several books,
A Heritage of Canadian Light (1968), Handy Things to
Have Around the House (1979), and Every Day Life
in Colonial Canada (1980) resulted from this research.
These are still standard references today; indeed, A
Heritage of Light was reprinted in February 2003 by
the University of Toronto Press. He became a speaker
in demand at various material culture conferences
over the next few decades.
In 1963, Loris left NMC under some controversy.
Upheaval in the administrative ranks of the NMC made
for some messy politics, which Loris did not care for.
Returning to Toronto and the ROM, he became the
Head of the Life Sciences Division at the ROM, and
a year later, he filled the newly created position of
Chief Biologist. By that time, the five former Royal
Ontario Museums (zoology, palaeontology, mineral-
ogy, geology and archaeology) had been amalgamat-
ed into a single institution under one Director. Much
of his continued success at ROM was due to Anne
Liebeck, Loris’ able secretary (Figure 7). She guarded
the entrance to Loris’ office and answered his telephone,
so that he could continue his studies virtually without
interruption. In 1964, he received a Diploma with
Distinction from the Museums Association of Great
Britain. With Loris’ return to Toronto came a profes-
sorship in the Department of Geology at the UT. He
took on three Ph.D. students before retiring: John Stor-
er (graduated in 1970), and Paul Ramaekers and Mark
Wilson, both of whom graduated in 1974. Loris offi-
cially retired in 1970, when he was appointed Professor
Emeritus at the UT in 1970, and Honorary Curator at
the ROM in 1971. Loris continued to serve the scien-
tific community after retirement — he was elected in
1971 to the Presidency of the Royal Canadian Insti-
tute, and in 1972 to the Presidency of the Internation-
al Palaeontological Union, a four-year term. He pub-
lished another 36 papers during this time, with a
familiar breadth of topics. Several papers hinted of
things to come: his museology papers concentrated
on lighting and lamps, and his articles on “Tertiary
Mammals of Saskatchewan, Part 1” and “The Great
Saskatchewan Mouse Mine” began a series of papers
on these important faunas from Saskatchewan. As
well, Loris’ paper on “Body temperature of dinosaurs
and its relationship to their extinction” in 1965 marks
the first, and often overlooked, discussion in the Eng-
SEYMOUR: TRIBUTE TO LORIS SHANO RUSSELL
FiGure 6. Loris Russell, 8 November 1956, as Head of the
Department of Natural History, National Museum of
Canada. Photographer unknown. (Photo courtesy of
the CMN Archives, negative #J4171).
lish scientific literature of what was later to become a
revolution in thinking: dinosaurs as active “warm-
blooded” animals. Grace often cited this paper as one
of the reasons she was so proud of “her hubby”. It
was not a secret wish of Loris’ that perhaps Bob
Bakker and John Ostrom (the oft-cited originators of
this hypothesis) and others might have given him
more credit for this early insightful work.
His official retirement only meant less administra-
tion. He continued fieldwork in Alberta each summer
with Grace and others, well into his eighties, until at
least 1988, supported by NSERC (Natural Science
and Engineering Research Council of Canada) grants.
These grants and the subsequent fieldwork meant that
he actively published papers until about 1990, with
over 40 contributions since retirement. He continued
to come into his ROM office daily from 1971 until
about 1990, when he first entered hospital for a hip-
replacement operation. He never left hospitals after
the first operation. From 1994 until 1997, while still
wheelchair-bound due to a second failed hip replace-
ment operation, I arranged that he visit ROM one day
a week (except during winters) using Wheel-Trans
services. During these visits he worked on his last
manuscript, concerning the biostratigraphy of the
Horseshoe Canyon Formation. Although this paper
was never published, staff at the Royal Tyrrell Museum
of Palaeontology and the Canadian Museum of Nature
plan to publish a paper in the near future on the bios-
tratigraphy of the Horseshoe Canyon Formation rec-
456
ognizing Loris’ essential contributions by including him
as a posthumous co-author. Many important palaeon-
tological contributions came from this post-retirement
period, for example, the series of papers on the Ter-
tiary Mammals of Saskatchewan (Parts 2 through 7).
More awards came late in his life, in particular, the
Canadian Silver Jubilee Medal in 1978, the Billings
Medal from the Geological Association of Canada in
1984 and the Romer-Simpson Medal from the Society
of Vertebrate Paleontology in 1992.
As Tokaryk (1998) noted, much of Loris’ scientific
work was accomplished solo, judging by the rarity of
co-authored publications (only 10 out of more than
200 papers published over 70 years have co-authors).
This was partly due to the paucity of other Canadian
palaeontologists at the time (although he was ably
assisted, or worked with, a number of others in the field),
but mostly to do with the fact that he could handle
both the geological and palaeontological parts of his
chosen projects. A measure of the impact of his work
can be taken by counting the number of his papers that
were abstracted in the German abstract series Palaeon-
tologishes Zentralblatt (after 1950 called Zentralblatt
fiir Geologie und Palaontologie, Teil 2) or Neues Jahr-
buch fiir Mineralogie, Geologie und Paliontologie
THE CANADIAN FIELD-NATURALIST
Vol. 118
4
Ficure 7. Loris Russell and Anne Liebeck at ROM, 1971. Photo by L. R. Warren. (Photo courtesy ROM Photography).
(after 1942 called Zentralblatt fiir Mineralogie, Geolo-
gie und Palaontologie). Between 1927 and 1989, I
found 68 Russell papers had been abstracted, by a
total of 15 different reviewers (besides those who wrote
anonymously), although more than half of this total
were written by Jaworski or Wenz on molluscs and
von Huene, primarily on dinosaurs.
He was an adventuresome scientist, always willing
to strike off in a new direction. While on holiday with
Grace in Hawaii, he collected some fossil land snails
at the famous Diamond Head locality of picture post-
card fame. A drawer of this material remains at the
ROM, labelled and researched, although he never did
publish on them. Nor was he afraid of being wrong,
or did he mind greatly if new research invalidated a
few of his ideas: that was the way science worked. As
long as the work was careful and the facts were straight,
then this was fine with him, an admirable quality in a
scientist!
Another quality that many people noticed in Loris
was his phenomenal memory for field localities. He
really could find fossil localities he hadn’t seen in 40
years. His successes were legion, so the few exceptions
stood out, and yet all of these exceptions seemed to
have complicating factors. For instance, he was frus-
2004
trated about not being able to relocate the Calgary
Paskapoo Formation localities he collected as a young
student, only to realise that housing developments
had probably covered the area. He tried many times
to find Brown’s (1914) Erickson’s Landing locality.
Although in Russell (1929) he reported relocating this
locality, Krause (1978) expressed some doubt about
this, and Loris must have harboured some doubts
himself. Eventually, as reported by Fox (1990), Loris
concluded that there was no way to determine from
exactly which level the slump block containing the fos-
sils was derived, and so he never was able to collect
significant additional material.
Certainly Loris had a happy outlook on life, and he
taught by example, both in the field and in the labora-
tory. He was an inspiring influence to all who worked
with him. He was also the kind of person who would
retreat to his workshop to solve design problems, per-
haps a legacy of his ham radio days. He designed a
unique machine for feeding a thin stream of washed
fossil concentrate onto a rubber belt (Figure 8), the
movement of which was controlled by a foot pedal.
The belt passed under a microscope, allowing him to
focus on, and select out, any fossils of interest with
his free hands. Uninteresting concentrate rotated off
the belt and into a box of scrap. We have preserved this
machine at the ROM; perhaps someday others will
use it. It was known by words beginning with the let-
ter ‘M’, such as ‘Miraculous Moving Miocene Mouse
Machine’. For work on site at the Kleinfelder Farm
locality in Saskatchewan (appropriately enough called
the ‘Mouse Mine’), he also designed two rotary sieves,
described in his 1970 Rotunda article.
Although Dr. Russell (as he was known) seemed a
little stiff and intimidating with some people, he actu-
ally had a wry yet somewhat playful sense of humour
that surfaced quietly with those he knew well. He was
quite amused by the ironies of growing older. On a
couple of occasions he observed: “We used to call
Scott and Osborn and their generation the ‘old boys’,
and look how things have turned out now”. He would
tell the story of being a young geological assistant in
the 1920s when one evening he got some sort of
buzzing insect stuck in his ear. On asking another
assistant, who was a medical student, what he should
do, he was told “Well, take it out of there!”. Loris’
father was a religious fundamentalist, so Loris learned
the Bible while young. In his later years he was not
religious, but appreciated and was amused by the fun-
damentalist side of Western life. He liked to recount
Charlie Sternberg’s remark “My, aren’t we clever’,
when William “Bible Bill” Aberhart (Dean of the
Calgary Prophetic Bible Institute) stated in a radio
sermon that palaeontologists were actually manufac-
turing fake dinosaur bones in seclusion in the bad-
lands. At a gathering for an NMC staff member about
to be married, Francis Cook noticed Loris was drink-
ing milk, whereas the rest of those in attendance were
SEYMOUR: TRIBUTE TO LORIS SHANO RUSSELL
457
FiGure 8. Loris Russell with the Marvellous Moving Miocene
Mouse Machine, 1981. Photographer unknown. (Photo
courtesy ROM Photography). :
not. The host, when this was mentioned, assured Fran-
cis that Loris was drinking milk only because he had
an ulcer, but that he had laced it with whiskey, there-
by obeying doctor’s orders yet joining his colleagues.
He always found his own way.
Several obituaries already have been written (Har-
ington 1998; Shaul 1998; Sues 1998; Tokaryk 1998;
Churcher 2003), and two appreciations (Swinton 1976;
Churcher 1993), with many additional biographical
details. Swinton (1976) also included a fairly complete
Russell bibliography up to 1976. A more complete
bibliography is included herein.
The Russell papers, including diaries, field notes,
photos, films (several different kinds), correspondence
and other records, were inventoried by Boden (1999)
and Baltovich (2001), and are placed in the ROM
archives. His slides and reprints of scientific articles
are stored in the Section of Palaeobiology, Depart-
ment of Natural History, ROM. Hopefully, someone
in the future will take advantage of this material (par-
ticularly the diaries and films) and write a book on
Loris Russell.
Acknowledgments
For personal information: John Storer (Yukon
Department of Tourism and Culture, Whitehorse),
Rufus Churcher (retired from the UT), Tony Flynn
(Seneca College, Toronto) and Grace’s niece Barbara
458
Rager, of Ottawa. Francis Cook, E. L. Bousfield, Dick
Harington and Richard Day, past and present NMC
(now CMN) staff, read an earlier draft and contributed
many useful comments and additions. In particular,
Richard Day located many bibliographic citations for
abstracts (and this started me looking for more!). For
salvaging the Russell diaries for the ROM: Tony Flynn.
For access to the ROM Archives, and for their interest
in the Russell papers: Julia Matthews and Sharon Hick.
For bibliographic assistance: Arthur Smith. For pho-
tographic assistance: Alison Murray and Peter Fenton.
I would like to most sincerely thank all of these people
for their assistance with this tribute; without them it
simply would not have been completed.
Documents and Literature Cited
Baltovich, R. 2001. Report on inventory project [adden-
dum]: the Loris Shano Russell papers. Unpublished
report, 18 pages. [on file in ROM Library and ROM Sec-
tion of Palaeobiology, Department of Natural History].
Boden, S. 1999. Report on inventory project: the Loris
Shano Russell papers. Unpublished report, 31 pages. [on
file in ROM Library and ROM Section of Palaeobiology,
Department of Natural History].
Brown, B. 1914. Cretaceous-Eocene correlation in New
Mexico, Wyoming, Montana, Alberta. Geological Soci-
ety of America Bulletin 25: 355-380.
Loris Shano Russell Bibliography
Compiled by KEVIN L. SEYMOUR
Included are books, book reviews, scientific arti-
cles and those on material culture, but probably not
all abstracts. Abstracts or reviews of Russell’s work
that were written by others are not included, but many
are on file in the Section of Palaeobiology, Depart-
ment of Natural History, ROM. Within any year, the
articles are not necessarily listed in strict chronologi-
cal order. For those papers with co-authors, all authors
are listed; if no author is listed, the paper was authored
solely by L. S. Russell. Copies of all publications are
on file in the Section of Palaeobiology, Department
of Natural History, ROM.
1923 Alberta and its birds. Bird-Lore 25(5): 348-350.
1926a Technique. American Journal of Science 11: 498-500.
1926b A new species of the genus Catopsalis Cope from the
Paskapoo Formation of Alberta. American Journal
of Science 12: 230-234.
1926c Mollusca of the Paskapoo Formation in Alberta. Trans-
actions of the Royal Society of Canada, Third Series,
20 (Section 4): 207-220, Plates 1-3.
1928a Didelphiidae from the Lance beds of Wyoming. Jour-
nal of Mammalogy 9: 229-232.
1928b A new fossil fish from the Paskapoo beds of Alberta.
American Journal of Science 15: 103-107.
1928c R. L. Rutherford and L. S. Russell. Mammal tracks
from the Paskapoo beds of Alberta. American Jour-
nal of Science 15: 262-264.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Churcher, C. S. 1993. Loris Shano Russell. (Eulogy for)
Romer Simpson Prize. Society of Vertebrate Paleontol-
ogy News Bulletin 157: 26-27.
Churcher, C. S. 2003. Loris Shano Russell, 1904-1998.
Proceedings of the Royal Society of Canada for 2001,
Sixth series, 12: 265-270.
Fox, R. C. 1990. The succession of Paleocene mammals in
western Canada. Pages 51-70 in Dawn of the Age of
Mammals in the northern part of the Rocky Mountain
Interior, North America. Edited by T. M. Bown and K. D.
Rose. Geological Society of America Special Paper 243.
Harington, C. R. 1998. In memoriam: Loris Shano Russell
1904-1998. Trail and Landscape 32(4): 166-169.
Krause, D. W. 1978. Paleocene primates from western Can-
ada. Canadian Journal of Earth Sciences 15: 1250-1271.
Russell, L. S. 1929. Paleocene vertebrates from Alberta.
American Journal of Science 17: 162-178.
Shaul, S. 1998. Shining a light on the dim past: lives lived -
Loris Shano Russell. Globe and Mail, August 12: A18.
Sues, H.-D. 1998. Loris Shano Russell, 1904-1998. Society
of Vertebrate Paleontology News Bulletin 174: 81-83.
Swinton, W. E. 1976. Loris Shano Russell: an appreciation.
Pages 3-13 in Athlon: essays on palaeontology in honour
of Loris Shano Russell. Edited by C. S. Churcher. Royal
Ontario Museum, Life Sciences Miscellaneous Publica-
tion.
Tokaryk, T. T. 1998. One of the last of the early giants.
Geology Today 14(6): 226-228.
1928d The genera Kindleia and Stylomyleodon. American
Journal of Science 15: 264.
1929a Paleocene vertebrates from Alberta. American Journal
of Science 17: 162-178.
1929b The validity of the genus Stylomyleodon. American
Journal of Science 17: 369-371.
Upper Cretaceous and Lower Tertiary Gastropoda from
Alberta. Transactions of the Royal Society of Cana-
da, Third Series, 23 (Section 4): 81-90, Plate 1.
1930a Early Tertiary mammal tracks from Alberta. Transac-
tions of the Royal Canadian Institute 17: 217-221,
Plates 7-11.
1930b A new species of Aspideretes from the Paskapoo For-
mation of Alberta. American Journal of Science 20:
27-32.
1930c Upper Cretaceous dinosaur faunas of North America.
Proceedings of the American Philosophical Society
69: 133-159.
1930d Fresh-water plesiosaurs. Bulletin of the Geological
Society of America 41: 198. [Abstract].
1930e Stratigraphy and paleontology of the Uppermost Cre-
taceous and Lower Tertiary Formations of Alberta.
Ph.D. thesis, Princeton University, 91 pages.
1931la Mollusca from the Upper Cretaceous and Lower Ter-
tiary of Alberta. Transactions of the Royal Society of
Canada, Third Series, 25 (Section 4): 9-19, Plates 1-2.
1931b Fresh-water plesiosaurs. Pan-American Geologist 53:
153. [Abstract].
193lc Fresh-water plesiosaurs. Canadian Field-Naturalist
45: 135-137.
1929c
2004
1931d
193 le
1932a
1932b
1932c
1932d
1932e
1932f
1932g
1933a
1933b
1933c
1933d
1933e
1933f
1933¢
1934a
1934b
1934c
1934d
1934e
1934f
1934¢
SEYMOUR: TRIBUTE TO LORIS SHANO RUSSELL
Early Tertiary Mollusca from Wyoming. Bulletins of
American Paleontology 18(64): 1-38, Plates 1-4.
Devonian fishes of eastern Canada. Bulletin of the
Geological Society of America 42:361. [Abstract]
Mollusca from the McMurray Formation of Northern
Alberta. Transactions of the Royal Society of Canada,
Third Series, 26 (Section 4): 1-7, Plate 1.
The Cretaceous-Tertiary transition of Alberta. Trans-
actions of the Royal Society of Canada, Third Series,
26 (Section 4): 121-156.
New data on the Paleocene mammals of Alberta, Cana-
da. Journal of Mammalogy 13: 48-54.
On the occurrence and relationships of the dinosaur
Troé6don. Annals and Magazine of Natural History,
Series 10, 9: 334-337.
New species of Mollusca from the St. Mary River For-
mation of Alberta. Canadian Field-Naturalist 46: 80-81.
Stratigraphy and structure of the eastern portion of the
Blood Indian reserve, Alberta. Geological Survey of
Canada, Summary Report 1931B: 26-38.
Fossil non-marine Mollusca from Saskatchewan. Trans-
actions of the Royal Canadian Institute 18: 337-341,
Plate 1.
A new species of Merychippus from the Miocene of
Saskatchewan. Canadian Field-Naturalist 47: 11.
L. S. Russell and R. T. D. Wickenden. Discovery of
an Upper Eocene mammalian fauna in Southern
Saskatchewan. Bulletin of the Geological Society of
America 44: 199. [Abstract].
Peking Man. The Civil Service Review 5: 104.
L. S. Russeil and R. T. D. Wickenden. An Upper
Eocene vertebrate fauna from Saskatchewan. Trans-
actions of the Royal Society of Canada, Third Series,
27 (Section 4): 53-66, Plate 1.
L. S. Russell and R. T. D. Wickenden. Upper Eocene
vertebrate fauna from Saskatchewan, Canada. Proceed-
ings of the Royal Society of Canada, Third Series,
27 (Appendix B): 143. [Abstract by title only].
Revision of the Lower Oligocene vertebrate fauna of
the Cypress Hills, Saskatchewan. Proceedings of the
Royal Society of Canada, Third Series, 27 (Appen-
dix B): 144. [Abstract by title only].
Early Tertiary mammal tracks from Alberta. Palaeon-
tologisches Zentralblatt 2: 321. [Abstract].
Reclassification of the fossil Unionidae (fresh-water
mussels) of Western Canada. Canadian Field-Naturalist
48: 1-4.
Pleistocene and post-Pleistocene molluscan faunas of
Southern Saskatchewan. Canadian Field-Naturalist
48: 34-37.
New fossil fresh-water Mollusca from the Cretaceous
and Paleocene of Montana. Journal of the Washing-
ton Academy of Sciences 24: 128-131.
Discovery of Middle Eocene Mammalia in British
Columbia. Proceedings of the Geological Society of
America for 1933: 368. [Abstract].
Restoration of the horned dinosaur Chasmosaurus.
Proceedings of the Geological Society of America for
1933: 368. [Abstract].
Revision of the Lower Oligocene vertebrate fauna of
the Cypress Hills, Saskatchewan. Transactions of the
Royal Canadian Institute 20: 49-67, Plates 7-10.
Fossil turtles from Saskatchewan and Alberta. Pro-
ceedings of the Royal Society of Canada, Third Series,
28 (Appendix C): 113. [Abstract].
1934h
19341
1936b
1936c
1936d
1937a
1937b
1937c
1937d
1937e
1937f
1938a
1938b
459
Fossil turtles from Saskatchewan and Alberta. Trans-
actions of the Royal Society of Canada, Third Series,
28 (Section 4): 101-110, Plates 1-6.
An Upper Eocene vertebrate fauna from Saskatchewan.
Palaeontologisches Zentralblatt 5: 43. [Abstract].
A Middle Eocene mammal from British Columbia.
American Journal of Science 29: 54-55.
Musculature and function in the Ceratopsia. Bulletin
of the National Museum of Canada 77: 39-48.
Fauna of the Upper Milk River beds, Southern Alberta.
Proceedings of the Royal Society of Canada, Third
Series, 29 (Appendix B): 99. [Abstract].
Fauna of the Upper Milk River beds, Southern Alberta.
Transactions of the Royal Society of Canada, Third
Series, 29 (Section 4): 115-128, Plates 1-5.
FE. Jj. Fraser, F. H. McLearn, L. S. Russell, P. S. War-
ren, and R. T. D. Wickenden. Geology of Southern
Saskatchewan. Geological Survey of Canada Mem-
oir 176: 1-137, Plates 1-5.
A Middle Eocene mammal from British Columbia.
Palaeontologisches Zentralblatt 6: 378. [Abstract].
Plesiosaur from the Upper Cretaceous of Manitoba.
Proceedings of the Geological Society of America
for 1934: 378. [Abstract].
Dinosaur restoration group in the National Museum
of Canada. Proceedings of the Geological Society of
America for 1934: 378. [Abstract].
A plesiosaur from the Upper Cretaceous of Manitoba.
Journal of Paleontology 9: 385-389, Plates 44-46.
Revision of the Lower Oligocene vertebrate fauna of
the Cypress Hills, Saskatchewan. Palaeontologisches
Zentralblatt 7: 49. [Abstract].
Oil and gas possibilities along Milk River, south-
eastern Alberta. Geological Survey of Canada Paper
36-12: 1-24.
Second multituberculate from the Belly River Forma-
tion of Alberta. Proceedings of the Geological Society
of America for 1935: 403. [Abstract].
New and interesting mammalian fossils from western
Canada. Transactions of the Royal Society of Canada,
Third Series, 30 (Section 4): 75-80, Plate 1.
A plesiosaur from the Upper Cretaceous of Manitoba.
Palaeontologisches Zentralblatt 8: 327. [Abstract].
Revision of the geology of the southern Alberta plains.
Transactions of the Canadian Institute of Mining and
Metallurgy 40: 185-196.
Preliminary Report. Del Bonita area, southern Alber-
ta. Geological Survey of Canada, Paper 37-10: 1-12.
L. S. Russell and J. C. Sproule. Preliminary Report.
Geology of the vicinity of Taber, Alberta. Geological
Survey of Canada, Paper 37-14: 1-7.
New non-marine Mollusca from the Upper Cretaceous
of Alberta. Proceedings of the Royal Society of Cana-
da, Third Series, 31 (Appendix B): 143. [Abstract].
New non-marine Mollusca from the Upper Cretaceous
of Alberta. Transactions of the Royal Society of Cana-
da, Third Series, 31 (Section 4): 61-67, Plate 1.
Fossil turtles from Saskatchewan and Alberta. Palaeon-
tologisches Zentralblatt 9: 373. [Abstract].
Rattlesnakes in Alberta. Canadian Geographical Jour-
nal 16(1): 33-41.
New species of Gastropoda from the Oligocene of
Colorado. Journal of Paleontology 12: 505-507.
460
1938c
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1938¢
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1940¢
1940h
19401
THE CANADIAN FIELD-NATURALIST
Complete skull of a titanothere from the Lower Oligo-
cene of Saskatchewan. Bulletin of the Geological Soci-
ety of America 49: 1920. [Abstract].
The skull of Hemipsalodon grandis, a giant Oligocene
creodont. Proceedings of the Royal Society of Canada,
Third Series, 32 (Appendix D): 146. [Abstract].
Origin of the sandstone dykes of South-eastern Alberta.
Proceedings of the Royal Society of Canada, Third
Series, 32 (Appendix D): 146. [Abstract].
The skull of Hemipsalodon grandis, a giant Oligocene
creodont. Transactions of the Royal Society of Canada,
Third Series, 32 (Section 4): 61-66, Plates 1-5.
New species of Gastropoda from the Oligocene of
Colorado. Proceedings of the Geological Society of
America for 1937: 288. [Abstract].
Skull of Hemipsalodon grandis Cope. Proceedings
of the Geological Society of America for 1937: 288.
[Abstract].
Land and sea movements in the Late Cretaceous of
Western Canada. Proceedings of the Royal Society of
Canada, Third Series, 33 (Appendix C): 198. [Abstract].
Edmontonia rugosidens (Gilmore), an armoured
dinosaur from the Belly River series of Alberta. Pro-
ceedings of the Royal Society of Canada, Third
Series, 33 (Appendix C): 200. [Abstract].
Land and sea movements in the Late Cretaceous of
Western Canada. Transactions of the Royal Society
of Canada, Third Series, 33 (Section 4): 81-99.
Sclerotic ring in the skull of Lambeosaurus. Bulletin
of the Geological Society of America 50: 1966.
[Abstract].
Notes on the occurrence of fossil fishes in the Upper
Devonian of Maguasha, Quebec. Contributions of the
Royal Ontario Museum of Palaeontology 2: 1-10,
Plate 1.
The sclerotic ring in the Hadrosauridae. Contributions
of the Royal Ontario Museum of Palaeontology 3:
1-7, Plates 1-2.
Studies of the Tertiary gravel deposits of Southern
Saskatchewan. Proceedings of the Royal Society of
Canada, Third Series, 34 (Appendix D): 158. [Abstract].
Titanotheres from the Lower Oligocene Cypress Hills
Formation of Saskatchewan. Proceedings of the Royal
Society of Canada, Third Series, 34 (Appendix D):
159. [Abstract].
Titanotheres from the Lower Oligocene Cypress
Hills Formation of Saskatchewan. Transactions of
the Royal Society of Canada, Third Series, 34 (Sec-
tion 4): 89-100, Plates 1-5.
Edmontonia rugosidens (Gilmore), an armoured
dinosaur from the Belly River series of Alberta. Uni-
versity of Toronto Studies, Geological Series 43: 1-
28, Plates I to VIII.
Geology of the Southern Alberta plains. Part 1,
Stratigraphy and structure. Geological Survey of
Canada Memoir 221: 1-128, 3 maps.
Micrichnus tracks from the Paskapoo Formation of
Alberta. Transactions of the Royal Canadian Insti-
tute 23(49): 67-74, Plates 1-2.
Discovery of a marine fauna in Eastend Formation
of Saskatchewan, Canada. Bulletin of the Geologi-
cal Society of America 51: 1976.
New genus of Gastropoda, probable ancestor of the
Grangerellidae from the Upper Cretaceous of Alberta.
1941a
1941b
1942a
1942b
1943a
1943b
1946a
1946b
1946c
1946d
1946e
1947a
1947b
1947c
1948a
1948b
1948c
1948d
1949a
1949b
Vol. 118
Bulletin of the Geological Society of America 51:
1976.
Prograngerella, a new ancestral land snail from the
Upper Cretaceous of Alberta. Journal of Paleontol-
ogy 15: 309-311.
Pleistocene horse remains from Saskatchewan. Pro-
ceedings of the Royal Society of Canada, Third Series,
35 (Appendix C): 188. [Abstract].
The structure of the crest in the dinosaur Parasaurolo-
phus. Proceedings of the Royal Society of Canada,
Third Series, 36 (Appendix C): 146. [Abstract].
The application of geology to strategy and tactics.
Proceedings of the Royal Society of Canada, Third
Series, 36 (Appendix C): 146. [Abstract].
Pleistocene horse teeth from Saskatchewan. Journal
of Paleontology 17: 110-114.
Marine fauna of the Eastend Formation of Saskat-
chewan. Journal of Paleontology 17: 281-288, Plates
47-49.
The crest of the dinosaur Parasaurolophus. Contri-
butions of the Royal Ontario Museum of Palaeontol-
ogy 11: 1-5.
Geophysical aspects of land-mine detection. Proceed-
ings of the Royal Society of Canada, Third Series,
40 (Appendix C): 170. [Abstract].
The lower jaw of the theropod dinosaur Troédon.
Proceedings of the Royal Society of Canada, Third
Series, 40 (Appendix C): 171. [Abstract].
Preliminary report on the stratigraphy of the Gaspé
limestone series, Forillon Peninsula, Cap des Rosiers
township, County of Gaspé South. Province of Quebec
Department of Mines, Bureau of Geological Surveys,
Preliminary Report 195: 1-14.
Rapport préliminaire sur la stratigraphie des séries de
calcaires de Gaspé, péninsule de Forillon, canton de
Cap des Rosiers, Comté de Gaspé Sud. Province de
Québec, Ministére des Mines, Service de la Carte
Géologique, Rapport préliminaire 195: 1-16 [French
translation of above].
Late Cretaceous and Early Tertiary correlation in
Alberta and Saskatchewan. Bulletin of the Geologi-
cal Society of America 58: 1223. [Abstract].
Post-glacial mastodon remains from southwestern
Ontario. Bulletin of the Geological Society of Amer-
ica 58: 1223. [Abstract].
A new locality for fossil fishes and eurypterids in the
Middle Devonian of Gaspé, Quebec. Contributions
of the Royal Ontario Museum of Palaeontology 12:
1-6.
A Middle Paleocene mammal tooth from the foothills
of Alberta. American Journal of Science 246: 152-
156, Plate 1.
The dentary of Troddon, a genus of theropod dino-
saurs. Journal of Paleontology 22: 625-629.
Post-glacial occurrence of mastodon remains in south-
western Ontario. Transactions of the Royal Canadian
Institute 27(57): 57-64.
Faunal facies in the Late Cretaceous marine deposits
of western Canada. Bulletin of the Geological Society
of America 59: 1348-1349. [Abstract].
The relationships of the Alberta Cretaceous dinosaur
“Laosaurus” minimus Gilmore. Journal of Paleon-
tology 23: 518-520.
Preliminary Report. The geology of the southern
part of the Cypress Hills, southwestern Saskatchewan.
2004
1950a
1950b
1950c
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1951b
1951c
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1952¢
1952h
1953a
1953b
1953¢
1953d
1953e
SEYMOUR: TRIBUTE TO LORIS SHANO RUSSELL
Saskatchewan Geological Survey, Petroleum Geolo-
gy Series 1: 1-56.
Correlation of the Cretaceous-Tertiary transition in
Saskatchewan and Alberta. Bulletin of the Geologi-
cal Society of America 61: 27-42.
The Tertiary gravels of Saskatchewan. Proceedings
of the Royal Society of Canada, Third Series, 44
(Appendix F): 226. [Abstract].
The Tertiary gravels of Saskatchewan. Transactions
of the Royal Society of Canada, Third Series, 44
(Section 4): 51-59.
Acanthodians of the Upper Devonian Escuminac For-
mation, Maguasha, Quebec. Annals and Magazine
of Natural History, Series 12, 4: 401-407.
Personalities in paleontology (Charles M. Sternberg).
News Bulletin of the Society of Vertebrate Paleon-
tology 31: 28-30.
Bobasatrania? canadensis (Lambe), a giant chon-
drostean fish from the Rocky Mountains. Annual
Report of the National Museum of Canada for the fis-
cal year 1949-50, Bulletin 123: 218-224, Plates 45-46.
Age of the Front-Range deformation in the North
American Cordillera. Proceedings of the Royal
Society of Canada, Third Series, 45 (Appendix D):
201. [Abstract].
Age of the Front-Range deformation in the North
American Cordillera. Transactions of the Royal Soci-
ety of Canada, Third Series, 45 (Section 4): 47-69.
Land snails of the Cypress Hills and their signifi-
cance. Canadian Field-Naturalist 65: 174-175.
The Northeast Conference of the American Associa-
tion of Museums, Cooperstown, New York, 19th &
20" October, 1951. Bulletin of the Canadian Muse-
ums Association 5(1): 7-12.
Succession duties and museum bequests. Bulletin of
the Canadian Museums Association 5(1): 13-14.
Television and museums — an interim report. Bulletin
of the Canadian Museums Association 5(1): 15-16.
Out-of-doors museums. Bulletin of the Canadian
Museums Association 5(2): 9-12.
A new species of eurypterid from the Devonian of
Gaspé. Proceedings of the Royal Society of Canada,
Third Series, 46 (Appendix C): 149-150. [Abstract].
Cretaceous mammals of Alberta. Annual Report of
the National Museum of Canada for the fiscal year
1950-51, Bulletin 126: 110-119, Plates 14-15.
Molluscan fauna of the Kishenehn Formation, South-
eastern British Columbia. Annual Report of the Nation-
al Museum of Canada for the fiscal year 1950-51,
Bulletin 126: 120-141, Plates 16-19.
Television and museums - second report. Bulletin of
the Canadian Museums Association 5(4): 14-16.
Gettysburg, a museum of fields and hillsides. Bulletin
of the Canadian Museums Association 6(1): 10-12.
Upper Cretaceous stratigraphy of southwestern Saskat-
chewan. Billings Geological Society, Guidebook,
Fourth Annual Field Conference: 87-97.
Tertiary stratigraphy of southwestern Saskatchewan.
Billings Geological Society, Guidebook, Fourth Annu-
al Field Conference: 106-113.
Museum news bulletins. Bulletin of the Canadian
Museums Association 6(2): 8-11.
Fauna and age of the Kishenehn Formation, south-
eastern British Columbia. Proceedings of the Royal
1953f
1953¢
1953h
1954b
1954c
1954d
1954e
1954f
1955a
1955b
1955c
1955d
1955e
1955f
1955g
1956a
1956b
1956c
1956d
1956e
1956f
461
Society of Canada, Third Series, 47 (Appendix C):
155. [Abstract].
The new art gallery of Hamilton. Bulletin of the
Canadian Museums Association 6(4): 4.
Museums of applied science. Bulletin of the Canadian
Museums Association 6(4): 5-7.
The new Kwakiutl house of Thunderbird Park. Bulletin
of the Canadian Museums Association 6(4): 7-8.
a A new species of eurypterid from the Devonian of
Gaspé. Annual Report of the National Museum of
Canada for the fiscal year 1952-53, Bulletin 132:
83-91, Plates 1-2.
Mammalian fauna of the Kishenehn Formation,
southeastern British Columbia. Annual Report of
the National Museum of Canada for the fiscal year
1952-53, Bulletin 132: 92-111, Plates 1-3.
Evidence of tooth structure on the relationships of
the early groups of Carnivora. Evolution 8: 166-171.
The Eocene-Oligocene transition as a time of major
orogeny in Western North America. Proceedings of the
Royal Society of Canada, Third Series, 48 (Appendix
C): 35. [Abstract].
The Eocene-Oligocene transition as a time of major
orogeny in Western North America. Transactions of
the Royal Society of Canada, Third Series, 48 (Sec-
tion 4): 65-69.
A new species of Cephalaspis from the Devonian
Gaspé sandstone at D’ Aiguillon. Le Naturaliste Cana-
dien 81: 245-254.
Dutch painting — the golden age. Bulletin of the Cana-
dian Museums Association 8(1): 1-3.
Television and museums — third report. Bulletin of
the Canadian Museums Association 8(1): 10-16.
Opening of the new Saskatchewan museum. Bulletin
of the Canadian Museums Association 8(2): 8.
Fort Ticonderoga bicentenary. Bulletin of the Canadian
Museums Association 8(2): 11-13.
Age of the Princeton Group, southwestern British
Columbia. Proceedings of the Royal Society of Canada,
Third Series, 49 (Appendix C): 40. [Abstract].
Recollections of some Alberta museums. Bulletin of
the Canadian Museums Association 8(3): 9-12.
Additions to the molluscan fauna of the Kishenehn
Formation, Southeastern British Columbia and adja-
cent Montana. Annual Report of the National Muse-
um of Canada for the fiscal year 1953-54, Bulletin
136: 102-119, Plates 1-3.
Plastics in the museum. Bulletin of the Canadian
Museums Association 9(1): 10-15.
Additional occurrences of fossil horse remains in
western Canada. Annual Report of the National Muse-
um of Canada for the fiscal year 1954-55, Bulletin
142: 153-154.
New discoveries of Miocene vertebrates in Saskatche-
wan. Proceedings of the Royal Society of Canada,
Third Series, 50 (Appendix C): 39. [Abstract].
Nonmarine Mollusca from the North Park Formation
of Saratoga Valley, Wyoming. Journal of Paleontology
30: 1260-1263.
The National Museum of History, Mexico. Bulletin
of the Canadian Museums Association 9(4): 15-16.
The Cretaceous reptile Champsosaurus natator Parks.
National Museum of Canada Bulletin 145: 1-51,
Plates 1-12.
462
1957a
1957b
1957c
1957d
1957e
1957f
1958a
1958b
1958c
1958d
1958e
1958f
1959a
1959b
1959¢c
1959d
1960a
1960b
196la
1961b
THE CANADIAN FIELD-NATURALIST
Tenth anniversary of the Canadian Museums Asso-
ciation. Bulletin of the Canadian Museums Associa-
tion 10(1): 1-2.
International Geophysical Year exhibit at the National
Museum. Bulletin of the Canadian Museums Asso-
ciation 10(1): 8-12.
One man’s impressions of the Lincoln Nebraska meet-
ing of the American Association of Museums. Bulletin
of the Canadian Museums Association 10(2): 10-14.
The eleventh annual meeting of the Northeast Muse-
ums Conference, Montreal and Quebec cities, Sep-
tember 3rd, 4th and Sth, 1957. Bulletin of the Cana-
dian Museums Association 10(3): 1-5.
Historical conservation along the St. Lawrence Sea-
way. Bulletin of the Canadian Museums Association
10(3): 7-9.
Tertiary plains of Alberta and Saskatchewan. Proceed-
ings of the Geological Association of Canada 9: 17-19.
Mollusca from the Tertiary of Princeton, British
Columbia. Annual Report of the National Museum
of Canada for the fiscal year 1955-56, Bulletin 147:
84-95, Plates 1-2.
Paleocene mammal teeth from Alberta. Annual Report
of the National Museum of Canada for the fiscal
year 1955-56, Bulletin 147: 96-103, Plate 1.
Report on the annual meeting of the Canadian Muse-
ums Association, Windsor, Ontario, May 7th to 9th,
1958. Bulletin of the Canadian Museums Associa-
tion 11(2): 3-15.
Mammal teeth from the Edmonton Formation at Scab-
by Butte, Alberta. Proceedings of the Royal Society of
Canada, Third Series, 52 (Appendix C): 24. [Abstract].
A horse astragalus from the Hand Hills conglomer-
ate of Alberta. National Museum of Canada, Natural
History Papers 1: 1-3.
A palaeontological view of convergence, parallelism
and orthogenesis. XVth International Congress of
Zoology, Section 1, Paper 24. [Abstract].
The dentition of rabbits and the origin of the Lago-
morpha. National Museum of Canada Contributions
to Zoology for 1958, Bulletin 166: 41-45.
Continental zoology of the North American Pleis-
tocene. Problems of the Pleistocene and Arctic, Pub-
lications of the McGill University Museums 1(1):
39-45.
Fossil mammals and intercontinental connections.
Proceedings of the Royal Society of Canada, Third
Series, 52 (Appendix C): 18. [Abstract].
Darwin: the origin of species. Pamphlet to accompa-
ny an exhibit at the National Museum of Canada
celebrating the 100th anniversary of the publication
of “The Origin of Species”. 3 pages.
The geological record of evolution. Pages 3-11 in
Evolution: Its Science and Doctrine. Edited by T. W.
M. Cameron. University of Toronto Press, Toronto.
Fossil mammals and intercontinental connections.
Pages 63-78 in Evolution: Its Science and Doctrine.
Edited by T. W. M. Cameron. University of Toronto
Press, Toronto.
The National Museum of Canada 1910 to 1960.
Department of Northern Affairs and National Re-
sources, Ottawa. 37 pages.
A museum for Canadians. Annual Report for 1960-
61, Department of Northern Affairs and National
Resources, 13 pages.
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Swinton to ROM. Bulletin of the Canadian Muse-
ums Association 13(4): 5.
Mammalian migrations in the Pleistocene. Problems
of the Pleistocene and Arctic, Publications of the
McGill University Museums 2(2): 48-55.
Mammal teeth from the St. Mary River Formation
(Upper Cretaceous) at Scabby Butte, Alberta. Nation-
al Museum of Canada, Natural History Papers 14: 1-4.
Rudolph Martin Anderson. Canadian Geographical
Journal 45(6): 198-199.
Problems and potentialities of the history museum.
Curator 6: 341-349.
Canadian museums — this centenary and the next. Bul-
letin of the Canadian Museum Association 14(4): 8-14.
Kishenehn Formation. Bulletin of Canadian Petroleum
Geology 12: 536-543.
Cretaceous non-marine faunas of northwestern North
America. Royal Ontario Museum Life Sciences
Contribution 61: 1-24.
The coming of kerosene. The Rushlight 30(2): 3-6.
The problem of the Willow Creek Formation. Cana-
dian Journal of Earth Sciences 2: 11-14.
Pushing back the dawn. Meeting Place, Journal of
the Royal Ontario Museum 1(3): 82-87.
Body temperature of dinosaurs and its relationships to
their extinction. Journal of Paleontology 39: 497-501.
Alice Evelyn Wilson, 1881-1964. Canadian Field-
Naturalist 79: 159-161.
Frank Harris McLearn, 1885-1964. Proceedings of
the Royal Society of Canada, Fourth Series, 3: 135-
139.
The mastodon. Royal Ontario Museum “What? Why?
When? How? Where? Who?” 6: 1-16.
Tertiary mammals of Saskatchewan, Part I: The
Eocene fauna. Royal Ontario Museum Life Sciences
Contribution 67: 1-33, Plates 1-7.
W. A. Clemens and L. S. Russell. Mammalian fossils
from the Upper Edmonton Formation. Pages 32-40
in Vertebrate Palaeontology in Alberta. Report of a
Conference held at the University of Alberta, Aug.
29-Sept. 3, 1963. University of Alberta, Edmonton.
The continental Tertiary of Western Canada. Pages
41-52 in Vertebrate Palaeontology in Alberta. Report of
a conference held at the University of Alberta Aug. 29
to Sept. 3, 1963. University of Alberta, Edmonton.
Macropalaeontology of the surface formations, Cypress
Hills area, Alberta and Saskatchewan. Alberta Society
of Petroleum Geologists, 15th Annual Field Conference
Guide Book, Part 1, Cypress Hills Plateau: 131-136.
A Paleocene conglomerate in westcentral Alberta.
Canadian Journal of Earth Sciences 3: 127-128.
Dinosaur hunting in western Canada. Royal Ontario
Museum Life Sciences Contribution 70: 1-37.
The changing environment of the dinosaurs in North
America. The Advancement of Science, 23(110):
197-204.
Palaeontology of the Swan Hills area, north-central
Alberta. Transactions of the Royal Society of Canada,
Fourth Series, 4 (Appendix): 16. [Abstract].
Exploring the “New Red Sandstone”. Meeting Place,
Journal of the Royal Ontario Museum 1(8): 105-107.
Lighting the pioneer Ontario home. Royal Ontario
Museum “What? Why? When? How? Where? Who?”
12: 1-16.
2004
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1974b
SEYMOUR: TRIBUTE TO LORIS SHANO RUSSELL
More heat than light. The Rushlight 32(2): 1-4.
Palaeontology of the Swan Hills area, north-central
Alberta. Royal Ontario Museum Life Sciences Con-
tribution 71: 1-31, Plate 1.
Comment on: The inability of dinosaurs to hibernate
as a possible key factor in their extinction, by J. M.
Cys. Journal of Paleontology 41: 267.
Confederation lamps. Canadian Antiques Collector
2(3): 9-11.
Review of: Fossil mammals of the type Lance For-
mation of Wyoming, Part I: Marsupialia by W. A.
Clemens. Journal of Paleontology 41: 813-814.
Review of: Marsh’s Dinosaurs: The collections from
Como Bluffs by J.-H. Ostrom and J.S. McIntosh.
Journal of Paleontology 41: 1029-1030.
Unionidae from the Cretaceous and Tertiary of Alber-
ta and Montana. Journal of Paleontology 41: 1116-
1120.
A pedunculate cirripede from Upper Cretaceous rocks
of Saskatchewan. Journal of Paleontology 41: 1544-
1547.
A dinosaur bone from Willow Creek beds in Montana.
Canadian Journal of Earth Sciences 5: 327-329.
A new cetacean from Oligocene Sooke Formation of
Vancouver Island. Canadian Journal of Earth Sci-
ences 5: 929-933, Plates 1-2.
A Heritage of Light. University of Toronto Press,
Toronto. 344 pages.
Banquet lamp from the 1870s — a correction. Ontario
Showcase 34(4): 6-7.
Adventures in old-time lighting. Rotunda 2(1): 16-25.
The great Saskatchewan Mouse Mine. Rotunda 3(1):
16-24.
Can we neglect research? Museum News 48(6): 13-
14, 48.
Correlation of the Upper Cretaceous Montana Group
between southern Alberta and Montana. Canadian
Journal of Earth Sciences 7: 1099-1108.
Those remarkable dinosaurs. Rotunda 4(1): 4-17.
L. S. Russell and C. S. Churcher. Vertebrate palaeon-
tology, Cretaceous to Recent, Interior Plains, Canada.
XXIV International Geological Congress (Montreal,
Canada), Field Excursion Guidebook 24, Part A21:
1-46.
Tertiary mammals of Saskatchewan, Part II: The
Oligocene fauna, non-ungulate orders. Royal Ontario
Museum Life Sciences Contributions 84: 1-97.
Report of the President. Proceedings of the Royal
Canadian Institute, Series 5, 19: 2-5.
The fifty million year pedigree of the horse. Proceed-
ings of the Royal Canadian Institute, Series 5, 19: 6-15.
Geological evidence on the extinction of some large
terrestrial vertebrates. Canadian Journal of Earth Sci-
ences 10: 140-145.
Everyday Life in Colonial Canada. Copp Clark Pub-
lishing Company, Toronto. 207 pages.
Erratum: Geological evidence on the extinction of
some large terrestrial vertebrates. Canadian Journal
of Earth Sciences 10: 1361.
R. E. Sloan and L. S. Russell. Mammals from the
St. Mary River Formation (Cretaceous) of southwest-
ern Alberta. Royal Ontario Museum Life Sciences
Contribution 95: 1-21.
Fauna and correlation of the Ravenscrag Formation
(Paleocene) of southwestern Saskatchewan. Royal
1974c
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463
Ontario Museum Life Sciences Contribution 102: 1-
53).
Tools of the Trades. Pages 227-239 in The Book of
Canadian Antiques. Edited by D. B. Webster. McGraw-
Hill Ryerson, Toronto.
Review of: Cars of Canada by H. Durnford and G.
Baechler. Canada: An Historical Magazine 2(1 ): 59-60.
Lower Cretaceous non-marine fauna of Alberta and
Montana. Geological Society of America, Abstracts
with Programs 7(6): 847. [Abstract]
Revision of the fossil horses from the Cypress Hills
Formation (Lower Oligocene) of Saskatchewan. Cana-
dian Journal of Earth Sciences 12: 636-648, Plates 1-6.
Mammalian faunal sucession in the Cretaceous sys-
tem of Western North America. Pages 137-161 in W.
G. E. Caldwell (editor), The Cretaceous System in the
Western Interior of North America. Geological Asso-
ciation of Canada Special Paper 13.
“Carbide” Willson. Canada: An Historical Magazine
3(1): 20-33.
The first Canadian cooking stove. Canada: An Histor-
ical Magazine 3(2): 34-35.
Pelecypods of the Hell Creek Formation (Uppermost
Cretaceous) of Garfield County, Montana. Canadian
Journal of Earth Sciences 13: 365-388, Plates 1-7.
The image of palaeontology. Pages 14-17 in Athlon:
Essays in Honour of Loris Shano Russell. Edited by
C. S. Churcher. Royal Ontario Museum Life Sci-
ences Miscellaneous Publication.
The palaeogeographic significance of the polypro-
todont marsupials. XX Vth International Geological
Congress, Sydney, Australia, Abstracts 1(7C): 333-
334. [Abstract].
A new species of talpid insectivore from the Miocene
of Saskatchewan. Canadian Journal of Earth Sciences
13: 1602-1607.
Early nineteenth-century lighting. Pages 186-201 in
Building early America: contributions toward a his-
tory of a great industry. Edited by C. E. Peterson.
Chilton Books Company, Radnor, Pennsylvania.
Early Canadian sewing machines. Canadian Collector
11(5): 26-29.
L. S. Russell and G. Edmund. Obituary: Levi Stern-
berg, 1894-1976. News Bulletin of the Society of
Vertebrate Paleontology 110: 43-44.
Tertiary mammals of Saskatchewan, Part IV: The
Oligocene anthracotheres. Royal Ontario Museum
Life Sciences Contributions 115: 1-16.
Handy Things to Have Around the House. McGraw-
Hill Ryerson Limited, Toronto. 176 pages.
Tertiary mammals of Saskatchewan, Part V: The
Oligocene entelodonts. Royal Ontario Museum Life
Sciences Contributions 122: 1-42.
A new species of Brachyhyops? (Mammalia, Artio-
dactyla) from the Oligocene Cypress Hills Forma-
tion of Saskatchewan. Royal Ontario Museum Life
Sciences Occasional Paper 33: 1-8.
Alf Erling Porsild 1901-1977. Proceedings of the
Royal Society of Canada, Fourth Series, 18: 111-114.
Invention and discovery/Invention et découverte: the
role of the inventor in Canada and the use of the patent
office records. Pages 120-128 in Science, Technology,
and Canadian History. Edited by R. A. Jarrell and N.
R. Ball. Wilfrid Laurier University Press, Waterloo,
Ontario.
464
1982a
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THE CANADIAN FIELD-NATURALIST
Tertiary mammals of Saskatchewan, Part VI: The
Oligocene rhinoceroses. Royal Ontario Museum Life
Sciences Contributions 133: 1-58.
Charles Mortram Sternberg, 1885-1981. News Bulletin
of the Society of Vertebrate Paleontology 124: 70-72.
Charles Mortram Sternberg, 1885-1981. Canadian
Field-Naturalist 96: 483-486, and cover photograph.
Charles Mortram Sternberg, 1885-1981. Proceed-
ings of the Royal Society of Canada, Fourth Series,
20: 132-135.
Evidence for an unconformity at the Scollard-Battle
contact, Upper Cretaceous strata, Alberta. Canadian
Journal of Earth Sciences 20: 1219-1231.
Tertiary mammals of Saskatchewan, Part VII: Oligo-
cene marsupials. Royal Ontario Museum Life Sci-
ences Contributions 139: 1-13.
Bringing them back alive. Rotunda 17(2): 12-17.
Exploring a great dinosaur graveyard. Rotunda 19(2):
20-29.
Biostratigraphy and palaeontology of the Scollard
Formation, Late Cretaceous and Paleocene of Alberta.
Royal Ontario Museum Life Sciences Contributions
147: 1-23.
R. J. Emry, L. S. Russell and P. R. Bjork. The
Chadronian, Orellan, and Whitneyan North American
1988
1989
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land mammal ages. Pages 118-152 in Cenozoic Mam-
mals of North America: geochronology and _bios-
tratigraphy. Edited by M. O. Woodburne. University
of California Press, Berkeley.
The first fossil hunters. Alberta 1(1): 11-16.
Preface. Pages 1-2 in Geological History of Saskatche-
wan by J. Storer. Saskatchewan Museum of Natural
History, Regina. 90 pages.
Thomas Chesmer Weston and the Red Deer River fossil
fields. Earth Sciences History 9(1): 3-5.
Charles Mortram Sternberg and the Alberta dinosaurs.
Pages 1x-xill in Dinosaur Systematics: Approaches
and Perspectives. Edited by K. Carpenter and P. J.
Currie. Cambridge University Press, Cambridge.
D. F. Stott, J. Dixon, J. R. Dietrich, D. H. McNeil,
L. S. Russell, and A. R. Sweet. Tertiary. Pages 439-
465 in Sedimentary Cover of the Craton in Canada.
Edited by D. F. Stott and J. D. Aiken. Geological
Survey of Canada, Geology of Canada 5.
A Heritage of Light. University of Toronto Press,
Toronto. 344 pages. [reprint of 1968 volume].
unpublished Biostratigraphy of the Horseshoe Canyon For-
mation, Edmonton Group, Upper Cretaceous of Alber-
ta. Unpublished manuscript on file at ROM.
Book Reviews
ZOOLOGY
The Uses and Curation of Birds’ Egg Collections: An Examination and Biography
By Martin Limbert. Peregrine Books, 27 Hunger Hills Avenue,
Horsforth, Leeds, West Yorkshire LS18 S5JS. Hardcover.
97 pages, £31 which includes postage to Canada if paid
by postal money order.
This book was written largely to explain why egg
collections should be preserved and to counter nega-
tive attitudes in Britain, where egg collecting has been
illegal for half a century. Sadly, some museums have
progressively removed birds’ eggs from public display
and consigned them instead to storage and, often, neg-
lect. The need for and methods of careful preservation
of surviving egg collections are discussed in some
detail.
There is much here of historical interest. System-
atic egg collecting in England dates back at least to
1662. Hewitson in 1831 coined the term, “oology.”
Overzealous collecting at times contributed to species’
declines. Egg set data are valuable in mapping distri-
bution limits of individual bird species, but errors in
identification and outright fraud by some egg dealers
mean that some cannot be accepted at face value; the
Canadian example of Walter Raine is mentioned in
this regard.
Limbert points out that nests and eggs have yet to
be described for up to three thousand bird species in
the world, and much information from extant collec-
tions has not yet been shared. Only recently, numerous
egg collections were studied to analyse 12 000 clutch-
es of the Common Cuckoo, thereby adding greatly to
our understanding of the extent of variation in size
and colour of cuckoo eggs deposited in the nests of
different hosts. Phenologic investigation reveals the
extent to which the eggs are laid earlier in warmer
Birds of Nunavut: A Checklist
By James M. Richards, Y. Robert Tymstra, and Anthony W.
White. Birders Journal, 701 Rossland Road East, Suite
393, Whitby, Ontario LIN 9K3 Canada 21 pages. Canadian
$8. Paper plus $1.50 postage.
This attractive booklet lists 254 confirmed species,
including 124 that are known to breed, plus 9 hypo-
thetical species. Separate codes in columns give status
codes for abundance and breeding for three arbitrary
geographic subdivisions, “Mainland” (most but not all
of the former territory of Keewatin), “Arctic Islands,”
and “Bay Islands” (south of sixty degrees). As evi-
dence that birding knowledge of Nunavut is increas-
years. Eggs are occasionally useful in determining
phylogenetic relationships of unusual species such as
the Sandgrouse. Preserved contents of eggs can be
saved for pesticide analysis. And, as modern ornithol-
ogists learned from Ratcliffe in 1962, egg-shell thin-
ning has been an indicator of pesticide burdens and
thus a method of monitoring the environment.
Of interest to many readers will be the gastronomic
aspects of seabird egg-collecting on cliffs, especially
the abundant and highly palatable egg of the Common
Guillemot at Flamborough. Later, eggs from this guille-
mot colony became celebrated among oologists for
their variety of marking and colour.
This book deals almost exclusively with oological
matters — and oology publications — concerning Great
Britain. Thirty-three valuable pages of bibliography
are given, citing mainly European sources; the land-
mark American publications of Bent, Bendire and
Reed are not included. Oology periodicals began forty
years later in Britain than those in the United States,
but ceased publication about the same time. as the
Oologist, the last survivor in America.
I detected one error in terminology, the use of “ex-
tinction” from one country of a species surviving else-
where; he should have used “extirpation.” This attrac-
tive, but expensive, little book is recommended to
anyone interested in the British approach to past bird’s
egg collections.
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N 0J8
Canada
ing rapidly, 48 confirmed species have been added
during the three years immediately prior to publica-
tion. An excellent map is unusually helpful because it
gives both the former English names and the Inuktitut
names (new for most of us) for each settlement, many
of which were initially Hudson’s Bay Company fur
trading posts. There are two pages of bibliography. All
in all, this is a commendable work in progress, and
the price is within easy reach.
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N 0J8
Canada
465
466
THE CANADIAN FIELD-NATURALIST
Vol. 118
Birds of the Untamed West: The History of Birdlife in Nebraska, 1750 to 1875
By James E. Ducey. 2000. Making History, [but released for
review in 2002]. 2415 N 56th Street, Omaha, Nebraska
68104 USA. 300 pages. U.S. $25.00. Paper.
This book is a valiant attempt to report the ornitho-
logical history of Nebraska to 1875. Commendable
strengths include Chapter 1, which discusses the bird
knowledge and lore of the native Americans, the Lako-
ta, Missouria, Otoe, Omaha, Pawnee, Ponca, and Win-
nebago tribes. Native language bird names are pro-
vided when available. Chapter 2 provides a summary
of historic explorations, most of which were made by
men merely passing through the state while heading
farther north and west. Many of these explorers came
through in autumn, after the bird breeding season was
over. Exceptions were Lewis and Clark, in Nebraska
from 11 July to 8 September 1804, and Thomas Say
with the Major Long expedition, present from 19 Sep-
tember 1819 to 6 June 1820. Chapter 3 provides a suc-
cinct account of the early bird habitats, and Chapter 4
tells which species were found in each of these habi-
tats. Ducey provides, in square brackets, occasional
corrections of obviously misleading statements in
Aughey’s 1877 paper. The list of references I found
impressive. Thirty-three early illustrations add to the
interest and attractiveness of the book.
For each observation, the name of the current Ne-
braska county is provided in upper case letters: “shout-
ing” in modern computer parlance and to me a bit
annoying. Unlike Robert E. Stewart’s North Dakota
book, Ducey does not provide a map showing the loca-
tion of each county, forcing the reader to provide him-
self with a Nebraska state map before reading very
far.
Before listing the shortcomings of Chapter 5, the last
half of the book, I chose to use Myron Swenk’s histori-
cal articles in Nebraska Bird Review (in the late 1930s)
as a veracity check. I was not too surprised to find that
Swenk had, in the late 1930s, provided more detail and
better documentation than Ducey. If one takes the Lewis
and Clark expedition as an example, Swenk used a not
excessive seven pages, including a map showing the
progress day by day, consulted original, primary sources,
and gave more detail about extant diaries of several
members of the expedition. As a further check, I com-
pared the four-plus pages of Nebraska citations in Gol-
lop’s Eskimo Curlew monograph with Ducey’s account,
which again was less complete.
Chapter 5, a List of Species, occupies 110 pages; it
lists excavated faunal remains from various forts and
Indian camps, and is a useful compilation that leads
the reader to original sources. Sadly, Ducey fails to
place the verbatim accounts of each species in the ex-
plorer’s words, indicated by quotation marks or a dif-
ferent font. As a result, one can rarely differentiate fact
from Ducey’s speculation, extrapolation, and “best
guesses.” His terminology and presentation are incon-
sistent, especially concerning whether an individual
species 1s a migrant or a resident, and whether or not
there is specific evidence of breeding. His use of “migra-
tory species” is a less satisfactory term than “migrant.”
Far too often, the term “potential breeder” is used with-
out evidence of dates or localities for eggs or young.
Clearly, a conventional publishing house would have
provided the outside editorial assistance that this
book lacks. The index is incomplete.
In spite of my caveats, especially the idiosyncratic
presentation of the species list, anyone interested in
the history of ornithology in Nebraska will find much
of interest in this inexpensive book.
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N 0J8
Canada
Birds of Nebraska: Their Distribution and Temporal Occurrence
By Roger S. Sharpe, W. Ross Silcock, and Joel G. Jorgensen.
2001. University of Nebraska Press, 233 North 8" Street,
Lincoln, Nebraska 68588-0255 USA 520 pages. U.S.
$69.95. Cloth.
This book is a nearly ideal state bird book, a scholar-
ly compilation of sightings and specimens, with careful
assessment of questionable sight and specimen records.
Subspecies receive detailed and precise attention. There
is helpful information about the best spots to search
for each species. Good use is made of data from
Breeding Bird Surveys and Christmas Bird Counts,
but only sporadic use is made of banding recoveries.
The price is kept low by omitting paintings of each
bird species, a feature of more sumptuous state books.
Four maps are useful for locating counties, but one
must consult the Gazeteer (which fails to include Pine
Ridge) to locate specific towns, parks, refuges and
other geographic features.
The introduction deals with geography, geomorphol-
ogy, aquatic systems, and climate, and then describes
each of the main environments. The history of Nebraska
ornithology is given in ten succinct pages, while anoth-
er six tell how to use the species accounts, emphasiz-
ing the key importance of the Distribution and Ecolo-
gy section for each species; sadly, the reader is not
alerted to the list of abbreviations in Appendix 1.
As might be expected in such a book, there is a
wealth of intriguing information, especially about range
extensions and both increases and decreases in popu-
lations; commendably, the maximum number of indi-
viduals seen at one time is provided for most species.
Other items that caught my attention were: Gray Par-
tridge spread into Nebraska spontaneously from South
Dakota and Iowa after much earlier attempts to intro-
duce them directly had failed; most Ruffed Grouse
disappeared by the 1880s, and it is now listed as an
2004
extirpated species; a Clapper Rail caught in a mink trap
in January was the farthest inland record, the nearest
being Tennessee; several hundred Buff-breasted Sand-
pipers followed a farmer working a field; a Cliff Swal-
low colony contained 3700 nests. There is a useful
warning about reliance on vocalizations to separate the
Eastern from the Western Wood-Pewee. The authors
also mention a population of chickadees in the Wild-
cat Hills that resembled Black-capped Chickadees
morphologically, but sang Mountain Chickadee songs.
Regrettably, lower priority is given to nest records as
compared to sightings, although the latter are of less-
er biological importance. Only a relatively few species
have data from the Cornell Nest Card Program, with
detailed numbers and dates of nests. For some other
breeding species, dates and localities of nests, eggs or
flightless young are not provided; we can only guess
that in some cases they were not available, but surely
for at least the Mourning Dove and Yellow-headed
Blackbird they were simply omitted. No list of host
species for Nebraska is provided for the Brown-head-
ed Cowbird.
It would have been helpful to place unaccepted
records within square brackets and add abbreviations
for journals at the top of the list of references. The
Book REVIEWS
467
subspecies account for the Great Horned Owl is incor-
rect since the wapacuthu race of the Great Horned
Owl has been discredited. The account of the Poor-
will is misleading, implying that the Flint Hills are in
Nebraska, whereas they are in Kansas. Mention is
made of a Golden Eagle nest with four young with-
out comment that this may be the first such record in
the North American literature, though observations
of two Golden Eagle nests with four eggs have been
published previously.
My minor criticisms aside, this is an excellent sum-
mary of what is known about Nebraska birds. The state
is important for the number of its bird species (415
with a specimen or recognizable photograph, 13 with
a description acceptable to the state committee, and 5
extinct or extirpated), and because it is the meeting
place for many closely related species which overlap
in range and sometimes interbreed. Birds of Nebraska
is a substantial and welcome addition to ornithology
in general and to state bird books in particular.
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N OJ8
Canada
Canadian Skin and Scales: A Complete Encyclopedia of Canadian Amphibians and Reptiles
By Pat E. Bumstead. Illustrated by Norman H. Worsley.
2003. Simply Wild Publications Inc., 100 Lake Lucerne
Close SE, Calgary. Alberta T2J 3H8 Canada 161 pages.
$24.95.
Although subtitled “a complete encyclopedia” this
book obviously was never intended to be so preten-
tious, but instead to serve young naturalists’ as a “first
book”. The cover, with bright colour photos of a
Horned Lizard (Stephen Glendining), Plains Garter
Snake, Western Painted Turtle, Northern Leopard Frog,
and Tiger Salamander (Brian Woltski), will attract
them. Any suspected western bias is soon dispelled
by the content, which is spread evenly across Canada.
Black-and-white sketches by Norman H. Worsley de-
pict all Canadian species and a selection of extra-limital
representatives of families. Many are adequate, some
good, but others are barely recognizable (e.g., the wrin-
kled Spotted Salamander on page 25 and Black Rat
Snake on page 124), and one is clearly the wrong
selection (the Ensatina on page 32 of a southern pat-
tern not occurring in Canada).
The pedagogical style begins with “Canadian Crea-
tures”, covering communal activities, wintering, being
dark, food resources and hibernating sites, and advan-
tages for those reptiles bearing young (in Canada, two
lizards and 13 snakes) rather than laying eggs.
Province-by-province species lists follow. Chapters
2-9 deal with amphibians in general, salamanders and
newts (21 species), frogs and toads (25), reptiles in
general, turtles and tortoises (14), lizards (5), and snakes
(24). Each family and each species which occurs in
Canada is an individual account. Those for families
give world and Canadian species totals, world range,
characteristics, and reproduction. The species accounts
include common and scientific name, a paragraph of
introduction, colour, reproduction, “where do they
live” (habitat and provinces), and a “did you know”
section. A series of questions with reference to the
page where an answer can be found are at the bottom
of many of the pages in this section. Chapter 9 deals
with Conservation and includes definitions for status
categories and species thought to be extirpated in
Canada (Timber Rattlesnake, Pacific Pond Turtle,
Pygmy Horned Lizard, Pacific Gopher Snake, East-
ern Tiger Salamander). Nine threats to others are List-
ed from habitat loss to introduction of exotic species.
A “you can help” section presents ideas for group and
individual participation. A final chapter, “Etcetera”,
covers diagrams of forms and features, the availability
of a teachers guide, and a list of Canadian internet
wildlife links, words to know, published and internet
resources used, and a five-page index. Finally, there
is a note from the author and a short biography of the
illustrator.
Although primarily concerned with Canada, the text
erratically adds extra-limital filler statements such as
that Mudpuppies “have been introduced in large New
England rivers” or that Western Skinks have been found
on islands off the coast of California. For the geograph-
ically challenged it is not made clear that species listed
for “Newfoundland” are those for the political entity
468
that includes mainland Labrador (accounting for the
salamanders included), or that the generally arctic
Nunavut extends south to include islands in Hudson
Bay (accounting for the occurrence of a frog and a
toad in the territory).
The foreword, an endorsement by Carolyn and
David Seburn, rightly extols the book for its overrid-
ing themes of excitement in observing amphibians
and reptiles, the need to treat them with respect, and
the importance of conserving their habitats. But they
overlook, or were unaware of, problems precipitated
by generalizations and simplifications while copying
information from the literature apparently without per-
sonal experience with many forms. Particularly mis-
leading in all frog and toad accounts is that the num-
THE CANADIAN FIELD-NATURALIST
Vol. 118
ber of eggs is followed by an “adults appear” which
actually refers to when tadpoles transform, the result-
ing froglets are not “adults” (mature) for months or
another year or more later. For all toads, spadefoots,
and treefrogs only the aquatic habitats where they
breed are given under “where they live” whereas
most are terrestrial much of the year. Unfortunately,
such “information” is as easily absorbed by the un-
wary and uncritical beginner as fact, and detracts from
the otherwise commendable concept and aim of the
effort.
FRANCIS R. COOK
Canadian Museum of Nature, Ottawa, Ontario K1P 6P4
Canada
Conservation and Ecology of Turtles of the Mid-Atlantic Region: A Symposium
Edited by Christopher W. Swarth, Willem M. Roosenburg
and Erik Kiviat. 2004. Bibliomania! books @biblioma
nia.com. 122 pages. U.S. $22.50.
The Mid-Atlantic region of the USA (from Vir-
ginia to New York) is an area of exceptional turtle
diversity, with 22 species (including four sea turtles).
It is also an area under exceptional development
pressure. A two-day conference was organized to dis-
cuss the status and ecology of the species affected
and held in October 1999.
This volume brings together 11 peer-reviewed
papers and 18 abstracts from the conference. The
book begins with an introduction by the editors and the
text of a keynote address by Michael Klemens, who
briefly summarizes the conclusions from his book
Turtle Conservation (2000; Smithsonian Institution
Press). The papers cover only six of the possible species
occurring in the area, with three papers on each of the
Diamondback Terrapin and the Box Turtle, two on
the Red-bellied Turtle and one each on the Blanding’s
Turtle, Bog Turtle, and Spotted Turtle. The papers
cover a wide range of topics including nest predation,
head-starting, habitat change detection, and population
For Love of Insects
By Thomas Eisner. 2003. The Belknap Press of Harvard Uni-
versity Press. Cambridge, Massachusetts, and London,
England. 464 pages. U.S. $29.95. Cloth.
Thomas Eisner is an entomological legend. His
photo, on the dust jacket of this fine book, shows a
middle-aged man cockily riding his bicycle, seated
backward on the handle bars. Eisner is to entomology
what Richard Feynman was to physics — brilliant,
quirky, and full of good stories. If, for some reason,
you need to be convinced of the fact that insects are
among the most amazing creatures on earth, this is
the book for you.
The preface to this book of insect tales compares
Thomas Eisner to Jean-Henri Fabre, the pioneer writer
on insect behaviour, who lived in the 19" century in the
ecology. Although the papers are peer-reviewed, they
are of varying quality. One of the papers is barely more
than a page in length and is little more than a report on
the number of turtles caught at one site. From a con-
servation perspective, the most interesting paper is by
Erik Kiviat (one of the editors) and various collabo-
rators and deals with the response of Blanding’s Turtles
to wetland and upland habitat creation as part of a
wetland mitigation project. Although the results are still
preliminary (three years) Blanding’s Turtles made use
of constructed nesting sites and wetlands. It is inter-
esting, however, that the turtles did not choose to over-
winter in constructed wetlands.
This collection is not the definitive statement on
the conservation of turtles in the eastern U.S. There are
no papers (although some abstracts) on many topics,
such as traffic mortality, or the effects of toxins, or
genetic isolation. Nonetheless, it is a valuable snapshot
of the wide range of activities being undertaken and it
will be of interest to anyone involved in turtle conservation.
DAVID SEBURN
Seburn Ecological Services, 920 Mussell Road, RR 1, Oxford
Mills, Ontario KOG 1S0 Canada
south of France. E. O. Wilson, the preface’s author,
seems comfortable with this comparison, but to me
they are two very different sorts of scientists. Fabre
was a poor man, and a loner. His observations were
conducted with no institutional support, and his genius
(Darwin called him “the incomparable observer”) was
not recognized until Fabre was a very old man. Eis-
ner, by contrast, is a hot-shot researcher at the top of
his game, at what is probably the finest university for
insect studies in North America (Cornell, in Ithaca,
New York), surrounded by cooperative peers, gradu-
ate students, and lots of grant money. While Fabre’s
stories tell of hardship and isolation, Eisner’s explore
the life of a modern biologist in the publish-or-perish
world of research science. (Publishing, by the way,
2004
seems to come as easily to Eisner as sneezing comes
to most of the rest of us.)
The greatest thing about Eisner, however, is that he
keeps the passion alive, and dwells not on the institu-
tional politics of science, but on his life-long fascina-
tion with the creatures that he studies. Eisner is a
chemical ecologist, and thus the book is largely about
insects and the chemicals they produce. But don’t get
the impression that it is technically difficult to under-
stand. It begins with a chapter on bombardier beetles,
and the amazing way that they spray boiling quinines
out their butts, and direct them accurately into the
faces of their enemies. This chapter, like the others,
does a nifty little dance between the insects and their
adaptations on the one hand, and the process of sci-
entific discovery on the other. The rest of the book is
just as spellbinding, and in it the reader is treated to
such juicy tidbits as explanations of how living things
can defend themselves with cyanide without acciden-
tally committing suicide, along with a host of other
marvelous insect adaptations, all skilfully elucidated
by Eisner, his colleagues, and his students. The chap-
ter on spider webs is wonderful. And if you think you
understand insects and mimicry, this book will surely
The Freshwater Fishes of Manitoba
By Kenneth W. Stewart and Douglas A. Watkinson. 2004.
University of Manitoba Press, 301 St. John’s College,
University of Manitoba, Winnipeg, Manitoba, R3T 2M5.
xvii + 276 pages. $29.95. Paper.
This book is a delight to read and use. The layout
is innovative and the text is in an exceptionally clear
font and is well written. The book is dedicated to the
late Dr. Ed J. Crossman of the Royal Ontario Museum
and co-author of the book Freshwater Fishes of Canada.
The freshwater fishes of Manitoba comprise 79
native species, | re-introduced species after extirpation,
10 introduced species, 2 artificial hybrids and 4 estu-
arine species from the Hudson Bay coast. This is the
third most diverse ichthyofauna in Canada after Ontario
and Quebec. Fifteen species from waters outside, but
neighbouring Manitoba, are included as they may
eventually be discovered in the province. There are
various introductory sections such as biogeography,
geography, species diversity patterns, and summary
sections like a glossary and a checklist, usually found
in fish books. There is also an appendix which sum-
marises fish distributions by watershed and a list of
references. There is no index but the unique layout
assists in navigating the pages.
The presentation of the book is very attractive and
easy to use. Each family account with its species has a
unique colour which appears in text headings, scientif-
ic and common names here and in tables elsewhere,
and along the upper half of the outer page margin (out-
lining the English and French names) which allows
rapid flipping as a search mechanism. It is immedi-
BooK REVIEWS
469
expose you to vast unexpected dimensions to this sup-
posedly simple phenomenon.
Thomas Eisner is also a superb photographer, and
one of the other great strengths of this book lies in
the pictures. He also uses clever illustrations to make
his point, and is clearly the sort of person who is
good at entertaining his undergraduate students while
he teaches. All of this comes together masterfully, to
create a very fine book indeed. Do I have any criti-
cisms? Not really, although for a book about “insects”
it contains a wealth of information on arachnids as
well. I suppose Eisner and his publisher didn’t want
to use the term “arthropods,” or the term “bugs” to
get around this perennial problem. No—this is a superb
book, and a book that naturalists at all levels will
enjoy. At the weekly entomology luncheon at the
University of Alberta, I found that many of my senior
colleagues (very well-read and enthusiastic entomolo-
gists!) were amazed by how much they learned from
“For Love of Insects.” I enthusiastically agree, and
recommend it heartily.
JOHN H. ACORN
Department of Renewable Resources University of Alberta,
Edmonton, Alberta, TST 5L7 Canada
ately obvious when one moves from one family to
another in the text and quick searches for a particular
group are facilitated. The scientific and English fami-
ly name is at the top right and left of each page and
also allows rapid flip searches.
The series of habitat photographs in the geography
section are excellent, and have descriptive comments.
One, showing the lower Churchill River could be
almost anywhere in the vast boreal forest except for
that peculiar hazard to Manitoban freshwater ichthy-
ologists, a Polar Bear paddling by.
Each species account gives the English, French
and scientific names, a colour photograph of the fish,
a section on Identification with key characters in bold
(sometimes only a single, short sentence for distinc-
tive species), a Distribution in Manitoba, Biological
Notes including spawning, growth and adult size, feed-
ing, habitat, and ecological role, and Importance to
People. The latter refers to commercial, angling, eco-
logical and conservation importance. There is no
lengthy anatomical description of the species as is seen
in most fish books, characters being restricted to those
used in identification with some explanation of colour
variations and amplification of characters from the
Keys.
All the fish illustrations are ideally positioned in
the species description rather than grouped as colour
plates. These photographs are generally excellent, al-
though some key characters such as mouth parts are
not evident and a close-up photograph of them would
have added to the reader’s understanding.
470
The distribution of fishes on the maps is very clear.
Red spots show known occurrences, black spots intro-
ductions while grey shading shows the continuous range
of native species. The grey shading generally conforms
to distributions based on the red spots, filling in the
gaps. However in a number of species, the limits of grey
shading conform neither to the red spots nor obvious-
ly to drainage basins. There is no explanation of how
this overall distribution was arrived at but is presum-
ably related to ecological limits for the species and
physical barriers. Some form of shading to fill in lakes
would have made the background map clearer and
perhaps partially address the previous comment.
Identification keys for each family are found at the
beginning of each family account. An alternative ar-
rangement is to group all keys together and this is
one many field and laboratory biologists would pre-
fer. Fish are wet and slimy and having keys grouped
together makes for less page turning or facilitates xerox-
ing and annotating. The keys work well although the
one for distinguishing the Brown and Black bullheads
gives diagrams of the supraethmoid shapes without
explaining what or where this structure is (and it is
not in the Glossary either).
Some other minor points of criticism and comment
must be noted. The scientific names lack the author
and date, perhaps not of significance to most readers
but a nuisance to find for those not familiar with the
ichthyological literature. The copy I have lacks paper
covers and there is only the briefest of blurbs on the
authors whose names are sufficiently common not to
lend themselves to easy Googling — more background
on the authors is often of interest to readers. The com-
mon names of fishes in English and French are on the
margin of each page enabling a rapid flip through as
a search. However the scientific name is not there
(and there is space to add it) which would have been
a great convenience. It is necessary to remember to
flip back to front as well as front to back since some
species are only on one page; this is inescapable in
the design. The key to Cottidae is a little confusing as
“Key to the freshwater sculpins and marine sculpins
The History of Ornithology in Virginia
By David W. Johnston. 2003. The University of Virginia
Press, Box 400318, Charlottesville, Virginia 22904-4318
USA. 219 pages. $35.00 U.S. Cloth.
True to the promise implicit in his title, David John-
ston’s book is a thorough history of ornithology in
Virginia. The first five chapters take us from the Ter-
tiary period 65 million years ago through to an exam-
ination of 19th-century reports and collections. Along
the way we learn all manner of interesting facts. The
abundance of skeletal elements of the extinct Passen-
ger Pigeon show it to have been common in the late
Pleistocene over 12,000 years ago, and Rock Ptarmi-
gan, Spruce Grouse and Gray Jay remains indicate a
cooler climate at the time. Archaeological research at
THE CANADIAN FIELD-NATURALIST
Vol. 118
of the genus Myoxocephalus” as this can be read as
being a key to only Myoxocephalus species although
Cottus species and freshwater Myoxocephalus are
included. The photographs note whether a specimen
is fresh or preserved but readers should be warned that
preserved here generally means very recent preserva-
tion as colour is still retained — museum specimens
of any age soon lose the colour; compare the colour-
ful “preserved” northern redbelly dace with the really
preserved and brownish deepwater sculpin. A few
photographs are not as revealing as one could hope
for, the colourful sticklebacks being poorly served in
this respect. The Glossary is good, distinguishing such
terms as bar, band and stripe although commensial is
more commonly spelled commensal and watershed is
not a “water body together with all its tributaries” but
strictly “an elevated boundary area separating tribu-
taries draining to different river systems”, and the
subopercular bone does not lie completely above the
interopercular but mainly behind it (see www.brian-
coad.com).
Although books on fishes do tend to separate into
those on marine species and those in fresh waters, the
Manitoban coastal fauna on Hudson Bay comprises
only 27 species (Coad and Reist 2004) and could
have been included in the book. The authors do in
fact deal with 13 of these species which are found in
estuarine and fresh waters also. So another 14 spe-
cies would have given a complete treatment of the
Manitoban fishes.
This book will long stand as the definitive guide to
Manitoban freshwater fishes and sets a standard for
all subsequent provincial and national books of fish
faunas.
Literature Cited
Coad, B. W., and Reist, J. D. 2004. Annotated List of the Arctic
Marine Fishes of Canada. Canadian Manuscript Report
of Fisheries and Aquatic Sciences, 2674: iv + 112 pages.
BRIAN W. COAD
Canadian Museum of Nature, PO Box 3443, Station Douglas,
Ottawa, Ontario K1P 6P4 Canada
a 1700-year-old Indian midden provided the state’s only
record of the Ivory-billed Woodpecker. Around 1650,
early English settlers were so hungry that at times
they ate bluebirds, larks, cardinals and goldfinches —
and Carolina Parakeets — as well as waterfowl, shore-
birds, and upland game birds. When settlers arrived
from England about 1590, the Indians were cutting
holes in gourds to entice Purple Martins to nest.
The chapters on early observers and naturalists are
particularly interesting. Thomas Hariot, a young man
selected by Sir Walter Raleigh to be part of the 1585
expedition and settlement, made one of the first
attempts to list North American birds, but Johnston
tells us that Hariot’s list of 111 species has never been
found. Fortunately, the paintings of John White, Har-
2004
iot’s fellow expedition member and grandfather of
Virginia Dare (the first English child born in Ameri-
ca), have survived. White painted 35 species of birds
and gave the Algonquian name for 23 of them.
The first naturalists in Virginia were the clergyman
and botanist, John Banister, who lived at Bristol Parish
from 1678 until he was accidentally killed in 1692,
and the Reverend John Clayton (1657-1725), who
published information about birds and weather in the
world’s first scientific journal, Philosophical Transac-
tions of the Royal Society of London; four pages of
Clayton’s account are reproduced by Johnston. Sadly,
although Mark Catesby spent seven years in Virginia,
1712-1719, he was then a botanical collector who
had not yet learned to paint birds; from those years
he mentioned only 33 bird species. When he returned
later for another six years, Catesby spent his time far-
ther south, so that his famous book deals mainly with
the Carolinas and rarely makes specific mention of
Virginia. In 1787, Thomas Jefferson, 14 years before
he became the third president of the United States,
made the first attempt to list all the birds of Virginia,
adding 34 additional species to the 100 pictured for
adjacent regions by Catesby.
Later chapters deal specifically with topics such as
the contributions of ornithologists with the Smithson-
ian Institution and the United States government; con-
servation and game laws; artist-naturalists; extirpated
and introduced bird species; falconry; and regions of
ornithological importance describing the observers
All-Weather Hawk Watcher’s Field Journal
By Donald Heintzelman. J. L. Darling Corp. 2614 Pacific
Hwy., Tacoma, Washington 98424-1017 USA. 66 pages.
U.S. $7.95 Paper
This handy pocket field notebook, 12 by 17.5 cm.,
consists of a conservation note, a one-page introduc-
tion, a three-page list of the diurnal birds of prey of
North and Central America, and 51 pages for field
observations. At the top of each page are blanks to
Self-Portrait With Turtles: A Memoir
By David Carroll. 2004. Houghton Mifflin, 222 Berkeley
Street, Boston, Massachusetts USA. 181 pages. U.S. $23.
David Carroll first saw a Spotted Turtle at the age
of eight. He has been enchanted by these amazing
creatures ever since.
In this exquisitely written book the author of The
Year of the Turtle and Swampwalker’s Journal shares
his obsession with turtles, nature and art. This basi-
cally chronological book is divided into four sections:
Early Years, Art School, Middle Years, Later Years.
Through these sections we see the development of a
consummate naturalist and artist, witness his choice of
art school over science and the growth of his teaching
and artistic careers. The book concludes with Carroll
hunting for turtles on the 50" anniversary of his first
discovery of a Spotted Turtle.
BOOK REVIEWS
47]
and the contributions for each. Many famous natural-
ists worked in or passed through Virginia, among
them John James Audubon and Roger Tory Peterson.
Peterson, while stationed with the U.S. army at Fort
Belvoir, “successfully petitioned the officer-in-charge
to reroute the line of march on the drill field to avoid
an occupied Horned Lark’s nest” (page 121).
Items deserving special commendation are the
detailed lists: principal ornithological accomplishments;
type specimens from Virginia; local bird lists, 1870-
1926; recent bird lists since 1952; Virginia nature
writing, 1817-1998; books since 1965 that mention
Virginia’s avifauna; Algonquian Indian names of birds;
bird banders, 1923-1965; principal collectors of bird
specimens; and observers reporting migration records
to the U.S. Biological Survey, 1884-1946. Detailed
references throughout and a selection of old draw-
ings and more recent photographs add to the interest.
Johnston’s scholarly and painstaking research makes
this is one of the finest ornithological histories avail-
able for any state. There are some weaknesses, such
as the lack of a Virginia map and an incomplete and
inconsistent index which omits names of some impor-
tant people. This book is a necessity in every museum
and University library in North America, and for any
one with an interest in the history of ornithology.
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N 0J8,
Canada
fill in for date, time, weather, and location, including
GPS coordinates. The special feature is the use of all-
weather writing paper so that one can write in the
rain!
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N OJ8,
Canada
Carroll’s memoir overcomes the common pitfall of
bogging down in autobiographical trivia. His writing
is compelling and thought-provoking: “Consecrated
to the God of my parents before my eyes were open,
I lived my first eight years in a closed circle of family,
relatives, church, and school. I lived in a totally human
environment filled with human concerns and consid-
erations. It was a world built by people for people.”
And yet within three days of his family moving to a
new home, Carroll had discovered a wetland and en-
countered a Spotted Turtle: “With that first turtle I
crossed a boundary of greater dimensions than I can
ever fully comprehend. I changed lives within a life,
worlds within a world.”
Although Carroll’s passion is turtles, his deep con-
nection with nature will resonate with any avid natu-
472
ralist. His writing is honest and moving in its evoca-
tion of special places and moments as well as the loss
of many of those special places over time: “My long
history with turtles has been marked time and again
by loss of place, by the physical and spiritual annihi-
lation of the landscape, compelling me to move on in
search of wilder places.”
This is also the kind of book you can give to non-
naturalist friends to try to make them understand why
THE CANADIAN FIELD-NATURALIST
Vol. 118
you love wading through swamps. Its combination of
graceful writing, compelling anecdotes and Carroll’s
own beautiful black and white illustrations are enough
to enchant almost any intelligent reader.
DAVID SEBURN
Seburn Ecological Services, 920 Mussell Road, RR 1, Oxford
Mills, Ontario KOG 1SO Canada
Wild Mammals of North America: Biology, Management, and Conservation (Second edition)
Edited by George A. Feldhamer, Bruce C. Thompson, and
Joseph A. Chapman. 2003. The Johns Hopkins University
Press, 2715 North Charles Street, Baltimore, Maryland
21218-4363 USA. xiii + 1216 pages. U.S. $175. Cloth.
After a 21 year interlude, the update of this monu-
mental volume on the biology and management of
North American mammals has added a third editor
and given a more prominent role to conservation as
opposed to economic importance. Even with a larger
page format and a reduction of two chapters, the sec-
ond edition is longer than the first, which reflects the
accumulated increase in research over the past two
decades. All of the accounts are updated to various
degrees with some references as recent as the same
year of publication (2003) of this book. A completely
new set of authors has been recruited to write half (28)
of the 55 chapters. Only six chapters have retained the
original contributors and these are all single authored
accounts. However, three of these accounts (black bear,
badger, and manatee) are negligibly changed from the
first edition. Of the 102 authors, there are three who
have contributed to two chapters.
The species coverage of this revised volume has
been slightly modified. There are new accounts for
Cynomys ludovicianus (Black-tailed Prairie Dog) and
Neotoma floridana (Eastern Woodrat) but the invasive
Rattus norvegicus (Brown Rat) has been removed and
the species of foxes, Martes, and skunks that were each
previously presented in two chapters have each been
combined. Furthermore, three chapters have been ex-
panded including the addition of Macrotus californicus
(California Leaf-nosed Bat) to the bats, Ammospermo-
philus (antelope ground squirrel) to the ground squirrels,
and the subsuming of Cervus nippon (Sika Deer) into
a more inclusive non-native large mammals category
covering several species at the end of the book. Recent
taxonomy also has been incorporated such as the
generic use of Lontra for the river otter, Puma for the
Mountain Lion, and Jayassu for the Collared Peccary.
Of the over 400 species of mammals known from
North America, approximately half (210) are covered
but 155 of these species are not full accounts. The
chapters range from 28 detailed single-species accounts
to six chapters that focus on two species with multi-
taxa reports comprising the remainder. Some of these
latter chapters concentrate on higher taxonomic groups
including the six species of voles (genus Microtus)
found in North America; two genera of ground squir-
rels (Spermophilus and Ammospermophilus) covering
25 species; six species of foxes in the genera Alopex,
Urocyon and Vulpes; 19 species of pocket gophers in
the family Geomyidae; six species of bats from the
Vespertilionidae family, one species from Molossidae,
and one species from Phyllostomidae; six species rep-
resenting the toothed whale suborder Odontoceti; and
11 species of the baleen whale suborder Mysticeti. The
final chapter treats several exotic or alien species and
their associated problems as related to the native fauna.
The general format within each account essentially
has remained the same as the first edition. Chapters
begin by reviewing the nomenclature, distribution, and
description of the species or species-group. Most
accounts include life history topics such as physiology,
reproduction, age estimation, ecology, feeding habits,
behavior, and mortality. A summary is then presented
on the economic status, management, conservation, and
research needs of the taxa under study. Other subjects
covered by some but not all accounts are genetics,
anatomy, development and habitat. Except for the last
chapter, all have distribution maps, skull figures, and
most have photographs of live animals. The book ends
with two appendices identifying cranial bones and illus-
trating standard cranial measurements, a glossary, and
an index.
With over 100 contributors to this edited book on
wild mammal species deemed to have management
significance in North America, it was inevitable that
there would be inconsistent treatment across groups.
For example, the account of the Black Bear (Ursus
americanus) is one of the shortest chapters although
it is a relatively well-studied and endangered mammal
that is in need of a comprehensive management pro-
gramme. There is almost no mention of its conservation
status or of its economic importance, and the chapter
is not much changed from the first edition. In contrast,
the longest single-species account is for the Bison
(Bison bison), a highly managed species with very few
free-ranging individuals. The text has been substantially
revised from the original account and is one of the
more thoroughly covered species. Within the multi-taxa
chapters, the presentation of information was not stan-
dardized, making it difficult to locate specific infor-
mation for comparative purposes. For example, the
seals began with general characteristics for pinnipeds
2004
and then finished with individual accounts for the 16
different species. In contrast, toothed whales included
three detailed and sequential species accounts fol-
lowed by abbreviated discussions on three other
species.
Overall, this revised edition contains some of the
most comprehensive descriptions of mammal species
found in North America. Notwithstanding the afore-
mentioned criticisms, the editors have continued the
fine tradition of thoroughness and scholarship estab-
lished in their first volume. Not only are the accounts
a summary of our biological knowledge of the larger
species but the information also is interpreted and
presented in the context of management and conser-
vation. This book will be the primary reference source
that bridges the gap between applied biology and policy
Book REVIEWS
473
implementation. A companion volume dealing with
the small mammals, and the other half of mammalian
diversity, in North America would be a nice comple-
ment but perhaps wishful thinking for others to under-
take. One noticeable drawback is that the publication
is expensive, which will discourage students, researchers,
and government workers from purchasing it for their
personal library. This book, however, is a required
monograph for institutional and departmental libraries
that have an interest in not only mammals and their
conservation or management but also wildlife ecology,
in general.
BURTON K. LIM
Centre for Biodiversity and Conservation Biology, Royal
Ontario Museum, 100 Queen’s Park, Toronto, Ontario
M5S 2C6 Canada
| Pete Dunne on Bird Watching: The How-to, Where-to and When-to of Birding
By Peter Dunne. 2003. Houghton Mifflin, 222 Berkeley Street,
Boston, Massachusetts 02116. USA. 352 pages. U.S. $12.
Birdwatching is one of the fastest growing outdoor
activities in North America. Once the obsession of a
few, it is now firmly lodged in the mainstream. Bird
books have proliferated, the optical equipment gets
better every year, and birding clubs and media are now
commonplace: there are even television shows about
birding. With all these riches, what is a novice to do?
Pete Dunne’s latest work is a good place to start. With
this cleverly thought out book, Pete Dunne starts at
the beginning and provides the tools and tips to make
birding a lifelong journey of discovery.
The author is a gifted communicator and teacher,
making the material accessible and a fun read, while
at the same time packing dozens of tools and tips into
three hundred information-filled pages. The place he
Starts is the backyard — precisely the place where many
people first get hooked on birds. He then walks the
reader through the tools of the trade, the fundamen-
tals of birding, applied birding (“for fun, purpose...
| even profit!”), eventually bringing the reader full cir-
_ cle to ethics and a solid conclusion that reminds us of
_ why we birdwatch. Each chapter ends with a useful
_ summary of key learning objectives, which helps to
_ hammer home the important points. He keeps the
| material alive by interspersing anecdotes from his own
rich experience, and others gleaned from a veritable
who’s who of North American birding. There are plen-
ty of photos (black-and-white, this is no coffee table
| book) to illustrate points the author wants to make.
| The author’s dry wit frequently surfaces, so be pre-
_ pared for the occasional good laugh.
Some of the advice is priceless, particularly ten key
questions to ask when identifying a bird, and a sec-
tion entitled “learning to see.” This is complemented
by practical advice on things like how to pick binoc-
ulars, field guides and spotting scopes. For example,
_ the author provides a helpful hint on how to check to
see if that great pair of binoculars you are thinking of
buying is in alignment; if they are not, your eyes will
suffer.
There is also plenty of advice — generic and specific
— on “where to go” and how to maximize your birding
once you get there (my favorite: “the power of the
pause”, wait, and birds will show up). He also talks
about how to contribute to the store of knowledge
while having good fun, for example by participating
on Christmas Counts and Breeding Bird Atlases. In
the final chapters the author notches the level up sev-
eral grades, letting novice birders in on some of the
inner secrets of successful birders like how to be where
and when the birds are. He even divulges the secret
of the perfect Eastern Screech Owl imitation (I’m not
telling, you will have to read the book to find out.)
Are there things I do not like about this book? Not
many, but there are a few. The format, with plenty of
inserts, is occasionally disconcerting, particularly some
of the “‘insider’s insights” with sometimes abrupt shifts
from the author’s voice to another, in one case into a
lecturing tone thankfully absent in the rest of the book.
Sometimes the order of things is confusing, for exam-
ple the discussion on spotting scopes is widely sepa-
rated from that on binoculars. While this follows a
logical sequence (most birders start with binoculars
and only “graduate” to scopes later on in their birding
careers) is does seem misplaced. The advice provided
is solid and if followed will make for better birders,
but there are a few minor missteps. For example, the
author perpetuates the oft-repeated myth that European
birds are less responsive to squeaking than those in
North America — not true in my experience. The book
is also unabashedly North American centric; there is
very little here about the rest of the world. Occasion-
ally the book drifts towards the advertorial, for example
a limited number of bird tour companies are high-
lighted, but generally the author strikes the right bal-
ance. There is one point in the book that I objected
474
to, and that was the description of the author, in a line
with a dozen other birders, wading through a long
grass prairie in an attempt to flush a Baird’s Sparrow.
While this anecdote was properly set in a discussion of
ethics (he stepped on a grouse nest) the action described
was out of character with the rest of the book (or even
the advice provided in the rest of the book) and the
ethical dimensions could have been more forcefully
argued. These points do not seriously detract from the
book, and I would rank it among the best birding “how-
to” books I have encountered.
BOTANY
THE CANADIAN FIELD-NATURALIST
Vol. 118
This book is aimed at the novice. If you have just
started birding, this book is for you. If you know some-
one who has just started, this book would make a great
gift. You may even want to lend it to your spouse,
friends or relatives; anyone who is trying to figure out
what all the fuss is about. Better still: donate it to the
local school library after you are done with it. Will
there be more to learn after you put this book down?
Absolutely, but that is the whole point of the book:
birding is a lifelong discovery.
MARK GAWN
1354 Viking Drive, Ottawa, Ontario K1V 7J6 Canada
Alpine Plants of North America: An Encyclopaedia of Mountain Flowers from the Rockies to
Alaska
By Graham Nicholls and Rick Lupp, Consulting Editor. 2003.
Timber Press, 133 SW 2nd Avenue, Ste. 450, Portland,
Oregon 97204 USA. 344 pages. U.S. $49.95. Cloth.
Entitled Alpine Plants of North America, this 344 page
book takes an all-embracing look at many of nature’s
floral delights, which the author explains as being cate-
gorized as alpines, though they may be found any-
where from seaside to high mountain. Mr. Nicholls
wins my applause by telling us that he likes to limit
his plants to 30 cm (12 inches) in height, which I find
keeps plants in scale in an average home rock garden.
The title might be a bit amusing to a Canadian — it
appears to have been accomplished by excluding any
plant references to land we hold dear! We are told the
book is intended for practical, on site use, both in the
field and in an owner’s garden — generally Graham
has succeeded but he falters a bit in the area of plant
identification — something which is vital to enthusias-
tic alpine plant lovers. May I suggest that a few less
species photographs and more emphasis on their clarity
(there were a number of photos from which identifi-
cation would be difficult if not impossible). More close-
ups of flowers and foliage would help a great deal.
I thought that the format of the book was excellent:
information on plants’ natural growing areas and cul-
tural tips made for a most helpful package of useful
information. Choosing the best location and growing
medium for our newest acquisitions is very often a
painful experience. Having several identical plants and
plenty of spare sites is sometimes our best hope of
Arboretum America, A Philosophy of the Forest
By Diana Beresford-Kroeger. 2003. University of Michigan
Press, 839 Greene Street, Ann Arbor, Michigan 48104-
3209 USA. 196 pages. U.S. $29.00.
Arboretum America, A Philosophy of the Forest is
a unique work. It’s a book about trees in a compound
context — global, local and personal — informed by an
success. However, a careful reading of the needs of each
species covered in this book should save many early
plant funerals!
The introduction of little known species is great fun
and I applaud Mr. Nicholls’s inclusion of Talimums
in his writing. I have only one species in my collec-
tion to date — T. selinoides — but after seeing photos
of such beauties as T. brevifolium, and T: *Zoe’, I shall
be very soon searching for more. It is most amazing
to observe the miniature size, quantity and length of
blooming period in this enjoyable plant.
It is refreshing to find a proven plantsman willing
to share his knowledge of plant propagation so freely.
This is most evident in his detailed directions concern-
ing the taking of cuttings from various species of Phlox.
Perhaps his most helpful writings in this area are the
descriptions of each species’ natural surroundings, soil
conditions, and moisture tolerance. The book entices
the reader to find suppliers of seeds, plants, or best of
all to follow in Graham Nicholls’ footsteps — to see at first
hand the alpine specimens he has so carefully covered.
Both author Graham Nicholls and consulting editor
Rick Lupp have done a magnificent job in producing
a book of much needed information about the identi-
fication and growing of alpines and done it in a neat,
readable, and orderly fashion. This book will give the
reader true value for his or her money.
WILLIAM BARKER
8 Stonecroft Terrace, Kanata, Ottawa, Ontario, K2K 2T9
Canada
intriguing variety of perspectives, including ecology,
ethnobotany, horticulture, ethnology and mythology.
The result is an eclectic and appealing book, no great
surprise considering that the author, Canadian Diana
Beresford-Kroeger, is, according to the back cover, a
“botanist, medical and agricultural researcher, lecturer
and self-defined “renegade scientist” in the fields of
2004
classical botany, medical biochemistry, organic chem-
istry and nuclear chemistry.”
The book starts with an introduction that includes
appealing stories from Beresford-Kroeger’s child-
hood, a discussion of the world as a global garden, a
definition of Beresford-Kroeger’s concept of “bio-
planning’’(covered in her previous book Bioplanning
a North Temperate Garden), and a description of how
bioplanning applies to forests. She then goes on to
profile 20 North American tree groupings, including
— genus followed by common name — Acer (Maple),
_ Asimina triloba (Pawpaw), Betula (Birch), Carya
(Hickory), Catalpa (Catalpa), Crataegus (Hawthorn),
Fraxinus (Ash), Gleditsia (Honey Locus), Juglans
nigra (Black Walnut), Magnolia acuminata (Cucum-
ber Tree), Ostrya virginiana (Hop Hornbeam), Pinus
(Pine), Ptelea trifoliata (Wafer Ash), Quercus (Oak),
_ Sambucus (Elderberry), Sassafras (Sassafras), Thuja
occidentalis (Cedar), Tilia (Basswood), Tsuga (Hem-
| lock), Ulmus (Elm).
It’s puzzling, this choice of trees. Why these group-
ings and not others? Why include elderberries and
leave out dogwoods, why hemlocks and not firs, why
_ birches and not aspens? The author never tells us why;
_ never explains her inclusion and exclusion criteria.
And I can’t help but wonder, as I wander the fields
_ and forests of home, about the cherries and beeches,
_ tamaracks and spruces ... should they not be includ-
ed in forest bioplanning too?
That little grievance aside, the book is vibrant and
_ delightful, with much to teach from the wide range of
_ perspectives mentioned earlier. Each profile includes
_ six sections: “The Global Garden”, tracing the history
and geography of each tree grouping; “Organic Care”,
_ covering related horticultural topics; “Medicine”,
discussing traditional and potential medicinal uses;
“Ecofunction”, describing the trees’ ecological roles;
_ Cape Cod Wildflowers: A Vanishing Heritage
By Mario J. DiGregorio and Jeff Wallner. 2003. University
Press of New England, One Court Street, Lebanon, New
Hampshire 03766 USA. 169 pages. U.S. $19.95.
_ This is a reprint of the original volume first pub-
_ lished in 1989 by Mountain Press Publishing Company,
_ with a new introduction by the authors. As the authors
| state, “This book is an appreciation, a guide, and a
_ plea for protection. On one hand it explores the arcane
_ lore of the medieval herbalists... On the other, it chron-
icles the latest scientific understanding of flowers’
ecological importance and current attempts to pre-
serve natural diversity.”
If not unique, this book is at least one of very few
examples of this particular approach to botanical
description. It is arranged in chapters based upon habitat
types, all common to the Cape Cod area. Each habitat
is described in the opening of its chapter. The habitats
_ include woodlands; ponds and bogs; sandplains; salt
Book REVIEWS
475
“Bioplan”, explaining how the trees have been and
could continue to be incorporated into human envi-
ronments; and “Design”, about the trees’ appearances
and aesthetic properties.
Much of the information was new to me. Like a
maple biochemical, acerin, currently being investi-
gated for antiviral and antibiotic qualities. Like the
birch being one of the two sacred trees given to the
Aboriginal peoples of North America. Like pines con-
tributing numerous important air-freshening com-
pounds to the atmosphere. Like hawthorn fruit being
called a “pome” which, along with the leaves, pro-
duces a number of biochemicals which form a high-
energy compound beneficial to migrating birds. Like
basswoods producing huge crops of nectar at a time
when bees need it desperately and many other flow-
ering plants have stopped blooming.
The profiles are interspersed with photographs of
other members of the forest community — lichens,
fungi, flowering plants, shrubs — which help enhance
the bioplanning concept and paint a larger picture of
the forest ecosystem. And the occasional yellow boxes
with relevant stories from the author’s life add a pleas-
ing personal touch.
One of the most personal touches in the book appears
at the end of the introduction, where Beresford-Kroeger
shares with us her dream “that a moratorium will be
put on the cutting of what is left of the global forests
and that ordinary people with an acorn and a shovel
begin the long road back to nature.” Ordinary people.
That’s me. Though I don’t know if I have any acorns
around. But there’s a collection of shovels in the gar-
den shed, and space along the fence. Perhaps I could
manage to find a handful of maple keys ...
R. SANDER-REGIER
RR5 Shawville, Quebec JOX 2YO Canada
marshes; and dunes and beaches, with an additional
chapter to accommodate alien species.
Each habitat type is represented by ten to fifteen
species endemic to each area. As the authors admit,
the sampling is limited in scope, covering only 66 of
the 1300 species of vascular plants found in the Cape
Cod area. Each species is covered on facing pages,
with the left-hand page containing a description of the
plant and other comments on such aspects as propa-
gation and threats to its environment. A colour photo-
graph of the flower is located on the right hand page.
The authors could have, however, spent a little more
time in researching their data, especially since this is
the second edition of their work. The pollination process
of Cypripedium acaule, for instance, suffers from the
following extremely fanciful and highly inaccurate
description. “Drawn by the promise of a sugar “high”
from the nectar inside, insects enter through the slit...
On the way out the insect is plastered with a natural
476
glue on which, in turn, pollen is dusted. Emerging from
the flower with cargo (of pollen) and payment (in nec-
tar) the insect goes to another flower where, in the same
intricate exit process, some of the pollen is deposited
on the stigma to fertilize the plant and produce new
seed.” Of course, Cyp. acaule has no nectary, therefore
there is no payment in nectar; pollen is not dusted;
and the picture of an insect “plastered with natural
glue” is entirely missleading. Because the above pas-
sage occurs in chapter one, a suspicion tends to be
THE CANADIAN FIELD-NATURALIST
Vol. 118
planted early as to the accuracy of the rest of the text.
The authors are to be commended in producing a
book dedicated to the ever growing threats to our nat-
ural environment. Although the scope of this volume
is limited to the Cape Cod area of Massachusetts, its
message could equally apply to almost anywhere in
North America.
WILLIAM R. ARTHURS
1228 Lampman Crescent, Ottawa, Ontario K2C 1P8 Canada
Lewis Clark’s Field Guide to Wild Flowers of the Sea Coast in the Pacific Northwest
Compiled and photographed by Lewis J. Clarke, edited and
composed by John G. Trelawny. 2004. Harbour Publishing
P.O. Box 219, Madeira Park, British Columbia VON 2HO
Canada. 80 pages. Second Edition.Canadian $12.95.
The first edition of this beautiful little book was pub-
lished by Gray’s Publishing Limited, Sidney, British
Columbia, in 1974 and numbered 64 pages. In this sec-
ond edition which numbers 80 pages, John Trelawny
has made some changes in the introduction and includ-
ed some acknowledgements. Like the first edition,
the pages are not numbered, but each species and the
accompanying descriptive text is numbered sequen-
tially so that they can readily be found from the index
which includes both scientific and common names.
The 95 flower pictures in this second edition are
absolutely beautiful and in many are somewhat clearer
than those in the first edition because of more modern
technology in producing them from the photo slides
and like the 1974 edition each photo has a scale mark-
er which gives the size of the picture in relation to the
average plant size. A glossary at the end of the volume
depicts various leaf shapes and flower parts to aid the
user in understanding the descriptive text which ac-
companies each photograph. New plant photographs
have been provided by T. & S. Armstrong, M. Barker,
Ugo Cagnetta, W. Merilees, F. Pratt, H. Roemer, W.
van Dieren, and M. Wheatley.
WILLIAM J. Copy
Biodiversity, National Program on Environmental Health,
Agriculture and Agri-Food Canada, Research Branch, Wm.
Saunders Building, Central Experimental Farm, Ottawa,
Ontario K1A 0C6 Canada.
Wild Flowers of Field & Slope in the Pacific Northwest
By Lewis J. Clark. 2002. Harbour Publishing, P.O. Box 219,
Madeira Park, British Columbia VON 2HO Canada. 108
pages.Canadian $9.95. Paper
Wild Flowers of Forest & Woodland in the Pacific Northwest
By Lewis J. Clark. 2003. Harbour Publishing, P.O. Box 219,
Madeira Park, British Columbia VON 2HO Canada. 100
pages. Canadian $12.95.
Wild Flowers of the Mountains in the Pacific Northwest
By Lewis J. Clark. 2003. Harbour Publishing, P.O. Box 219,
Madeira Park, British Columbia VON 2HO Canada. 106
pages. Canadian $12.95.
These three books contain absolutely beautiful colour
photographs. The photographs are numbered sequen-
tially and each one has a marker [0.5] to indicate its
size and is accompanied by a printed paragraph with
the common and scientific names, a detailed descrip-
tion, together with the habitat and range, and a number
to indicate its sequence in the book. There are 108 in
the first book, 100 in the second and 106 in the third.
There is a four or five page interesting introduction at
the front of each book and an index, glossary and a
list of Additional Field Guides available from Har-
bour Publishing at the end. There are most interest-
ing pictures on the front covers of each book. On the
back covers there is a note about the author, Dr. Lewis
J. Clark together with a map of the Pacific Northwest
on which there are shaded areas depicting where the
wild flowers can be found. All are elegant.
WILLIAM J. Coby
Biodiversity, National Program on Environmental Health, Agri-
culture and Agri-Food Canada, Wm. Saunders Building, Cen-
tral Experimental Farm, Ottawa, Ontario K1A 0C6 Canada
2004
ENVIRONMENT
BooK REVIEWS
477
Conserving Living Natural Resources in the Context of a Changing World
By Bertie Josephson Weddell. 2002. Cambridge University
Press, 40 West 20th Street, New York, New York 1001 1-
4221 USA. 426 pages. £70 Cloth, £24.95 Paper.
Conserving Living Natural Resources in the context
of a changing world is an excellent information source
for anyone interested in natural resource management;
in the evolution of attitudes, mainly North American,
and knowledge regarding natural resources; in the
development, over time, of the relationship between
human beings and the natural environment — or any
combination of the above.
Weddell writes in the preface that she designed the
book as an introduction to natural resource conserva-
_ tion for students, and as a review for managers. As such
' it covers three different approaches to natural resource
_ management — utilitarian, preservationist, and sustain-
able-ecosystem — in more or less chronological order.
For each approach, Weddell traces the historical
conditions that set the stage for that type of resource
management and discusses its strengths and weakness-
es. She also explains the approach’s central concepts,
both philosophical and scientific, and describes its
principal techniques. Weddell makes sure to empha-
size why it is important to learn about the different
approaches, even if certain aspects are now slightly
outmoded. She makes four excellent points: (1) that
there is no single correct way to manage natural re-
sources; (2) that our generation has not necessarily
discovered “the truth”; (3) that it is important to under-
stand how we got to where we are today so that we
can learn from our mistakes; and (4) that some of the
approaches discussed in the book, even if they are
out of date, are still widely applied today.
Part I of the book, “Management to maximize pro-
duction of featured species — a utilitarian approach to
conservation’, discusses the commodification of re-
sources, the impacts (habitat alteration, species de-
clines, extinctions) of the commodification, and the
responses (regulation, protection) to those impacts. It
_also traces the development of the discipline of natu-
ral resource management, describes the central concepts
of the utilitarian approach (population growth, inter-
actions between populations, habitats), and explains
_ its main techniques (harvest management, habitat man-
agement, management to minimize conflicts between
pest species and people).
In Part I, “Protection and restoration of populations
_ and habitats — a preservationist approach to conserva-
tion”, Weddell describes economic and demographic
changes after World War II, and discusses the in-
creasing awareness of ecological problems during that
period (invasive species, toxic substances, ongoing
extinctions). She also covers the rise of preservationist
management, its central concepts (causes of extinction,
speciation, classification), and the principal techniques
relating to species protection and restoration, and to
ecosystem protection and restoration.
In Part ILl, “Management to maintain processes
and structures — a sustainable-ecosystem approach to
conservation”, Weddell provides an overview of more
recent pressures to move beyond the protection of
species and reserves, including practical, scientific,
political, ethical and philosophical considerations. She
also traces the rise of sustainable-ecosystem manage-
ment, describes its central concepts (equilibrium the-
ories, the flux of nature), and discusses two main tech-
niques: conserving natural processes and contexts, and
including people in the conservation process.
The book covers a lot of ground, much of it fairly
complex, and it isn’t short. But Weddell’s clear and
simple writing style makes the content is easy to read
and understand. And she includes lots of helpful dia-
grams and dynamic examples. It all makes for -pleas-
ant and highly informative reading — particularly the
historical background sections, which provide a valu-
able and relevant context for understanding the disci-
pline of natural resource management.
Weddell closes the book by emphasizing that each
of the natural resource management approaches — utili-
tarian, preservationist and sustainable-ecosystem — has
much to teach us about solving contemporary problems.
She stresses that each approach has advantages and
disadvantages that make it appropriate to particular
circumstances, and that it is possible to blend elements
from all three approaches.
She also points out, and I quote: “I believe that as
we continue to search for responsible ways to manage
living natural resources, a large dose of humility is
appropriate. Science, whether theoretic or applied, is
an ongoing process.... Although our understanding of
the natural world is more detailed than it used to be,
there is still a lot we do not know. Management should
err on the side of caution, therefore. There will always
be surprises.” Wise words.
R. SANDER-REGIER
RRS5 Shawville, Quebec JOX 2YO Canada
478
THE CANADIAN FIELD-NATURALIST
Vol. 118
Visions of the Land: Science, Literature, and the American Environment from the Era of
Exploration to the Age of Ecology
By Michael A. Bryson. 2002. The University of Virginia Press,
Box 400318, Charlottesville, Virginia 22904-4318 USA.
228 pages. U.S. $16.50. Paper.
Visions of the Land, part of an “Explorations in
Ecocriticism” series, is an interesting look at the rela-
tionship between science, the natural environment and
human beings, as expressed in literature published in
the United States from, as the subtitle suggests, the
period of exploration in the 19" century to roughly
the 1960s. Some aspects of that relationship would
also apply to Canada.
The authors examined in the book cover quite the
range — from explorers John Charles Frémont (Amer-
ican West) and Richard Byrd (polar regions), to author
and feminist Charlotte Perkins Gilman, naturalist Susan
Fenimore Cooper, and scientists John Wesley Powell,
Rachel Carson and Loren Eiseley. The types of writ-
ing also vary widely — from exploration narratives
and technical reports, to fictional utopias, natural his-
tories, popular scientific literature, and more.
The book is divided into three parts: |. Narratives
of Exploration and the Scientist-Hero (Frémond and
Byrd); 2. Imagined Communities and the Scientific
Management of Nature (Powell and Perkins Gilman);
and 3. Nature’s Identity and the Critique of Science
(Fenimore Cooper, Carson and Eiseley). The book’s
sub-title suggests a certain chronological order in the
material, but that turned out not to be the case, which
made reading and comprehension a little confusing.
It was also a little difficult to follow the author’s argu-
ments through the themes covered in the three parts. I
would have found it more effective had Bryson sim-
ply written a chapter on each of the authors.
Nevertheless, there is lots of good content in the
book regarding science and connections with human
perspectives on the natural environment. Frémont, for
example, was the “glamour boy of American westward
expansion”, the archetypal macho scientist-explorer,
who worked and wrote both scientific reports and
popular literature at a time when the country was ex-
panding ever faster westward, and when surveying
technology and cartographic techniques were contin-
ually improving. Frémont’s writing combines descrip-
tive and poetic elements with analytical, quantitative
elements. The science he practises and expresses is
highly rational and empirical, and the land something
to be studied, catalogued and mapped.
John Wesley Powell, featured in Part 2 of the book,
is another fascinating character in the history of the
American West. An explorer-scientist like Frémont —
as well as an ethnologist, philosopher, writer and gov-
ernment leader — Powell was, according to Bryson,
“one of the most important and influential scientists
of his age.” Powell’s work emphasises the scientific
control of a mechanistic nature while at the same time
recognising nature’s self-regulating properties and the
need for careful settlement and agricultural practices.
Powell is aware of and interested in community, par-
ticularly with respect to the need for human commu-
nities to develop a responsible relationship with nature
and to use science wisely.
Susan Fenimore Cooper, featured in Part 3, is one
of the two non-scientist writers discussed by Bryson,
although she was a dedicated naturalist and keen
observer. Her work falls into the 19" century natural
history writing tradition which helped inform the
ecological science developed in the following century.
Her book, Rural Hours, published in 1854, combines
natural history, cultural analysis and personal stories
to create an environmental and social portrait of her
home region in central New York state. Bryson finds
Rural Hours fascinating “not only because it com-
bines multiple strands of the nature writing tradition
but also because it provides a complex and fairly sub-
stantial critique of the relation between nature and
the human community.” Fenimore Cooper views sci-
ence not as something which can be used to objectify
or control nature, unlike Frémont or Powell. Science,
in her view, is a “system of study meant to foster
moral and intellectual connections between the
observer and the outside world.”
I learned a lot about the evolution of scientific
thinking and its influence on the human-nature rela-
tionship in Visions of the Land. 1 also discovered some
fascinating writers and books — ones I’m sure to look
up and enjoy in the future.
R. SANDER-REGIER
RRS5 Shawville, Quebec JOX 2Y0O Canada
Genetics, Demography and Viability of Fragmented Populations
Edited by A. G. Young, and G. M. Clarke. 2000. Cambridge
University Press, 40 West 20th Street New York, New York
10011-4221 USA. 438 pages. Canadian $63. Paper.
This is another Australian CSIRO (Commonwealth
Scientific and Industrial Research Organization) flag-
ship publication of international importance to research
and conservation. “The continuing global trend towards
non-sustainable exploitation of natural resources means
that more, rather than fewer, species are going to be
affected by habitat loss, degradation and fragmenta-
tion in the future”. The editors of this important book
make it clear that the species of this globe will either
have to survive in zoos, or in smaller fragments. For in-
stance, the range of many Australian mammals declined
already by over 90% and is now confined to off-shore
islands; and in New Zealand the native forest cover has
already been reduced from 78% in pre-human times to
23% today. Obviously, for many plants and animals
in the world, preservation with relatively intact habitats
is no longer an option.
2004
Already Darwin (1876) had documentated inbreed-
ing depression in both cultivated and native plant spe-
cies. The two major goals of modern conservation gen-
etics are the maintenance of genetic variation and the
avoidance of inbreeding depression.
This book consists of three parts (Introductory Con-
cepts, Animal and Plant Case Studies) and includes
20 research papers from 42 international authors. Most
of the contributors come from the southern hemi-
sphere (Australia and New Zealand) as well as from
the English speaking research sphere (USA, UK).
However, their research applications come from many
parts of the world and cover the variety of the animal
kingdom (Red-cockaded Woodpecker, Golden Lion
Tamarins, Mexican Wolves, Bonytail Chub, Chinook
~ Salmon, Golden Sun Moth, Desert Bighorn Sheep,
small mammals) and a variety of plant species. The
plant section is of special interest here as plants are
used to present genetic mechanisms transferable to
animal populations and their conservation. It even
includes an endangered dry forest tree species (Swi-
etenia humilis) in Central America now listed with
CITES (as are two Mahagoni tree species; formerly of
major economical value). I also admire the 54 pages
_ of references and a detailed book index.
Although local extinction is not infrequent to observe
in nature “Habitat destruction is the most obvious cause
of species decline and the most difficult to reverse”.
Recent fragmentation shaped the global landscape
nowadays, which has nothing to do anymore with the
original habitat. This books makes a pledge that we
need to find a limit how we affect the global environ-
ment. “The techniques for doing so will come more
from economics, psychology and sociology rather than
from biology”. However, as the editors show, biology
has an important role to play beyond identification of
species and ecosystems.
It’s a challenge to find the right gene that determines
inbreeding in a cost-effective way. The book is full of
GGTGCTAGs, Dendrograms, Nei Genetic Distances,
Phylogenies etc. The presented papers report in great
detail on DNA extraction and processing methods such
_as PCR, but less so on statistics. Commonly applied
software packages and methods to derive evidences are
|GENEPOP, GenAIEx, SPARKS, PROC INBREED
(SAS), PCA, bootstrapping, VORTEX and RAMAS.
Authors conclude that relying entirely on neural molec-
ular markers is inadequate. Most of the presented gene
studies in this book are based on mtDNa and Allo-
zymes; microsatellites might track fragmentation pro-
cesses quicker.
_ Concepts and terms like Minimum Viable Popula-
tions (MVP) metapoluation paradigm, effective pop-
ulation size, rescue effect, simulation models, demog-
-taphy, transition matrix and the movements of pests,
pathogens and predators are discussed as well. Some
of the presented studies cover a period of over 10 years.
The well known study on Cheetah inbreeding effects
(e.g., population decline, susceptibility to disease)
‘Temains controversial. But in Bighorn Sheep, high
Book REVIEWS
479
heterozygosity is known to be associated with large
horn size at sexual maturity, which confers breeding
superiority. It is worthwhile to note that over the last
200 years alone 98% of Desert Bighorn Sheep popu-
lations have been reduced.
This complex publication makes for a bible on
fragmentation as being genetically harmful.
Much of the book deals with the landmark publi-
cations by Caughley (1994) and Lande (1988) and pro-
vides further evidence and research on these topics. It
is in support of the classical conservation arguments;
e.g., Those brought forward by Soulé. The book some-
what promotes the Australian conservation view, which
might not necessarily be shared world-wide. For in-
stance, the foreword cites Randal O’ Toole (1999) who
stated that “conservation biology is not a science but
a political movement based at least in part of nine-
teenth-century ideals of what an ecosystem is all
about”. The reader of this book will definitely learn
that genetic loss will have negative effects on econom-
ic and physical well-being. “Each extinction erodes
the biological legacy, and humanity slips away. Stew-
ardship for the planet and its inhabitants will have
been lost, replaced by greed, ignorance, and short-
sightedness”. Brooks (1997) contemplated already that
“while the ship is sinking, conservation geneticists are
busy counting the deck chairs”. The contributing authors
to this book make a case for managing through genet-
ics; they are frank about the fact that many problems
with endangered species cannot be solved with
genetic techniques alone but that genetics will allow
for much more informed decisions. As the authors
show, true population estimates are hard to get from
field work, and DNA offers major opportunities to infer
some basic life-history, demographic and population
parameters.
I am very glad that this book stresses the impor-
tance of spatial issues for PVA, but true GIS papers
are unfortunately not presented. Some papers deal
indirectly with what can be defined as Landscape
Ecology though. Readers will also appreciate the great
summary of the most important elements of a suc-
cessful PVA. Some really good model philosophy is
presented, too. PVAs are coined as a “loaded gun”
pointing towards economics and others. The book
deals nicely with data uncertainties in PVAs, PVA
acceptance in the research community and PVA appli-
cations, too. “Incomplete information does not mean
that meaningful results are impossible to obtain because
there is very significant value in building a model for its
own sake”, e.g., as a guide for further data collection
and bringing stakeholders together. A key argument
is that a PVA compares risk, but does not measure it.
Besides the many other interesting and important
papers in this book I, personally, really like the one
dealing with the faunal collapse and genetic erosion
in small mammal communities on islands in the Chiew
Larn reservoir in Thailand: it’s an island habitat mile
stone study with a 10 year data set.
480
The presented plant studies are very valuable because
plants as well as their response to habitat loss and frag-
mentation, are usually understudied. The pollination
papers show nicely that fragmentation has to consider
pollinators (bees and butterflies), too, besides the pollen-
mediated gene flow.
The correlation between population size and genet-
ic diversity is clear. This book supports the view that
it is increasingly apparent that the consequences of
fragmentation are dependent upon complex interactions
of demographic and genetic variables. However, the
relative importance of demography vs. genetics for
conservation of small populations or rare species is
still debated. In either case, inbreeding and reproduc-
tion failure alone have limited demographic effects.
However, when both are combined, and certainly when
applying the “precautionary principle” in conservation,
the two result in significantly reduced population
persistent times. The authors show well that multidis-
ciplinary approaches are crucial but that there is a
large degree of discipline rivalry perpetuated by the
structure of university faculties and departments and
by the patterns of research funding worldwide. DNA
A Primer of Ecological Genetics
By Jeffrey K. Conner and Daniel L. Hartl. Sinauer Associates,
Inc., Publishers, 23 Plumtree Road P.O. Box 407, Sun-
derland, Massachusetts 01375-0407 USA. 304 pages.
U.S. $47.92.
Recent developments in molecular biology have
lead to the application of increasingly sophisticated
genetic techniques to ecological questions. A primer
of ecological genetics serves as an introduction to
this rapidly expanding field. The intended readers for
this book are advanced undergraduate and graduate
students who will find it a valuable resource in their
studies. The authors also suggest that professional
biologists will benefit from the material presented,
but I don’t think this audience is as well served.
The book starts with the basic concepts of population
genetics, including a review of the most commonly
used molecular markers. Conner and Hartl then guide
the reader through theoretical and empirical advances
gained from two complementary approaches to this
field. The first is the study of genetic variation in nat-
ural populations. Observed levels of genetic variation
are routinely used to assess breeding systems, migra-
tion, and differentiation within and among popula-
tions, making a sound understanding of this material
essential for anyone working in conservation biology.
The second approach, quantitative genetics, deals with
insights gained from experimental studies. While much
of the relevant literature addresses breeding programs,
the authors argue convincingly for the value of quan-
titative genetics in studying natural populations.
A detailed discussion of natural selection follows,
and the closing chapter of the book covers some of
the major applications of population genetics — con-
THE CANADIAN FIELD-NATURALIST
Vol. 118
studies must remain incomplete as long as prey, pre-
dation, landscape and other factors get ignored.
Unfortunately, data reported upon in this book are
not freely available in a digital format for the public,
nor is that fact anywhere in this book emphasized; the
important topic of Metadata is not mentioned either.
This does not add to transparent decision making in
conservation and should be considered in any study.
As this book once more shows very clearly, “cur-
rently, we do have tools available to us that we are not
using”. If there is something to criticize in this book
then: Why do we produce, and focus on, superb sci-
ence, whereas most of our governments and the public
are over 15 years behind in their actions and implica-
tions towards efficient conservation? In the meantime,
the global landscape will be further exploited, with book
shelves getting bigger. This excellent book calls for
action: Management considering genetics is required.
FALK HUETTMANN
Institute of Arctic Biology, Biology & Wildlife Deptartment
Fairbanks, University of Alaska, Fairbanks, Alaska 99775
USA.
servation genetics, evolution of invasive species, trans-
gene escape, and the evolution of pesticide resistance.
This last chapter is an excellent grounding for the
book, providing concrete examples of the value of
ecological genetics to real world problems.
Overall the book is well thought out, and the authors
succeed for the most part in presenting this complex —
subject in an accessible way. The prominence of quan- —
titative genetics in the text is refreshing. The demands
required for quantitative genetic study have limited its
use in a conservation context. Conner and Hartl may
persuade some researchers to rise to the challenge and
combine observational and experimental work. The
determined individuals that do will likely produce some
very interesting results!
Some of the discussion was over-simplified. The
reader gains a general understanding of the concepts,
but will need to refer to the primary literature or a more
detailed reference to truly master the material. This is
the authors intention, as evidenced by the excellent
selection of current references included with each
chapter, accompanied by discussion questions. In this
light, the book will make a marvellous study guide for
a graduate seminar or senior undergraduate course.
However, professional biologists and conservation
managers are less likely to have the time and energy
to devote to the subject. Expanding the treatment to
make this book a “one-stop” reference would better ©
serve this audience.
TYLER SMITH
155 Vanguard Avenue, Pointe Claire, Quebec H9R 3T4 Canada
2004
MISCELLANEOUS
Book REVIEWS
48]
Smithsonian Institution Secretary Charles Doolittle Walcott
By Ellis L. Yochelson. 2001. Kent State University Press, 307
Lowry Hall, P.O. Box 5190, Kent, Ohio 44242 USA. 590
pages. U.S. $49.00.
This, the second and final volume of Yochelson’s
massive “insider” biography (Yochelson retired from
the Smithsonian in 1985), is clearly a labour of love.
The first volume, Charles Doolittle Walcott, Paleontol-
ogist, appeared in 1998. From Walcott’s daily diaries,
an unusual amount of detail is provided chronologi-
cally, month by month, as a record for future historians.
Fifty pages describe happenings in 1927 alone, when
Walcott was already seventy years old.
Charles Doolitte Walcott was a man of humble and
inauspicious beginnings, without any opportunity for
a college education. In his early twenties he sold a
collection of fossils to Louis Agassiz at Harvard Uni-
versity; a few years later he was offered a job as a
temporary field assistant, measuring the thickness of
rocks in Bryce Canyon, Utah, for the newly formed
United States Geological Survey. A man of great tact
and wisdom, Walcott never looked back; in 1933 the
fifth edition of American Men of Science listed him
posthumously as the third most important geological
scientist in the country, and he collected twelve hon-
orary degrees from as many universities.
Walcott is of enormous importance to Canada. He
spent about three months each summer for 18 of 19
years, 1907 through 1925, studying geology and pale-
ontology in the Canadian Rocky Mountains. In Yoho
National Park, above Emerald Lake, he discovered
the Burgess Shale, rated world-wide by Stephen Jay
Gould as “the most precious and important of all fos-
sil localities.” In addition to his heavy administrative
duties during the remainder of the year, Walcott spent
his spare hours in winter studying and describing
these fossils. This lifelong devotion to his field of sci-
ence is all the more remarkable when one considers
his burdensome official duties. From 1907 until his
death in 1927 he occupied the powerful post of secre-
tary of the Smithsonian Institution. He also served
variously as president of the Paleontological Society,
National Parks Association, American Philosophical
Society, Washington Academy of Sciences, National
Academy of Sciences, and the American Association
for the Advancement of Science, was chair of both the
Carnegie Institute of Washington and the National
Advisory Committee for Aeronautics, and was First
Vice Chairman of the National Research Council and
the American Federation of Arts. One of the most
powerful men in Washington, a mover and a shaker,
Walcott dined with presidents, cabinet members,
supreme court justices, and foreign diplomats. In spite
of these pressures, Walcott was a devoted husband
and father. His chauffeur, butler, furnace stoker, and
loyal family retainer at home in Washington, Arthur
Brown, was also his camp manager, nurse, cook,
general guardian and friend in each of his mountain
camps, and the “unofficial mayor of black Washington.”
Walcott’s first wife, Lura, died of tuberculosis less
than two years after their marriage. Thirteen years
later, in 1888, he married Helena Stevens; their hon-
eymoon was spent looking at rocks in Newfoundland.
Helena was a competent geologist who, at her first
International Congress of Geology in London, Eng-
land, corrected the reversal of Middle and Lower
Cambrian levels previously described for New York
State rocks. According to daughter Helen’s reminis-
cences, her mother Helena was also the first to split
open a piece of Burgess shale, lying by the trail, while
waiting for her husband to climb the scree above. It
proved to have an unusual diversity and complexity
of fossils, included many soft-bellied organisms,
unequalled anywhere in the world. Helena had four
children, all but the oldest of whom accompanied
them on one or more summer geology expeditions to
Canada. Helena died in a train accident in Connecticut
in July 1911, so Walcott had a much shortened field
season that year.
In 1914, Walcott married Mary Vaux, shortly before
her fifty-fifth birthday. A Philadelphia Quaker, she had
measured and photographed, with her father, George
Vaux, the movements of Illecillewaet and other gla-
ciers in the Canadian Rockies, since the 1880s. Mary
took the place of Helena in assisting with fossil col-
lecting, but also painted superb portraits of wildflowers.
Towards the end of his life, Walcott assisted Mary
Vaux Walcott in having the Smithsonian Institution
publish her sumptuous five-volume North American
Wild Flowers, “the monumental ... Audubon of the
floral world.” The alpine flowers were painted while
with her husband in the Canadian Rockies.
Yochelson inserts chatty comments about many top-
ics, including Walcott’s children. Citations are satis-
factory, but index entries are haphazardly incomplete.
I detected nine spelling or typographical errors.
In the final chapter, Yochelson succinctly and con-
vincingly counters some of the grossly unfair impres-
sions left after reading Stephen Jay Gould’s best-selling
Wonderful Life: The Burgess Shale and the Nature of
History. Contrary to Gould’s intimations, Walcott sup-
ported the concept of evolution, “an act of considerable
courage, not an indication that he was hidebound in
his thinking ... Walcott did not propose new classes
and new phyla. The time was simply not ripe ...
Gould has judged Walcott by the context of his own
notions more than half a century later.” Walcott’s
detailed descriptions of the fossil organisms in the
Burgess shale clearly ranks as among the greatest
discoveries in paleontology.
Any reader of this review who has read Gould’s
Wonderful Life, should read Yochelson’s final chapter,
and each library that holds a copy of Gould,should
add this book as well as Simon Conway Norris’ The
NEw TITLES
+Available * Assigned
Zoology
Amphibians and Reptiles of Pakistan. By M. Khan. 2005.
Krieger Publishing, P.O. Box 9542, Melbourne, Florida 32902
USA. No price available.
The Amphibians and Reptiles of El Salvador. By G. Kohler,
M. Vessely and E. Greebaum. Krieger Publishing, P.O. Box
9542, Melbourne, Florida 32902 USA. No price available.
The Anatomy of Reptiles. By J. Wyneken. 2005. Krieger
Publishing, P.O. Box 9542, Melbourne, Florida 32902 USA.
No price available.
*Birds of Australia —- Seventh Edition. By K. Simpson and
N. Day. 2004. Princeton University Press, 41 William Street,
Princeton, New Jersey, 08540-5237 USA. 392 pages. U.S.
$39.50.
Birds of the Raincoast. H. Thommasen and K. Hutchings.
2004. Harbour Publishing, P.O. Box 219, Madeira Park,
British Columbia VON 2HO Canada. 200 pages. Can $44.95.
Cloth.
*A Citizen’s Guide to Ecology. By L. Slobodkin. 2004. Oxford
University Press Canada, 70 Wynford Drive, Don Mills, On-
tario, M3C 1J9. 245 pages. U.S. $14.95. Paper.
Dictionary of Herpetology. By H. Lillywhite. Krieger Pub-
lishing, P.O. Box 9542, Melbourne, Florida 32902 USA. No
price available.
The Exotic Amphibians and Reptiles of Florida. By W.
Meshaka, B. Butterfield and B. Hague. 2004. Krieger Publish-
ing, P.O. Box 9542, Melbourne, Florida 32902 USA.166 pages.
U.S. $34.50.
Experimental Approaches to Conservation Biology. Edit-
ed by M. S. Gordon and S. M. Bartol. 2004. University of
California Press, 2120 Berkeley Way, Berkeley, California
94704-1012 USA. 358 pages. U.S. $75.00.
A Field Guide to the Reptiles and Amphibians of Bali. By
J. L. McKay. 2005. Krieger Publishing P.O. Box 9542, Mel-
bourne, Florida 32902 USA. No price available.Guide to
the Amphibians and Reptiles of Japan. By R. Goris and N.
Maeda. 2004. Krieger Publishing, P.O. Box 9542, Melbourne,
Florida 32902 USA. 296 pages. U.S. $69.50. Cloth.
*Mammals of the World — A Checklist. By A. Duff and A.
Lawson. 2004. Yale University Press, P.O. Box 209040 New
Haven, Connecticutt 06520-9040 USA. 312 pages. U.S. $45.00.
+The Monarch Butterfly — Biology and Conservation. By
K. Oberhauser and M. Solensky (Editors). 2004. Cornell
University Press, 512 East State Street, Ithaca, New York
14850 USA. vii + 248 pages. U.S. $39.95.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Crucible of Creation as a rebuttal. On its own merits,
Yochelson’s book deserves to be in every major library.
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N OJ8
Canada
Our Life with Birds. By J. and G. Tveten. 2004. Texas A&M
University Press, Lewis Street, 4354 TAMU, College Station,
Texas 77843 USA. 256 pages. U.S. $24.95. Cloth.
The Panther Chameleon. By G. Ferguson, J. Murphy, J.
Ramanamanjato and A. Rasselimanana. 2004. Krieger Publish-
ing P.O. Box 9542, Melbourne, Florida 32902 USA. 166 pages.
U.S. $39.50 Cloth.
Penguins of the World. By W. Lynch. 2004. Firefly Books
Ltd., 3680 Victoria Park Avenue, Toronto, Ontario M2H 3K1
Canada. 144 pages. Can $35.00. Cloth.
+ Prairie Ghost — Pronghorn and Human Interaction in
Early America. By R. McCabe, B. Ogera, H. Reeves. 2004.
University Press of Colorado, 5589 Arapahoe Avenue, Suite
206C, Boulder, Colorado 80303 USA. 208 pages. U.S. $29.95.
Cloth.
Snakes of the Americas: Checklist and Lexicon. By R.
Tipton. Krieger Publishing, P.O. Box 9542, Melbourne,
Florida 32902 USA. No price available.
Status and Conservation of Florida Amphibians and Rep-
tiles. By W. Meshaka, and K. Babbitt. 2005. Krieger Publishing
P.O. Box 9542, Melbourne, Florida 32902 USA. No price
available.
*The Wolves of Algonquin Park a 12 Year Ecological
study. By J. and M. Theberge. 2004. University of Waterloo,
Waterloo, Ontario. Contact bkevans@fes.uwaterloo.ca.
Canadian $ 23.50 Paper.
Botany
Biological Control of Invasive Plants in the United States.
Edited by E. Coombs, J. Clark, G. Piper and A. Cofrancesco.
2004. Oregon State University Press, 102 Adams Hall, Cor-
vallis Oregon 97331 USA. 448 pages. U.S. $45.00. Paper.
+ Emulating Natural Forest Landscape Disturbances —
Concepts and Applications. By A. Perera, L. Buse, and M.
Weber. 2004. Columbia University Press, 61 W. 62nd Street,
New York, New York 10023 USA. 352 pages. U.S. $74.50.
Cloth.
*Gathering Moss — A Natural and Cultural History of
Mosses. By R. Kimmerer. 2004. Oregon State University
Press, 102 Adams Hall, Corvallis, Oregon 97331 USA. 176
pages. U.S. $17.95. Paper.
Klamath Heartlands — A guide to the Klamath Reserva-
tion Forest Plan. By E. Wolf. 2004. Oregan State Universi-
ty Press, 102 Adams Hall, Corvallis Oregon 97331 USA. 56
pages. U.S. $19.95. Paper.
2004
Tree — A life Story. By D. Suzuki and W. Grady. 2004. Grey-
stone, #201 — 2323 Quebec Street Vancouver, British Colum-
bia V5T 4S7 Canada. 192 pages. Canadian $28.00 Cloth.
Environment
Death Takes a Gander. By Christine Goff. 2004. CLG,
Box 3280, Evergreen, Colorado 80437 USA. 224 pages.
U.S. $5.99. Paper.
Managing Environmental Policy: A Casebook. By R.
Watson, D. Kiel, and S. Robar. Krieger Publishing. P.O.
Box 9542, Melbourne, Florida 32902 USA. 180 pages. U.S.
$27.50. Cloth.
Prairie — A Natural History. By Candace Savage. 2004.
Greystone, #201 — 2323 Quebec Street Vancouver, British
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Cloth.
The Sacred Balance. By D. Suzuki and A. McConnnell.
2004. Greystone #201 — 2323 Quebec Street, Vancouver,
British Columbia V5T 4S7 Canada. 160 pages. Canadian
$34.95. Cloth.
Young Naturalists
Hummingbirds. By L. Aziz. 2004. Firefly Books Ltd., 3680
Victoria Park Avenue, Toronto, Ontario M2H 3K1 Canada.
64 pages. Canadian $9.95. Paper.
Penguins. By W. Lynch. 2004. Firefly Books Ltd., 3680
Victoria Park Avenue, Toronto, Ontario M2H 3K1 Canada.
64 pages. Canadian $ 9.95 Paper.
484
THE CANADIAN FIELD-NATURALIST
Vol. 118
News and Comment
Froglog: Newsletter of the Declining Amphibian Populations Task Force (63, 64)
Number 63, June 2004. Contents: Status of Three Species
if Toads in North-western Mexico (Georgina Santos Barrera
& Jesus Pacheco Rodriguez) — Ranids to the Rescue! (Jerry
Lea & Luca Luiselli) — Effects of Habitat Loss and Frag-
mentation on Anurans in Espinal Eco-region, Argentina: a
GIS approach (Paola Peltzer, G. Bock, R. Tardivo & R. Laj-
manovich) — DAPF Rapid Response Fund — Reports on
DAPTF Seed Grants — Froglog Shorts.
Number 64, August 2004. Contents: Morphological Abnor-
malities in Frogs of West Java, Indonesia (Mirza D. Kusrini,
Ross A. Alford, Anisa Fitri, Dede M. Nasir, Sumantri Rahard-
yansah — Press Release: Concerns Remain About UV—B
Damage To Amphibians (Andy Blaustein) — New Labora-
tory of Natural Sounds in Cuba (Ansel Fong Grillo) — Reports
on DAPTE Seed Grants (Tim Halliday) — WebFroglog [see
Marine Turtle Newsletter (105)
July 2004. 32 pages: articles: The Status and Conserva-
tion of Sea Turtles in Kenya — Observations of Loggerhead
Turtles Feeding on Discarded Fish Catch, Kefalonia — notes:
Back to the Old Ways — letters to the editor: TEDs 00 —
meeting reports — IUCNMTSG Update — book reviews —
news & legal briefs — recent publications.
The Marine Turtle Newsletter is edited by Brendan J. God-
ley and Annette C. Broderick, Marine Turtle Research Group,
www.opem.ac.uk/daptf and www.open.ac.uk/daptt/froglog]
— Announcements and Meetings.
Froglog is the bi-monthly newsletter of the Declining
Amphibian Populations Task Force of The World Conservation
Union (IUCN)/Species Survival Commission (SSC) and is
supported by The Open University, The World Congress of
Herpetology, and Arizona State University. The newsletter is
Edited by John W. Wilkinson, Department of Biological Sci-
ences, The Open University, Walton Hall, Milton Keynes,
MK7 6AA, United Kingdom; e-mail: daptf@open.ac.uk.
Funding for Froglog is underwritten by the Detroit Zoological
Institute, P. O. Box 39, Royal Oak, Michigan 48068-0039,
USA. Publication is also supported by Peace Frogs
www.peacefrogs.com and by RANA and the US National
Science Foundation grants DEB—0130273 and INT—0322375.
Centre for Ecology and Conservation, University of Exeter
in Cornwall, Tremough Campus, Penryn TR10 9EZ United
Kingdom; e—mail MTN @seaturtle.org; Fax +44 1392 263700.
Subscriptions and donations towards the production of the
MTN can be made online at <http://www.seaturtle.org/mtn/>
or postal mail to Michael Coyne (online Editor) Marine Tur-
tle Newsletter, | Southampton Place, Durham, North Carolina
27705 USA (e-mail: mcoyne @seaturtle.org).
The Boreal Dip Net/L’Epuisette Boreal: Newsletter of the Canadian Amphibian and Reptile
Conservation Network — Reseau Canadien de Conservation des Amphbiens et des Reptiles
8(2) June 2004
Contents: Editor’s Note — Kawartha Turtle Trauma Centre:
Now a Recognized Charity — 2993 Digital Frog -CARCNET/
RECCAR Scholarship Winner Kimberley Pearson (Sara L.
Ashpole) — A Survey if the Status of the Western Toad
(Bufo boreas) in Mount Revelstoke and Glacier National
Parks (Jesse Dykstra) — (Other) Upcoming Meetings: 18"
Annual Meeting of the Society for Conservation Biology
(Danna Schock) — The 9 Annual Meeting of the Canadian
Amphibian and Reptile Conservation Network (CARCNET)/
Reseau Canadien de Conservation des Amphibiens et des
Canadian Species at Risk May 2004
Issued by the Committee on the Status of Endangered Wild-
life in Canada (COSEWIC), the list is 49 pages containing:
About COSEWIC: mandate, membership, definitions —
Summary tables: Species designated in the “risk” and the
Extinct categories and the Not at Risk, and Data Deficient
categories (Tables 1-3) — Results of May 2004 COSEWIC
meeting (Tables 4-5) — Explanation of status change sym-
bols for reassessed species — COSEWIC Assessment Results
— Table 6: Species assessed and designated Extinct: Extinct
Category — Table 7: Species examined and designated in a
“risk category”: Etripated Category, Endangered Category,
Threatened Category, Special Concern Category — Table 8,
Species assessed and found to be on the Not at Risk cate-
gory — Table 9. Species considered and placed in the Data
Reptiles RECCAR) Coast Terrace Inn, Edmonton, Alberta
24-27, 2004 — Seasonal and Diurnal Patterns of Calling in
Eastern Canadian Amphibians: Compiling the conventional
wisdom as a null hypothesis (Frederick W. Schueler with con-
tributions from Wayne F. Weller, John Gilhen, Lenny Shirose,
and Brian Dalzell — Membership in CARCNET/RECCAR
(contact Bruce Pauli, Canadian Wildlife Service, National
Wildlife Research Centre, Carleton University, Raven Road,
Ottawa, Ontario K1A OH3. Web site: http://www.carcnet.ca/).
Deficient category — Record of Status Re-examinations —
Record of Name Changes. Listed as of May 2004 (with
November 2003 totals in parenthesis) are 12 (12) extinct, 21
(21) extirpated, 169 (153) endangered, 114 (102) threatened,
and 140 (143) of special concern. Of the 453 (431) forms in
these categories, 66 (64) are mammals, 60 (56) birds, 32
(31) reptiles, 19 (19) amphibians, 79 (807) fishes, 16 (13)
arthropods, 21 (18) molluscs, 145 (136) vascular plants, 11
(8) mosses, and 7 (6) lichens. In addition 151 (152) forms
have been considered and found not at risk, and 33 (29) to
be data deficient.
This publication is available from COSEWIC Secretariat,
Canadian Wildlife Service, Environment Canada, Ottawa,
Ontario K1A 0H3. See Web site: http://www.cosewic.gc.ca.
484
2004 ERRATUM 485
Erratum Canadian Field-Naturalist 118(2):
Back cover contents omission:
Fifteenth census of seabird populations in the sanctuaries of the North Shore of the Gulf
of St. Lawrence 1998-1999 JEAN-FRANCOIS RAIL AND GILLES CHAPDELAINE 256
Replacement Figure 2, page 161 for
Morphology and population characteristics of Vancouver Island Cougars, Puma concolor vancouverensis,
STEVEN F. WILSON, APRYL HAHN, AARON GLADDERS, KAREN M. L. Gon, AND DAviID M. SHACKLETON
4
@ Female
3 & Male
2 Males:
y = 1.45Ln(x) - 0.54
u R?= 0.70
O |
Ss
6 0
m Females: ®
4 Md @ y = 0.52Ln(x) - 1.09
R? = 0.34
-2
-3
0 2 4 6 8 10
Age (years)
FIGURE 2. Relationship between body size (derived from the principal component analysis on morphological measurements,
see text) and age for male and female Cougars in two Vancouver Island study areas. Logarithmic trend lines are
presented for males (squares m) and females (diamonds ®) pooled by study area. The body size measurement was
used because it was less condition-dependent than using total weight alone.
Minutes of the 125 Annual Business Meeting of
The Ottawa Field-Naturalists’ Club 13 January 2004
Place and time: Canadian Museum of Nature, Ottawa, Ontario, 7:30 p.m.
Garry McNulty, President
Thirty-five persons attended the meeting.
Chairperson:
Attendance:
Attendees spent the first half-hour reviewing the minutes of the previous meeting, the Treasurer’s Report and the Report of
Council. The meeting was called to order at 7:35 p.m. with some opening remarks from Gary McNulty, the President.
1. Minutes of the Previous Meeting
There were no changes to the minutes of the 124" Annual
Business Meeting.
It was moved by Fenja Brodo/David Hobden that the min-
utes be accepted.
(Motion Carried)
2. Business Arising from the Minutes
Garry McNulty inquired whether we were still receiving
the annual reports for the Trinidad and Tobago Naturalists’
Club. Frank Pope reported that we were receiving their annual
reports along with their newsletters.
The Soiree was revamped last year. Changes were made
to the venue and entertainment was included in the course of
the evening. Fenja Brodo, the new chair of the Excursions and
Lectures Committee, will be working with the Education and
Publicity Committee to continue the process of making the
Soiree an evening that members will not want to miss.
3. Communications Relating to the Annual
Business Meeting
There were no communications relating to the Annual
Business Meeting.
4. Treasurer’s Report
Frank Pope reviewed the financial report for the year end-
ing September 30, 2003, noting that the Club’s net assets had
decreased by approximately $60,000. This was due in large
part to the contribution of $55,000 to the Alfred Bog Fund.
Moved by Frank Pope and seconded by Roy John that the
Financial Report be accepted.
(Motion Carried)
5. Committee Reports
Gary McNulty introduced each of the Committee reports
and a representative of the appropriate Committee and asked
for questions and comments. He thanked the committee chairs
and committee members for their work over the past year.
Moved by Mike Murphy/Eleanor Zurbrigg, that the reports
be accepted.
(Motion Carried)
6. Nomination of the Auditor
Moved by Frank Pope, seconded by Bill Cody, that Janet
Gehr continue as Auditor for another year.
(Motion Carried)
7. Report of the Nominating Committee
President Mike Murphy
Vice President Gillian Marston
Secretary Susan Laurie Bourque
Treasurer Frank Pope
Past President Gary McNulty
Business Manager Bill Cody
Editor CFN Francis Cook
Editor T&L Karen McLachlan Hamilton
Committee Chairs
Birds Chris Traynor
Computers
Conservation Stan Rosenbaum
E&P John Cameron
E&L Fenja Brodo
Finance Louise Schwartz
FWG David Hobden
Macoun rep Barbara Gaertner
Membership Dave Smythe
Publications Ron Bedford
FON Rep Cendrine Huemer
Members at large
Kathy Conlan
Diane Lepage
Barbara Gaertner
Christine Lewis
Henry Steger
Chairs not on Council
Awards Ernie Brodo
Macoun Rob Lee
Nominations Fenja Brodo
Retiring from the Council: = Charles Clifford, Roy John,
Marcel Gahbauer,
Eleanor Zurbrigg
New on the Council: Christina Lewis, Henry Steger
Moved by Fenja Brodo, seconded by Frank Pope, that the
slate of nominations for the 2004 Council be accepted.
(Motion Carried)
8. New Business
There was no new business.
9. Presentation by David Hobden, ““FWG
and its Rise to Fame”
David Hobden presented an enjoyable and informative
digital photographic presentation created by Henry Steger and
486
2004
David Hobden. The presentation touched on the develop-
ment and flora and fauna of the Fletcher Wildlife Garden.
The digital format successfully combined prints, slides and
digital pictures. It was very well received.
MINUTES OF THE 125™ ANNUAL BUSINESS MEETING
487
10. Adjournment
Fenja Brodo made an announcement about the upcoming
4"" Annual Great Backdoor Bird Count.
Moved by Fenja Brodo/David Hobden that the meeting
be adjourned at 9:15 pm. (Motion Carried)
SUSAN LAURIE-BOURQUE, Recording Secretary
The Ottawa Field-Naturalists’ Club Committee Reports for 2003
Awards Committee
The Awards Committee met in January to consider nomi-
nations made for the various OFNC Awards. As a result of
our deliberations, the following four awards for the year 2002
were presented at the OFNC’s Annual Soirée, which took
place 26 April 2003 at St. Basil’s Church in Ottawa.
MEMBER OF THE YEAR:
Bill Royds: For his many contributions to the Club’s con-
servation efforts, especially during this last year as the link
between the OFNC and the Greenspace Alliance of Canada’s
Capital (GACC).
GEORGE MCGEE SERVICE AWARD:
David Hobden: For his active participation in the Con-
servation Committee and his enthusiastic, productive work
on the Fletcher Wildlife Garden Committee.
CONSERVATION AWARD — MEMBER:
Philip Fry: For establishing and maintaining the “Old
Field Garden” near Oxford Mills as a model for habitat
restoration and wildflower gardening.
CONSERVATION AWARD — NON-MEMBER:
Michéle André-St. Cyr: For her relentless work in pre-
venting the death of turtles along the highways of southern
Ontario by the establishment of “Turtle Crossing” signs,
and for her active and successful efforts in educating the
public about turtles.
I. BRoDO
Birds Committee
The Birds Committee participated jointly with the Club des
Ornithologues de l’Outaouais to run a successful Christmas
Bird Count in December 2002. The fall bird count was held
again in October 2003 and continues to grow in popularity.
We were again active in the Peregrine Falcon Watch at the
downtown nest site. One female was successfully fledged.
The Bird Record Sub-committee continues to review records
of rare birds and is currently compiling a lengthy database
of Ottawa bird records. The Bird Record Sub-committee
also finished publication of the new Ottawa District Bird
Checklist 2002. The checklist is available in many Ottawa
nature stores. The third year of surveying for the Ontario
Breeding Bird Atlas (Region 24) has been completed. There
are plans to add five more under-surveyed squares from an
adjacent region for the 2004 season. This years seed-a-thon
raised close to $400.00 for the club’s bird feeders. We con-
tinue to operate the rare bird alert and the Ottawa bird status
line, a recorded telephone message of current bird sightings.
Some members of the Committee participated in the Taver-
ner Cup competition
C. TRAYNOR
Computer Management Committee
This year, the Committee reviewed and revised their Terms
of Reference and the revisions were approved by the Council.
It also reviewed the state of the Club’s Membership Data-
base System application. Upon a recommendation by the
Computer Management Committee, the Council approved
the acquisition of Microsoft Access as the Club’s data entry
and database management technology. This product provides
a relational database engine with VisualBasic language sup-
port for applications development. The Membership Database
application will be redeveloped using Microsoft Access
during 2004.
M. MurpHy
Conservation Committee
Since November 2002 the CC has been assisting local
residents calling themselves Larose Defense Fund/Fond de
défense Larose with opposition to a proposed zoning change
within part of the forest. We expressed support for the preser-
vation of francophone heritage at other locations. The Club
contributed $1000 towards the Fund’s legal costs at an OMB
hearing.
In cooperation with the Greenspace Alliance of Canada’s
Capital, the CC appeared at City Planning and Development
Committee in regard to the 3rd draft of the Official Plan.
Some improvements were secured.
We helped the FON to hold this workshop at the Museum
of Nature in Ottawa.
Several Club members reviewed the City’s list of areas to
be studied and suggested additional areas. Adrianne Sinclair
of the CC was appointed to the Public Advisory Committee.
What in the 1970s the OFNC called the South Gloucester
Conservation Area gradually became a quarry, but the 177
City-owned acres were known to support uncommon plant
species. Despite intervention by the CC and the Greenspace
Alliance, the City voted to sell this land to the quarry owner
for $1.7M, but imposed requirements for environmental
assessment, and assigned the sale revenue to a natural land
acquisition fund.
S. ROSENBAUM
Education And Publicity Committee
The committee organized and managed OFNC participa-
tion in three major public events: the Ottawa Teachers Fed-
eration professional development day, the Carlingwood Wild-
life Festival and Health Canada’s celebration of Environment
Week. The Wildlife Festival was the largest and most success-
ful in attracting public interest. Twenty OFNC volunteers and
five Macoun members assisted with this event.
A demonstration of bird songs using tapes and slides was
provided as a pre-concert activity for the Young Peoples Con-
cert Series at the NAC, April 26.
The Ottawa Field-Naturalists’ Club presented three Natural
History Awards of $50.00 each plus an OFNC membership
at the Ottawa Regional Science Fair. The judges were Kathy
Conlan and Susan Laurie-Bourque.
A French version of the club brochure was prepared and
production begun at year’s end.
488
The sales table at the club’s evening presentations at the
Canadian Museum of Nature provided revenue of $400.
J. CAMERON
Excursions And Lectures Committee
In 2003 this Committee arranged 38 events and nine
monthly meetings including the ABM and the Soirée. Seven
general interest excursions were offered to Club members.
The Birds Committee ran 12 birding excursions, three bird
counts as well as assisted with The Taverner Cup. Two of our
monthly meetings were also devoted to birds. There were
six botanical excursions or workshops and two mushroom
activities. Insects were the subject of one excursion and two
of our monthly meetings. Other excursions were for mudpup-
pies, astronomy and a museum visit. Workshops were also
given on geology and on digital cameras. Two of our monthly
meetings were devoted to conservation matters and one intro-
duced us to polar environments.
The monthly meetings drew about 50 people on average.
Excursions and workshops are designed for a smaller number
of participants. This year we asked leaders to have partici-
pants sign a waiver form. The form is primarily designed to
inform participants about liability but it provides a record of
attendance.
F. BRODO
Executive Committee
The Executive Committee met in October to review sey-
eral items that required responses and/or action plans. As a
result of that meeting, action plans have been put in place to
address the following issues in 2004:
(1) review of electronic publication possibilities
(2) digital photo archives
(3) how to retain new members
(4) system to record names and number of persons parti-
cipating in club excursions and activities.
The Committee also reviewed the club’s liability insurance,
its role in the Taverner Cup, the issue of attracting volunteers
and it put in place a succession planning exercise and a sys-
tem to review and report on the publications of other nature
clubs. These matters require further action in 2004 but
should be completed by year end.
G. McNuLTy
Finance Committee
The Finance Committee met three times in calendar year
2003. The following items are highlighted: — a review of
existing and proposed honoraria was undertaken. No changes
to the current structure were recommended to Council.
— the committee recommended to Council that the Alfred
Bog Fund be topped up by $4,000 from the de Kiriline
Lawrence Fund, bringing the total OFNC contribution to
$59,000.
— options for replacement accounting software were assessed
but no decision was taken.
— areview of membership fees for 2004 was carried out, and
the Committee recommended to Council that the fees not
be raised for the upcoming year. However, given the ex-
pected year-end deficit, this issue will need serious con-
sideration next year.
— a budget for fiscal year 2003-04 was tabled and approved
at Council in the fall, showing a small projected deficit.
— other items such as the RoweCom bankruptcy, liability
and directors’ insurance, and Taverner Cup funding were
discussed.
L. SCHWARTZ
THE CANADIAN FIELD-NATURALIST
Vol. 118
Fletcher Wildlife Garden
Volunteers contributed over 3000 hours, mainly on Friday
or Sunday mornings. Their work is particularly noticeable
in the Backyard Garden. The Management Committee met
eleven times during the year.
The big achievement for the year was the production of
an agreement with Agricultureand Agri-Food Canada for
use of the site and occupation of the building. Negotiations
were completed in the summer and the agreement finally
signed in November. It is to run until April 2006. We wish
to thank Frank Pope for handling legal and insurance issues
and the final signing.
During the year we held a public event for International
Migratory Bird Day in May and our best plant sale ever in
June thanks to Algonquin College and our own volunteers.
Our traveling display was seen at Seedy Saturday, The
Wildlife Festival, Environment Day at Health Canada, an
Invasive Species Workshop at the Museum of Nature and at
the OFNC Soiree.
This year we had a part-time summer employee, since
we did not obtain a grant to support the position as we had
in previous years. She dealt with visitors, kept the Interpre-
tation Centre open and worked mainly on invasive plant con-
trol, supplementing the work of a group of volunteers.
The Interpretation Centre was opened by volunteers on
Sunday afternoons through the summer. Located there is a
small library, including a complete collection of the Cana-
dian Field-Naturalist, and two stereo microscopes for examin-
ing small specimens. The Centre was used for meetings by
OFNC Council and four committees and for workshops.
D. HOBDEN
Macoun Field Club Committee
The committee met just once, to plan the start-up of the
Macoun Club year; much of the work of organizing the pro-
gram from month to month was done over the telephone and
by e-mail. Some committee members arranged for speakers
each week and supervised the meetings, while others led
field trips twice a month. Some also led the high-school-age
members on camping trips at Christmas and in June.
Through this program, the children and teenagers of the
Macoun Club were introduced to local geology, lichens, plant
biology, insects, and wildlife (both Canadian and exotic). Field
trips gave members hands-on experience in identifying trees
and animal tracks, and allowed them to take part in the Club’s
ongoing research on butternut canker disease, lichen bio-
diversity, and porcupine populations.
The monthly newsletter and the annually produced Little
Bear magazine were both prepared by the young people them-
selves, while the Club’s web site was maintained jointly with
Committee members. Individual Macoun Club members pre-
sented natural science projects at the OFNC Soirée in April,
and the Club’s executive recounted the group’s activities for
the OFNC members assembled there.
R. LEE
Membership Committee
The distribution of memberships for 2003 is shown in the
table (below), with the comparable numbers for 2002 in
brackets. These statistics do not include the 23 affiliate orga-
nizations which receive free copies of the Club’s publications.
This year, the Club lost a long time member and valuable
contributor to the production of the Canadian Field-Naturalist
(CEN), with the death of Dr. Wilson Eedy, member since
1970 and Book-Review Editor of the CFN for many years.
D. SMYTHE
2004 MINUTES OF THE 125™ ANNUAL BUSINESS MEETING 489
| ° . . sae .
| Distribution of Memberships in The Ottawa Field-Naturalists’ Club
CANADIAN FOREIGN
| Type Local Other USA Other Total
_ Family 317 (340) 28 (29) | (1) | (2) 342 (372)
Individual 323 (345) Le C20) 24 (26) 6 (5) 464 (496)
Honorary 15 (15) 9 (9) 0 (0) 0 (0) 24 (24)
Life 21 (21) 20 (21) 7 (5S) | (1) 49 (48)
Sustaining 11 (8) 3 (2) 0 (O) 0) (QO) 1] (10)
Total 687 (729) 166 (181) 32. (32) 8 (8) 890 (950)
Publications Committee
The Publications Committee met twice in 2003.
_ Four issues of The Canadian Field-Naturalist were pub-
— lished in 2003: Volume 116, #2,3,4 and Volume 117, #1.
These four issues contained 698 pages; 47 articles; 20 notes;
_ 1 COSEWIC article; 81 book reviews; 144 new titles; 2
_ commemorative tributes; 24 pages of News and Comments;
and a 29 page index.
The long-time Book Review Editor, Wilson Eedy, died sud-
denly in the summer. His position has been taken over by
Roy John. All of the Associate Editors will be reappointed
for 2004.
Six articles qualified for support from the Manning Mem-
_ orial Fund for a total of $4044.
Steady progress was made in getting the publication sched-
ule back on track. The printing of The CFN has been taken
from St. Joseph and contracted to Gilmore Printing Services
Inc. beginning with Volume 117, #2. It is expected that this
will both reduce the printing costs and improve the photo-
graphic quality.
In response to an author’s complaint, the details of pub-
lication charges have been reworded. The new text says, in
effect, that only members of The Ottawa Field-Naturalists’
Club and subscribers to The CFN are eligible to apply for
waiver of page charges for the first five pages, and then only
if institutional funds are unavailable.
Volume 37 of Trail & Landscape was published in four
issues containing 192 pages with the usual mix of good articles
and news of Club events.
R. BEDFORD
490
Auditor’s Report
THE CANADIAN FIELD-NATURALIST
To The Members of THE OTTAWA FIELD NATURALISTS’ CLUB
I have audited the balance sheet of THE OTTAWA
FIELD-NATURALISTS’ Club as at September 30,
2003, the statement of changes in net assets, and the
statements of operations. These financial statements are
the responsibility of the organization’s management.
My responsibility is to express an opinion on these
statements based on my audit.
Except as explained in the following paragraph, I
conducted my audit in accordance with generally ac-
cepted auditing standards. Those standards require that
I plan and perform an audit to obtain reasonable as-
surance whether the financial statements are free of
material misstatement. An audit includes examining
evidence supporting the amounts and disclosures in
the financial statements. An audit also includes assess-
ing the accounting principles used and significant esti-
mates made by management, as well as evaluating the
overall financial statement presentation.
In common with many non-profit organizations,
the Ottawa Field-Naturalists’ Club derives some of its
revenue from memberships, donations, and fund raising
activities. These revenues are not readily susceptible to
complete audit verification, and accordingly, my veri-
fication was limited to accounting for the amounts
reflected in the records of the organization.
In my opinion, except for the effect of the adjust-
ments, if any, which I might have determined to be
necessary had I been able to satisfy myself concern-
ing the completeness of the revenues referred to in
the preceding paragraph, these financial statements
present fairly, in all material respects, the financial
position of the OFNC as at September 30, 2003, and
the results of its operations and changes in net assets
for the year then ended in accordance with generally
accepted accounting principles.
JANET M. GEHR
Chartered Accountant
North Gower, Ontario
January 12, 2004
Vol. 118
The Ottawa Field-Naturalists’ Club
Balance Sheet
September 30, 2003
2003 2002
ASSETS
CURRENT
Cash (Note 1) $ 2,781 $ 71,087
Investment certificates (Note 1) 43,764 84,790
Marketable securities (Note 2) 246,467 235,758
Accounts receivable 27,690 7,238
Prepaid expenses 1,000 1,000
321,702 399,873
CAPITAL ASSETS (Note 3) - _
Land — Alfred Bog 3,348 3,348
$ 325,050 $403,221
LIABILITIES AND FUND BALANCES
CURRENT
Accounts payable and
accrued liabilities $ 2,000 $ 2,000
Deferred revenue 12,075 13,500
14,075 15,500
Life memberships 12,663 2A
NET ASSETS
Unrestricted 60,609 80,325
Club reserve 100,000 100,000
Manning principal 100,000 100,000
Manning interest - OFNC 1,434 1,963
- CFN 13,153 13,179
Seedathon 1,618 2,087
Anne Hanes memorial 870 870
de Kiriline-Lawrence 18,798 23,975
Macoun Baillie Birdathon 3 5857/ S27
Alfred Bog 493 52,274
298,312 376,000
$ 325,050 $403,221
2004 MINUTES OF THE 125" ANNUAL BUSINESS MEETING 49]
The Ottawa Field-Naturalists’ Club The Ottawa Field-Naturalists’ Club
Statement of Operations Canadian Field-Naturalists — Statement Of Operations
For the Year Ended September 30, 2003 For the Year Ended September 30, 2003
2003 2002 2003 2002
REVENUE REVENUE
Memberships $ 14,615 $ 15,488 Memberships $ 9,743 $ 10,325
Trail and Landscape 193 196 Subscriptions 25,369 28,483
Interest 1,339 1,457 Reprints 9,534 5,608
GST rebate 780 4,532 Publication charges 50,559 16,812
Other 617 760 Interest and exchange 7,940 10,404
17,547 22,433 GST rebate 3,040 3,448
SS a Other 734 339
OPERATING EXPENSES 106,919 75,419
Affiliation fees 680 680
Computer 302 216 EXPENSES
Membership Syl 1,437 Publishing $ 80,758 $ 61,570
Office Assistant 1,000 1,000 Reprints 7,307 4,127
Telephone 1,622 1,848 Circulation 11,307 7,653
Insurance 655 655 Editing 4,183 2,652
Audit 1,000 1,000 Office Assistant 5,000 5,000
GST 1,290 136 Honoraria 9,000 9,000
Other 884 2,847 GST rebate 6,508 5,146
Tal RE: Suet 124,615 95,569
CLusB ACTIVITY EXPENSES ExcEss EXPENSES OVER
Awards is 471 REVENUE $ (17,696) $ (20,150)
Birds 1,696 223 ae Saupe
Education and Publicity 73 1322
Excursions and lectures 496 164
Macoun Field Club 851 1,027
Soiree 19 466
Trail and Landscape 8,368 9,088
Fletcher Wildlife Garden (Note 4) 2,623 1,294
Other = _
14,126 14,055
22,710 25,054
Excess EXPENSES OVER
REVENUE $ (5,163) $ (2,621)
492 THE CANADIAN FIELD-NATURALIST
The Ottawa Field-Naturalists’ Club Notes to the Financial Statements
September 30, 2003
1. CASH
Chequing
Savings
Nesbitt Burns
Fletcher Wildlife Garden
Investment Certificates: Maturity Maturity
Value Date
$ 44,385 04/29/04
2. MARKETABLE SECURITIES
Investment Certificates: Maturity Maturity
Value Date
Province of Newfoundland Coupon $ 44,782 10/17/11
Province of Manitoba Coupon 29,847 11/15/04
Ontario Savings Bonds 40,000 06/21/05
CMHC Global Debs 52,000 12/01/06
Province of Ontario Bond 30,000 09/12/07
Province of Newfoundland Bond 20,000 10/07/08
Government of Canada Coupon 30,167 12/01/09
Province of New Brunswick Bond 20,000 06/15/10
3. CAPITAL ASSETS
Equipment at a cost of $16,748 is fully amortized.
4. FLETCHER WILDLIFE GARDEN
REVENUE
Federal government
City of Ottawa
Taverner Cup
Sales
GST
Donations
Other
EXPENSES
Program
Backyard
Habitats
Interpretation centre
Administration
Publications
GST
Library
Other
2003
$ (3,777)
1,344
919
4,295
$ 2,781
Yield
1.00%
Yield
4.525%
5.119%
6.45%
5.250%
6.125%
6.263%
5.605%
6.231%
243
132
6,346
$ (2,623)
Vol. 118 !
2002
$ 5,589
58,336
919
5,868
$ 70,712
Book
Value
$ 43,764
Book
Value
$ 31,421
26,754
41,370
53,539
31,187
20,538
20,590
21,068
$246,467
2002
$ 3,059
1,450
1,354
872
398
292
7,425
3,174
123
1,864
783
1,048
337
303
87
8,719
$ (1,294)
2004 MINUTES OF THE 125™ ANNUAL BUSINESS MEETING 493
The Ottawa Field-Naturalists’ Club Statement of Changes in Net Assets
For the Year Ended September 30, 2003 (Note 5)
Net Beginning Excess Excess Other Ending
Assets Balance Expenses CFN Expenses OFNC Revenue Expenses Balance
Unrestricted $ 80,325 $ (17,696) $ (5,163) $ 3,143 a $ 60,609
Club Reserve 100,000 - - - ~ 100,000
Manning Principal 100,000 = - - - 100,000
Manning — OFNC (a) 1,963 ~ - 1,021 1,550 1,434
Manning — CEN (b) 13,179 ~ ~ 4,086 4,112 13,153
Seedathon 2,087 - - 502 971 1,618
Anne Hanes Memorial 870 - - = ~ 870
de Kiriline-Lawrence (c) 23,975 _ - 381 5,558 18,798
Macoun Baillie Birdathon (d) 1.327 — - 10 - 1,337
Alfred Bog (e) 52,274 - - 3,219 55,000 493
$ 376,000 $ (17,696) $ (5,163) $ 12,362 $ 67,191 $ 298,312
STATEMENT OF CHANGES IN NET ASSETS
a) Manning OFNC Expenses: Taverner Competition, $1,250; Peregrine Watch, $300;
b) Manning CFN Expenses: Vol. 114, No. 2, Douglas Clark, Grizzly Bears in Northern Manitoba $228; Vol. 116, No. 1,
Mark Hipfner et al., Common Eiders around Digges Sound $340; Gerald Kuzyk et al., Wolf response to sled dog
$160; Kevin White et al., Predation of wolves on wolverines and martens $160; W. A. Fuller, Canada and the buffalo
$1,609; Vol. 116, No. 3, John Goold et al., Sperm whale strandings $1,615.
c) de Kiriline Lawrence Expenses: Nature Conservancy of Canada — land in Alfred Bog $4,000; Sierra Club, Ottawa
Group — Leitrim Wetlands publicity — $1,000; Greenspace Alliance (Unger) — newspaper ad in defence of South
Gloucester Conservation Area $558.
d) Alfred Bog Expense: Nature Conservancy of Canada, $55,000 proceeds from fund raising campaign for acquisition
of land in Alfred Bog.
The Ottawa Field-Naturalists’ Club Summary of Significant Accounting Policies
September 30, 2003
1. Nature of Business
The organization is non-profit and incorporated under the
laws of Ontario (1884). The organization promotes the appre-
ciation, preservation, and conservation of Canada’s natural
heritage. It encourages investigation and publishes the results
of the research in all fields of natural history and diffuses
information on these fields as widely as possible. It also sup-
ports and cooperates with other organizations engaging in
preserving, maintaining or restoring environments of high
quality for living things.
2. Financial Instruments
The organization’s financial instruments consist of cash,
accounts receivable, marketable securities, and accounts pay-
able. Unless otherwise noted, it is the management’s opinion
that the organization is not exposed to significant interest,
currency, or credit risks arising from these financial instru-
ments. The fair value of these instruments approximate their
carrying values.
3. Capital Assets
Capital assets acquired after 1989 are expenses. Capital
assets acquired prior to 1990 were recorded as assets at cost
and amortized on a straight-line basis. These assets have
been fully amortized.
4. Statement of Changes in Financial Position
A statement of changes in financial position has not been
provided as it would not provide additional meaningful infor-
mation.
5. Foreign Currency
Transactions during the year in U.S. dollars have been
converted in the accounts to Canadian dollars at the exchange
rate effective at the date of the transaction. All monetary assets
in U.S. dollars at year end have been converted to Canadian
dollars at the rate effective on Sept. 30, 2003. Gains or losses
resulting therefrom are included in revenue or expenses.
Advice for Contributors to The Canadian Field-Naturalist
Content
The Canadian Field-Naturalist is a medium for the publi-
cation of scientific papers by amateur and professional natu-
ralists or field-biologists reporting observations and results
of investigations in any field of natural history provided that
they are original, significant, and relevant to Canada. All read-
ers and other potential contributors are invited to submit for
consideration their manuscripts meeting these criteria. The
journal also publishes natural history news and comment items
if judged by the Editor to be of interest to readers and sub-
scribers, and book reviews. Please correspond with the Book
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494
——SaEaS==—_—_=>—=—>=
TABLE OF CONTENTS (concluded) Volume 118 Number 3
}
ik
Sequential polyandry in Piping Plover, Charadrius melodus, nesting in eastern Canada
DIANE L. AMIRAULT, JONATHAN KIERSTEAD, PETER MACDONALD, and LARRY MACDONNELL
| American Dipper, Cinclus mexicanus, preys upon larval Tailed Frogs, Ascaphus truei
CurisTy A. Morrissey and ROBERTA OLENICK
Piping Plover, Charadrius melodus, egg viability after seawater immersion
JULIE MCKNIGHT, LINDA THOMAS, and DIANE L. AMIRAULT
Tribute
1A tribute to Loris Shano Russell, 1904-1998 KEVIN L. SEYMOUR
|Book Reviews
|ZooLocy: The Uses and Curation of Bird’s Egg Collections: An Examination and Bibliography — Birds of
| Nunavut: A Checklist — Birds of the Untamed West: The History of Birdlife in Nebraska, 1750 to 1875 —
Birds of Nebraska: Their Distribution and Temporal Occurrence — Canadian Skin and Scales: A Complete
Encyclopedia of Canadian Amphibians and Reptiles — Conservation and Ecology of Turtles of the Mid-
Atlantic Region: A Symposium — For Love of Insects — The Freshwater Fishes of Manitoba — The
History of Ornithology in Virginia — All-Weather Hawk Watcher’s Field Journal —- Self-Portrait with
Turtles: A Memoir — Wild Mammals of North America: Biology, Management, and Conservation
(Second edition) — Pete Dunne on Bird Watching: The How-to, Where-to and When-to of Birding
-|Borany: Alpine Plants of North America: An Encyclopaedia of Mountain Flowers from Rockies to Alaska
— Arboretum America, a Philosophy of the Forest — Cape Cod Wiidflowers: A Vanishing Heritage —
Lewis Clark’s Field Guide to Wild Flowers of the Sea Coast in the Pacific Northwest — Wild Flowers of
Field & Slope in the Pacific Northwest — Wild Flowers of Forest & Woodland in the Pacific Northwest
Wild Flowers of the Mountains of the Pacific Northwest
ENVIRONMENT: Conserving Living Natural Resources in the Context of a Changing World — Visions of the
Land: Science Literature, and the American Environment from the Era of Exploration to the Age of
Ecology — Genetic, Demography and Viability of Fragmented Populations — A Primer of Ecological
Genetics
MISCELLANEOUS: Smithsonian Institution Secretary Charles Doolittle Walcott
NEw TITLES
|News and Comment
Froglog: Newsletter of the Declining Amphibian Populations Task Force (63, 64) — Marine Turtle
Newsletter (105) — The Boreal Dip Net/L’Epuisette Boreal: Newsletter of the Canadian Amphibian and
Reptile Conservation Network - Reseau Canadien de Conservation des Amphbiens et des Reptiles 8(2)
June 2004 — Canadian Species at Risk May 2004
_|Errata: Canadian Field-Naturalist 118(2)
Omission from the back cover contents: Rail and Chapdelaine
Replacement figure for Wilson et al. page 161
Minutes of the 125 Annual Business Meeting of The Ottawa Field-Naturalists’ Club
Tuesday 13 January 2004
| Advise to Contributors to The Canadian Field-Naturalist
Mailing date of the previous issue 118(2): 10 May 2005
2004
444
446
448
45]
465
474
477
481
483
484
485
486
494
THE CANADIAN FIELD-NATURALIST Volume 118 Number 3
Articles
Population dynamics of Deer Mice, Peromyscus maniculatus, and Yellow-pine
Chipmunks, Zamias amoenus, in old field and orchard habitats
THOMAS P. SULLIVAN, DRUSCILLA S. SULLIVAN, and EUGENE J. HOGUE
Density and survival of lady beetles (Coccinellidae) in overwintering sites in Manitoba
W. J. TURNOCK and I. L. WISE
Description of age-O Round Goby, Neogobius melanostomus Pallus (Gobiidae) and ecotone
utilization in St. Clair lowland waters, Ontario JOHN K. LESLIE and CHARLES A. TIMMINS
A systematic analysis of the alpine saxifrage complex (Saxifragaceae) in the Canadian Arctic Islands
using morphology and chloroplast DNA data CAROLINE HEALY and LYNN J. GILLESPIE
The influence of prey availability and vegetation characteristics on scent station visitation rates
of Coyotes in a heterogeneous environment LYNDA A. RANDA and JOHN A. YUNGER
Presence of cavities in snags retained in forest cutblocks: Do management policies promote
species retention? Kim T. EVERETT and KEN A. OTTER
Summer diet of two White-tailed Deer, Odocoileus virginianus, populations living at low and
high density in southern Quebec CLAUDE DAIGLE, MICHAEL CRETE, LOUIS LESAGE,
JEAN-PIERRE OQUELLET, and JEAN HUOT
Winter habitat use by Wolves, Canis lupus, in relation to forest harvesting in west-central Alberta
GERALD W. KUZYK, JEFF KNETEMAN, and FIONA K. A. SCHMIEGELOW
Bird communities of the Garry Oak habitat in southwestern British Columbia
WAYNE R. ERICKSON
Invertebrate diversity under artificial cover in relation to boreal forest habitat characteristics
STEPHEN H. FERGUSON and DANIELLE K. A. BERUBE
Observations of habitat use by Polar Bears, Ursus maritimus, in the Alaskan Beaufort, Chukchi,
and northern Bering Seas DONALD J. HANSEN
New records for the Arctic Shrew, Sorex arcticus, and the newly recognized Maritime Shrew,
Sorex martimensis NEIL D. PERRY, DONALD T. STEWART, ELIZABETH M. MADDEN,
and THOMAS J. MAIER
Lichen zonation on coastal rocks on Gwaii Haanas National Park Reserve, Haida Gwaii
(Queen Charlotte Islands), British Columbia IRWIN M. BRobo and Norm A. SLOAN
Predaceous water beetles (Coleoptera: Adephaga: Dysticidae, Gyrinidae) collected along the
Horton and Thelon rivers in the Arctic Central Barrens of Canada
HELENA V. SHAVERDO and DONNA J. GIBERSON
Notes
Collapsing burrow causes death of a Eurasian Beaver, Castor fiber
Liat R. THOMSEN, FIONA SHARPE, and FRANK ROSELL
Frequency of tail breakage of the Northern Water Snake, Nerodia sipedon sipedon | KENNETH D. BOWEN
The Heather Vole, genus Phenacomys, in Alaska
S. O. MACDONALD, AMY M. RUNCK, and JOSEPH A. COOK
Extension de Vaire de distribution connue de la Musaraigne fuligineuse, Sorex fumeus, dans le nord-est
du Quebec JEAN-FRANCOIS DESROCHES and ISABELLE PICARD
Gulls, Larus spp., foraging at Pink Salmon, Oncorhynchus gobuscha, spawning runs — MAry F. WILLSON
(continued on inside back cover)
ISSN 0008-3550
2004
368
376
The CANADIAN
FIELD-NATURALIST
Published by THE OTTAWA FIELD-NATURALISTS’ CLUB, Ottawa, Canada
re Ave
Volume 118, Number 4 October—December 2004
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MCZ
LIBRARY
APR 0 3 2006
ARVARD
October-December 2004
The Canadian Field-Naturalist
Volume 118, Number 4
Stranding of a Pygmy Sperm Whale, Kogia breviceps, in the Northern
Gulf of St. Lawrence, Canada
LENA Measures!”, BENOIT ROBERGE?, and RICHARD SEARS®
' Fisheries and Oceans, Maurice Lamontagne Institute, 850 Route de la Mer, Mont-Joli, Québec GSH 324 Canada. (Author
to whom correspondence should be addressed.)
2 Parks Canada Agency, Mingan Archipelago National Park Reserve of Canada, 1303 de la Digue, Havre-Saint-Pierre,
Québec GOG 1P0 Canada
3 Mingan Island Cetacean Study, Inc., 625, rue du Centre, Longue-Pointe-de-Mingan, Québec GOV 1V0 Canada
Measures, Lena, Benoit Roberge, and Richard Sears. 2004. Stranding of a Pygmy Sperm Whale, Kogia breviceps, in the
Northern Gulf of St. Lawrence, Canada. Canadian Field-Naturalist 118(4): 495-498.
A Pygmy Sperm Whale, Kogia breviceps, stranded alive and later died in the Northern Gulf of St. Lawrence, Quebec, Canada
on 28 August 2001. This is the northern-most stranding of this species in the western Atlantic. The whale was estimated to be
approximately 3 m long and a longitudinal section from one tooth (31 mm long and 5.0 mm in diameter) revealed 3.5 growth
layer groups. ~
Key Words: Pygmy Sperm Whale, Kogia breviceps, Gulf of St. Lawrence, Quebec, Canada.
A Pygmy Sperm Whale (Kogia breviceps) was
found dead 28 August 2001 on the north shore of the
Gulf of St. Lawrence. It was observed alive on 27
August by a local resident, Mme Rose-Annette Blais,
northwest of St. Charles Island in the Mingan Archi-
pelago National Park Reserve. The whale was observed
making slow, undulating movements in shallow water
close to shore in Trilobites Bay (50°14'07"N; 63°21'
18"W) and was found dead the next morning on a
sandy beach in the bay. Personnel from Parks Canada
were alerted and arrived on site to examine the carcass.
The whale was estimated to be approximately 3 m long
(Figure 1). There were various wounds and lacerations
on the rostrum, flanks and abdomen (Figure 2). Two
teeth (one broken near the root) collected by Jacques
A. Thériault and his father, were later submitted for
analysis. Fisheries and Oceans Canada and the Min-
gan Island Cetacean Study, Inc. were informed of the
stranding but before the carcass could be collected
for necropsy it had been carried off by a rising tide
and was not seen again. Both teeth were deposited in
the Maurice Lamontagne Institute collection, Acces-
sion Number 11629.
The whale was identified as a Pygmy Sperm Whale
based on photographs, approximate length (3 m), the
low, falcate dorsal fin located posterior to the center
of the dorsum (Figures 1, 2) and size of one intact
tooth. The tooth was 31 mm long and 5.0 mm in diam-
eter at its widest point. In the dentine and cementum
layers there were 3.5 growth layer groups (GLG)
observed in a longitudinal section of the tooth. It is
unknown how many GLGs are laid down per year in
Pygmy Sperm Whales. If similar to the Sperm Whale
Physeter macrocephalus [1 GLG = 1 year of age (C.
Lockyer, personal communication; Perrin and Myrick
1980)], then this animal is almost 4 years old and
likely an adult (Handley 1966). Ross (1984) reported
3.5 GLGs in a sexually mature female that stranded
with a calf.
The Pygmy Sperm Whale can be confused with
the Dwarf Sperm Whale (Kogia simus). The latter is
smaller (2.7 m maximum length) with a taller dolphin-
like dorsal fin and teeth are less than 30 mm long and
less than 4.5 mm in diameter (Handley 1966; Leather-
wood and Reeves 1983).
Pygmy Sperm Whales are rarely observed in eastern
Canadian waters and have no COSEWIC (Committee
on the Status of Endangered Wildlife in Canada) status
(Baird et al. 1996). Seven, probably eight, Pygmy
Sperm Whale strandings have been reported prior to
the present report (Piers 1923; Sergeant et al. 1970:
Nelson et al. 1991; McAlpine et al. 1997; Lucas and
Hooker 2000) in Canada over the last century, specif-
ically in Halifax and on Sable Island in Nova Scotia,
in Blacks Harbour and Saint-John’s, New Brunswick
and on the French island of Miquelon near the south-
495
496 THE CANADIAN FIELD-NATURALIST Vol. 118
pau
FiGure |. Pygmy Sperm Whale beach-cast in Trilobites Bay on 27 August 2001. Length is approximately 3 m.
west coast of Newfoundland. The present report is the
northern-most stranding of this species in the western
Atlantic and the first within the Gulf of St. Lawrence.
The Pygmy Sperm Whale is a small pelagic, mainly
deep-water odontocete (occasionally seen motionless
in surface waters) found widely offshore on continen-
tal slopes throughout tropical and warm temperate
waters in the world. Most information on this species
has been obtained from beach-cast carcasses and re-
cently from live-stranded and rehabilitated animals in-
cluding mother-calf pairs or pregnant females (Hiick-
stadt and Antezana 2001; Scott et al. 2001; Manire et
al. 2002). Stomach analyses indicate that the Pygmy
Sperm Whale feeds primarily on cephalopods, crus-
taceans (shrimp, crab) and fish (Reeves et al. 2002).
In the western Atlantic most strandings have been
reported off the southeastern coast of the United States
(Caldwell and Caldwell 1989; Odell 1991) and live
individuals have been observed beyond the continental
shelf and in the Gulf Stream.
Recently, a rehabilitated Pygmy Sperm Whale
equipped with a time-depth recorder was released in
the Gulf Stream off the eastern coast of the United
States. It was observed for 5 days and remained east
of the continental shelf break (200 m isobath) but west
of the eastern edge of the Gulf Stream where sea-
surface temperatures were 27.8 — 30.0°C (Scott et al.
2001). Unfortunately, dive depth information was not
obtained and it is unclear whether the behaviour of
this individual reflects that of the species in general.
Odell et al. (1985 as cited in Caldwell and Caldwell
1989) noted that more strandings of Kogia (K. brevi-
ceps and K. simus) occur in Florida when the Gulf
Stream shifts farther offshore. They suggested that indi-
viduals following prey caught in Gulf Stream eddies
or rings that suddenly dissipate may become disori-
ented and, subsequently, strand. Gulf Stream rings
can occur to the north or south of the Gulf Stream but
anticyclonic or warm-core rings which are about
1000 m deep and exist on average 4.5 months, drift
southwestward to rejoin the Gulf Stream near Cape
Hatteras (Richardson 1976; Wiebe 1976). Gulf stream
rings have unique physical, chemical and biological
characteristics (Wiebe 1976; Joyce and Wiebe 1983;
Craddock et al.1992). Although warm-core rings do
not ride onto shallow continental shelves, they can
push slope water onto the shelf or entrain shelf water
into slope waters. Such shelf water entrainment was
suggested as providing suitable cephalopod habitat
which attracted Sperm Whales in the vicinity of a
warm-core ring off Georges Bank (Griffin 1999).
The occurrence of a Pygmy Sperm Whale in the
Gulf of St. Lawrence, especially in the northern Gulf,
seems unusual as water temperatures are relatively cold
[sea-surface temperatures are generally 12 — 18°C in
August (Vigeant 1987*)]. The minimum temperature
2004
MEASURES, ROBERGE, AND SEARS: STRANDING OF PYGMY SPERM WHALE
497
FiGuRE 2. Pygmy Sperm Whale in shallow water in Trilobites Bay (same specimen as in Figure 1). Note relative position of
dorsal fin on trunk.
tolerated by Pygmy Sperm Whales is unknown. Annu-
al mean air temperatures in most of the northwest At-
lantic, especially in the southern Gulf of St. Lawrence,
and sea-surface water temperatures throughout eastern
Canadian waters in 2001 were generally warmer than
normal (Drinkwater et al. 2002a*). In some areas, the
upper 30 m in the central and southern Gulf of St.
Lawrence show monthly anomalies of 3 - 4°C (Drink-
water et al. 2002b*; Gilbert 2002*). The Pygmy Sperm
Whale may have swam and drifted northeast follow-
ing prey in the Gulf Stream as suggested by Fraser
(1974), perhaps using warm-core rings as “stepping-
stones” (Peter Wiebe, personal communication) or
thermal fronts associated with warm-core rings as
observed by Griffin (1999). It may have entered the
Gulf of St. Lawrence in warm surface waters on the
Cape Breton side of the Cabot Strait when the Cape
Breton Current slows in summer (El-Sabh 1977). Dur-
ing a DFO research cruise in the Gulf of St. Law-
rence in August 2001 squid (/lex illecebrosus) were
collected but numbers of specimens collected were
not considered exceptional (D. Archambault, DFO,
unpublished data).
Acknowledgments
We thank R-A. Blais and J. A. Thériault for assis-
tance in this stranding and providing teeth. We also
thank S. Plamondon of Parks Canada who provided
photographs and J.-G. Gosselin of Fisheries and Oceans
Canada who determined the number of GLGs by cut-
ting the tooth. We appreciate that P. Best and J. Mead
examined the photographs and concurred with our
identification of the species.
Documents Cited (marked * in text)
Drinkwater, K. F., R. G. Pettipas, and W. M. Petri. 2002a.
An overview of meteorological, sea ice and sea-surface
temperature conditions off Eastern Canada during 2001.
Canadian Science Advisory Secretariat Research Docu-
ment 2002/048.
Drinkwater, K. F., R. G. Pettipas, and W. M. Petri. 2002b.
Physical environmental conditions in the Southern Gulf
of St. Lawrence during 2001. Canadian Science Advisory
Secretariat Research Document 2002/047.
Gilbert, D. 2002. Oceanographic conditions in the Gulf of
St. Lawrence in 2001 : physical oceanography. DFO Sci-
ence Stock Status Report.
498
Vigeant, G. 1987. Température mensuelle de ]’eau en surface
dans l’estuaire et le Golfe du Saint-Laurent. Service de
1’ Environnement Canada.
Literature Cited
Baird, R. W., D. Nelson, J. Lien, and D. W. Nagorsen.
1996. The status of the pygmy sperm whale, Kogia brevi-
ceps, in Canada. Canadian Field-Naturalist 110: 525-532.
Caldwell, D. K., and M. C. Caldwell. 1989. Pygmy sperm
whale Kogia breviceps (de Blainville, 1838): dwarf sperm
whale Kogia simus Owen, 1866. pages 235 — 260 in Hand-
book of marine mammals. Edited by S. H. Ridgway and
R. Harrison. Academic Press, London.
Craddock, J. E., R. H. Backus, and M. A. Daher. 1992.
Vertical distribution and species composition of midwater
fishes in warm-core Gulf Stream meander/ring 82-H. Deep
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El-Sabh, M. I. 1977. Oceanographic features, currents, and
transport in Cabot Strait. Journal of the Fisheries Research
Board of Canada 34: 516-528.
Fraser, F. C. 1974. Report on Cetacea stranded on the British
coasts from 1948 to 1966. British Museum (Natural History)
14.
Griffin, R. B. 1999. Sperm whale distributions and commu-
nity ecology associated with a warm-core ring off Georges
Bank. Marine Mammal Science 15: 33-51.
Handley, C. O., Jr. 1966. A synopsis of the genus Kogia
(pygmy sperm whales), pages 62 — 69 in Whales, dol-
phins and porpoises. Edited by K. S. Norris. University of
California Press, Berkeley and Los Angeles, Calif.
Hiickstaédt, L., and T. Antezana. 2001. An observation of
parturition in a stranded Kogia breviceps. Marine Mammal
Science 17: 362-365.
Joyce, T., and P. Wiebe. 1983. Warm-core rings of the Gulf
Stream. Oceanus 26: 34-44.
Leatherwood, S., and R. R. Reeves. 1983. The Sierra Club
handbook of whales and dolphins. Sierra Club Books, San
Francisco.
Lucas, Z. N., and S. H. Hooker. 2000. Cetacean strandings
on Sable Island, Nova Scotia, 1970 — 1998. Canadian Field-
Naturalist 114: 45-61.
Manire, C. A., L. Byrd, H. L. Rhinehart, P. Cunningham-
Smith, and D. R. Smith. 2002. Subacute atropine toxicity
in a pygmy sperm whale, Kogia breviceps. Journal of Zoo
and Wildlife Management 33: 66-72.
THE CANADIAN FIELD-NATURALIST
Vol. 118
McAlpine, D. F., L. D. Murison, and E. P. Hoberg. 1997.
New records for the pygmy sperm whale, Kogia breviceps
(Physeteridae) from Atlantic Canada with notes on diet
and parasites. Marine Mammal Science 13: 701—704.
Nelson, D., A. Desbrosse, J. Lien, P. Ostromm, and R.
Seton. 1991. A new stranding record of the pygmy sperm
whale, Kogia breviceps, in waters off Eastern Canada.
Canadian Field-Naturalist 105: 407-408.
Odell, D. K. 1991. A review of the Southeastern United States
Marine Mammal Stranding Network: 1978 — 1987. pages
19 — 23 in Marine Mammal Strandings in the United States.
Edited by J. E. Reynolds II and D. K. Odell. NOAA
Technical Report NMFS 98.
Perrin, W. F., and A. C. Myrick, Jr. Editors. 1980. Growth
of odontocetes and sirenians: problems in age determina-
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Special Issue 3: 1-229.
Piers, H. 1923. Accidental occurrence of the pygmy sperm
whale (Kogia breviceps) on the coast of Nova Scotia; an
extension of its known range, with remarks on the proba-
bility of the former presence in these waters of the true
sperm whale (Physeter macrocephalus). Proceedings and
Transactions of the Nova Scotia Institute of Science 15:
95-114.
Reeves, R. R., B. S. Stewart, P. J. Clapham, and J. A.
Powell. 2002. National Audubon Society guide to marine
mammals of the world. Alfred A. Knopf, New York.
Richardson, P. 1976. Gulf Stream rings. Oceanus 19: 65-68.
Ross, G. J. B. 1994. The smaller cetaceans of the south east
coast of southern Africa. Annals of the Cape Provincial
Museums (Natural History) 15: 173-410.
Scott, M. D., A. A. Hohn, A. J. Westgate, J. R. Nicolas, B.
R. Whitaker, and W. B. Campbell. 2001. A note on the
release and tracking of a rehabilitated pygmy sperm whale
(Kogia breviceps). Journal of Cetacean Research Man-
agement 3: 87- 4.
Sergeant, D. E., A. W. Mansfield, and B. Beck. 1970.
Inshore records of cetacea for eastern Canada, 1949 — 68.
Journal of the Fisheries Research Board of Canada 27:
1903-1915.
Wiebe, P. 1976. The biology of cold-core rings. Oceanus
19: 69-76.
Received 14 July 2003
Accepted 15 July 2004
Seed Dispersal by Brown Bears, Ursus arctos, in Southeastern Alaska
Mary FE. WILLSON! and Scott M. GENDE?
'5230 Terrace Place, Juneau, Alaska 99801 USA.
National Park Service, Glacier Bay Field Station, 3100 National Park Road, Juneau, Alaska 99801 USA
Willson, Mary F., and Scott M. Gende. 2004. Seed dispersal by Brown Bears, Ursus arctos, in southeastern Alaska. Canadian
Field-Naturalist 118(4): 499-503.
Mammals often consume fleshy fruits and disperse significant quantities of the enclosed seeds. In southeastern Alaska,
Brown Bears (Ursus arctos) are among the most important dispersers of seeds for the numerous plant species producing
fleshy fruits, because these bears are abundant, often eat large quantities of fruit, and commonly excrete seeds in germinable
condition. Scat analyses showed that Brown Bears on Chichagof Island ate increasing quantities of fruit through summer
and fall. Scats commonly contained several thousand seeds, often of two or more species. Four kinds of seeds of fleshy-
fruited plants that normally grow in forest understory germinated at similar levels when experimentally deposited (in bear
scats) in the two most common habitats (forest and muskeg), suggesting that habitat distribution of these plants is not deter-
mined simply by germination patterns. Although seed passage through bear digestive tracts and the composition of scats are
known to affect germination rates to some degree, the most important role of bears in seed dispersal is probably transport.
Key Words: Brown Bears, Ursus arctos, Southeastern Alaska, seed dispersal, fleshy fruits, Rubus, Ribes, Oplopanax, Vaccinium,
Streptopus.
Coastal rainforest ecosystems in southeastern Alaska
include many shrubs and herbs with fleshy fruits,
commonly consumed by vertebrates that disperse the
enclosed seeds (Willson 1991; Traveset et al. 2004).
Potential dispersal agents include corvids, thrushes,
warblers, waxwings, Pine Marten (Hickey et al. 1999)
and bears (Willson 1993, 1994). Bears are important
dispersers of seeds, because they can consume large
quantities of fruit (Welch et al. 1997; Farley and Rob-
bins 1995) and often range over considerable dis-
tances (Patten 1993), distributing seeds far from the
source. Furthermore, bears are numerous in south-
eastern Alaska, with density reaching several hundred
bears per 1000 km — perhaps as many as 700 or even
more in some areas (Miller et al. 1997; J. Whitman,
personal communication). The abundance of Brown
Bears (Ursus arctos) in southeastern Alaska provides
an opportunity to examine the consequences of bear
frugivory for seed dispersal.
The purpose of this paper is to describe the phenol-
ogy of Brown Bear frugivory, patterns of scat deposition
on a small spatial scale, seed abundance and composi-
tion in bear scats, and field tests of seed germination
from bear scats. We then integrate this information
with previous reports, in order to describe what is
known about this ecologically important interaction
in southeastern Alaska.
Study Area and Methods
Field work was conducted on northern Chichagof
Island in the Alexander Archipelago, at the southern end
of Port Frederick (approximately 58°N, 135°30'W).
The only bears on this island are Brown Bears. The
rainforest is composed chiefly of Sitka Spruce (Picea
sitchensis) and hemlock (Tsuga spp.), with occasional
muskegs (bogs) of Sphagnum moss, scattered Lodge-
pole Pines (Pinus contorta), and low shrubs. Brown
Bear scats were collected from abandoned logging
roads, at less than 300 m elevation, in the Neka River
valley and near Salt Lake Bay on opposite sides of
Port Frederick. During each road survey, all scats were
cleared from the road, so that the subsequent survey
recorded only scats deposited in the between-survey
interval. The roads passed through forests of differing
ages, clearcuts, and muskegs.
Seed composition of scats
The frequency of occurrence of seeds, and the prin-
cipal kinds of seeds present, were recorded in June-
September 1990-1993 in 4378 scats. A subset of 570
seed-containing scats was collected in August and
September 1990 and 1991, for quantitative estimates
of seed abundance. Each of these scats was mixed to
distribute the seeds throughout, and a subsample aver-
aging 24% + 2% (S. E.) of the total scat mass was
taken. In the weighed subsample, the seeds were iden-
tified to genus and counted; the number of seeds in
the entire scat was then estimated by extrapolation.
The frequency of seeds in scats through the summer
and early fall was examined, using | June as Day 1.
June scat collections represent the previous spring
months; collections in July, August, and September
represent only the preceding 30 days, approximately.
Seed germination
In order to compare seed germination in two prin-
cipal habitats, over 150 of the scats for which total
seed content was estimated were placed in two common
habitats (muskeg or forest). Scats were “planted” in
499
500
transects in each habitat, in whatever microhabitats
were available at about 2 m intervals. Muskeg and for-
est transects near Salt Lake Bay were established in
late summer, 1990, and in the Neka Valley in 1991.
Seedlings were counted in the planted scats annually
(in August) for three (Neka) or four (Salt Lake Bay)
years. For seedling censuses, each planted scat was
covered with a grid, and seedlings were counted in a
random selection of the grid squares. The proportion
of grid squares sampled usually ranged from 20% to
about 50% of the total scat. Emerging seedlings were
counted individually when possible, but so many seeds
germinated in some squares that it was impossible to
count them without destructive sampling, in which case
the abundance of seedlings was estimated visually.
The total number of emerging seedlings per scat was
extrapolated from this subsample. Curious bears and
heavy fall rains disturbed some of the planted scats and
thus reduced the usable sample size slightly. Because
it was impossible to mark individual seedlings in the
very dense clusters, the data are simply estimates of
annual germination, not of survivorship of seedlings.
Mortality of seedlings was very high and only a few
survived more than one year. We did not observe rodent
and bird predation on seeds in the experimental tran-
sects, although seed predation was sometimes evident
in scats on the road system.
The estimated percent of seeds germinating each
year was compared between habitats using a repeated-
measures ANOVA on arc-sine transformed data (PROC
GLM, SAS Systems Inc., Cary, North Carolina).
Because the power of this test was low (two sites,
two habitats), our results were re-examined, to see if
the outcome was merely a result of the few degrees
of freedom in the ANOVA. For this we used a t-test
(in which the planted scats were the replicates, so there
were more degrees of freedom in the test) to test for
differences in seedling germination between habitats
for the first and the last years at each site (no seedlings
in the censused grid squares survived for the entire
length of the experiment).
Results
Phenology of fruit consumption
Scats collected in early summer contained mostly
vegetable fiber and occasional deer remains (hair, bone,
hoof) with few seeds, as expected, because few fruits
are available at that time of year (some overwintered
THE CANADIAN FIELD-NATURALIST
Vol. 118
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Ficure |. Seasonal changes, for four years, in the percent of
bear scats containing seeds, Chichagof Island, south-
eastern Alaska. R, = 0.79, p < 0.001.
Viburnum and Maianthemum; some early Rubus spec-
tabilis). The frequency of seed-containing scats in-
creased through the summer, from less than 1% in
mid-June to over 90% in late August and early Sep-
tember (R, = 0.79, p < 0.001, n = 12; Figure 1).
Scat distribution at a small spatial scale
In addition to widespread deposition of scats on the
landscape (Patten 1993), defecations by a moving bear
can spread multiple deposits of a single defecation over
several meters, which could be ecologically important.
A survey of 1163 “scat trails” revealed that 42% were
multiple deposits, with 3% of them comprised of over
20 separate droppings spread over as much as 84 m.
Seed composition in scats
Seeds were identified at least to genus; in some
cases, the genus was represented by only one species
in this area (Sambucus racemosa, Rubus spectabilis,
Oplopanax horridum). In the case of Ribes, the species
was most likely bracteosum, which grew commonly
in this area. Likewise, Streptopus amplexifolius was
far more common in this area than two congeners.
Both Vaccinium ovalifolium and V. alaskense were
present and were not distinguishable in the scats. The
most commonly occurring seeds were Oplopanax,
Vaccinium, Ribes, Rubus, and Streptopus (Table 1).
Seeds had a high probability of being deposited
not only with numerous conspecifics but also with at
TABLE 1. Summary of frequency of occurrence of common kinds of seeds in scats on northern Chichagof Island. Data are
the number of months that the frequency of occurrence equaled or exceeded the stated value.
Kind of seed
Vaccinium Ribes Oplopanax Rubus Streptopus
Number of months = 20% 5 5) 1 1
3 ia “8
Number of months = 50% 3}
2004
WILLSON and GENDE: SEED DISPERSAL BY BROWN BEARS
TABLE 2. Average (S.E.) number of seeds per scat on northern Chichagof Island. N = 570 scats.
Year Month
Vaccinium Ribes
1990 July 3581 (667) 914 (767)
August 4655 (461) 700 (165)
September 2534 (468) 1918 (281)
199] July 4375 11(933) 2.02817 (-)
August 7193 (760) 364 (109)
September 4329 (795) 1302 (293)
4445 1971
x number of seeds/fruit* 47 12
x number of fruits 95 89
*from Traveset et al. 2004.
least one other kind of seed: in monthly samples, a
median of 60% (range 16-87%) of scats contained at
least two kinds of seeds, and sometimes as many as
five kinds. Vaccinium and Ribes were consistently the
most abundant seeds in scats collected (Table 2). In
most months, Rubus was next most abundant, followed
by Oplopanax and others. The maximum numbers
per scat for each of the genera listed in Table 2 were
approximately 37 000 Vaccinium, 14 500 Ribes, 7600
Rubus, 2000 Oplopanax, 1900 Sambucus, and 400
Streptopus. In addition to those represented in Table 2,
other kinds of seeds appeared in the scats sporadical-
ly (from fleshy fruits, Viburnum, Maianthemum; non-
fleshy fruits, Kalmia, Heracleum, Carex, grass).
Because the number of seeds per fruit differs greatly
among genera (Traveset et al. 2004), the approximate
number of consumed fruits of each type per scat differs
markedly from the abundances of seeds (Table 2).
The average scat represented only approximately 89
— 116 fruits of the most commonly consumed types.
Seed germination
Germination patterns were examined only for Vac-
cinium, Ribes, Rubus, and Oplopanax. A few Vaccinium
seeds germinated in the year they were planted (<1%
of all seeds estimated to be present); germination levels
were generally low (<6%) over the next four years
(Table 3). Annual germination of Oplopanax was also
rather low (<18%). In contrast, both Ribes and Rubus
germinated relatively well (up to 31-34% per year),
with the highest levels of germination often in the
second year after planting. All these kinds of seeds were
clearly capable of dormancy for at least four years.
There were no differences in germination percent-
ages between habitats for any species (ANOVA; range
of p-values: 0.17 — 0.82). The subsequent exploratory
t-test also revealed no differences between habitats
except for Vaccinium in one site — one statistically sig-
nificant outcome in 16 tests, which might happen by
chance alone. Variation among scats planted within a
habitat was relatively large, but it probably reflected the
biological reality of variation on a small spatial scale.
501
Kind of seed
Oplopanax Rubus Streptopus Sambucus
325). 1G18) 383 (91) = =
134 (22) 123) (182) 307 (8) 126 (42)
360 = (42) 830 (291) 41 (15) 88 (33)
3K (25) 650 (137) 47 (26) -
228 (40) 583 (120) 81 (20) -
374 (76) 54 = (20) 56 (12) 683 (606)
231 634 5] 110
2 42 22 3
116 15 2 37
Discussion
Bears are well-known frugivores, consuming many
species of fleshy fruits (Auger et al. 2002; Willson
1993). Fruits can be an important resource for prepar-
ing for winter dormancy and lactation (females give
birth in winter dens), and berry-crop failures can lead
to lower reproductive success (Rogers 1987). Bears can
consume many kilograms of fruits in a day (Welch et
al. 1997; Farley and Robbins 1995). Although a single
bear scat in the present study often contained thou-
sands of seeds, this represented relatively few fruits
and therefore only a small proportion of possible
daily consumption.
Composition of the fecal deposit can affect seed
germination and seedling growth (Traveset et al. 2001),
and the concentration of seeds in scats can lead to post-
dispersal seed predation and secondary dispersal via
scattering (Bermejo et al. 1998). Germination of seeds
passed by captive bears was generally similar to or
faster than that of seeds extracted from fruits by
researchers, although germination of some species
was quite low in all conditions and was sometimes
dependent on the substrates on which the seeds hap-
pen to land (Traveset and Willson 1997, 1998). But
rapid germination is not necessarily beneficial, if seed
dormancy is indeed an adaptation for dispersal in time.
The most important consistent effects of frugivory
by bears on seed dispersal may be transport, rather
than shifts of germination behavior of seeds passed
through the digestive tract. In a companion study, the
probability of seed deposition by Brown Bears on
Chichagof Island was greatest at 600-900m from a
source (Patten 1993). The greatest distance estimated
for seed transport by Brown Bears was over three km
(Patten 1993), and even though few seeds are likely
to be carried this far from their source, the extended
tail of the seed distribution pattern can be dispropor-
tionately important for dispersal ecology (Portnoy and
Willson 1992) and plant community ecology (Vellend
et al. 2003). Little habitat preference was shown by the
bears tracked on Chichagof, except for an avoidance
of bare-rock areas, so the probability of seed deposi-
502
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 3. Estimated average percent of seeds germinating per year in two common habitats at two sites on Chichagof Island,
southeastern Alaska.
Site Habitat Year Kind of seed
Vaccinium Ribes Oplopanax Rubus
Neka Forest 1992 3.9 (0.9) 0.2 (0.2) <0.1 = 22.5 (7.2)
n= 30 1993 2.8 (0.5) 30:8. e@li5e7) NS:42) HGLOSI) 28.5 (9.8)
1994 313 (0.9) 14.7 (9.0) 9.5 (4.9) 13.6 (4.8)
Muskeg 1992 5.9 (2:2) - Lal (1.0) 20.7 Ga)
n= 30 1993 2.9 (1.0) - 10.2 (8.4) 19.7 GS)
1994 1.2 (0.4) — TIEOe., .LO%6) 5.6 68)
Salt Lk Bay Forest 1991 2.4 (0.9) 19 x CluES)) 55} A) EOF (933)
n=60 1992 3.6 (0.8) 30.8 (16.2) 1.6 (0.8) 34.2 (8.7)
1993 1.8 (0.3) DES (es) iNet (0.5) 19.7 (6.9)
1994 ES (0.2) 1.0 (0.6) 3.0 (1.3) 9.8 (4.8)
Muskeg 1991 1.1 (0.5) 0.5 (0.5) 4.6 (2.7) heal (5.1)
n=49 1992 3.0 (1.0) 25.6 (10.4) 122, (0.7) 19.6 (6.9)
1993 1.8 (0.7) 6.3 (52) 0.9 (0.7) 10.7 (4.5)
1994 1.6 (0.8) 0.3 (0.2) 0.6 (0.4) 4.3 (3.0)
tion was proportional to habitat availability, including
logged areas (Patten 1993). Because forest was the
common habitat, this meant that the forest fruits, such
as most of the species examined here, had a fairly high
probability of deposition in the appropriate habitat
(Patten 1993). On a smaller scale, defecation by mov-
ing bears could increase the probability that seeds from
one defecation episode are deposited in more than one
habitat or microhabitat, as well as decrease the inten-
sity of seedling competition.
Germination of several forest and forest-edge species
was similar in forest and muskeg, indicating that habi-
tat distribution of these shrubs is not determined by
germination requirements at the habitat scale. The large
variances of the estimates of germination level not
only decreased the probability of detecting habitat
differences, but they also suggest that microhabitats
of seed deposition may be more important in deter-
mining germination success than habitats. Mortality
of seedlings was very high, in part an apparent result
of desiccation during periods of warm, sunny weather.
Especially at high densities, intra- and interspecific
competition was undoubtedly intense and probably
contributed to seedling mortality. However, occasion-
ally small groups of seedlings persisted and were still
alive when field work ended; similar “bear gardens”
were also found in natural settings (Willson 1994).
Bears are good seed dispersers: they commonly
transport germinable seeds up to hundreds of meters
from a source, often in appropriate habitat, simulta-
neously with a load of fertilizer that may influence
germination and growth. Although scats containing
numerous seeds produce conditions of high seedling
competition, several factors tend to reduce the impact
of competition on the effectiveness of dispersal. Ger-
mination may be spread over several years. Relatively
rapid passage through the gut and multiple defecations
per day within a bear’s home range spread scats over
the landscape. Scat trails of moving bears spread out
the seeds on a more local scale. Bears may be more
reliable dispersal agents for many kinds of seeds than
most frugivorous birds in this area, since the coastal
region is not a major flyway for migratory forest birds.
Acknowledgments.
This project was funded by the Pacific Northwest
Research Station, U.S. Forest Service. We are grate-
ful to J. Zasada for engaging us with bear-fruit inter-
actions, to our numerous field assistants, and to A.
Traveset for comments on the ms.
Literature Cited
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black bears (Ursus americanus) legitimate seed dispersers
for fleshy-fruited shrubs? American Midland Naturalist
147: 352-367.
Bermejo, T., A. Traveset, and M. F. Willson. 1998. Post-
dispersal seed predation in the temperate rainforest of
Southeastern Alaska. Canadian Field-Naturalist 112: 510-
512.
Farley, S. D., and C. T. Robbins. 1995. Lactation, hiberna-
tion, and mass dynamics of American black and grizzly
bears. Canadian Journal of Zoology 73: 2216-2222.
Hickey, J. R., R. W. Flynn, S. W. Buskirk, K. G. Gerow,
and M. F. Willson. 1999. An evaluation of a mammalian
predator, Martes americana, as a disperser of seeds. Oikos
87: 499-508.
Miller, S. D., G. C. White, R. A. Sellers, H. V. Reynolds,
J. W. Schoen, K. Titus, V. G. Barnes Jr., R. B. Smith,
R. R. Nelson, W. B. Ballard, and C. C. Schwartz. 1997.
Brown and black bear density estimation in Alaska using
radiotelemetry and replicated mark-resight techniques.
Wildlife Monographs 133: 1-55.
Patten, L. A. 1993. Seed dispersal patterns generated by brown
bears (Ursus arctos) in southeastern Alaska. MS thesis,
Washington State University, Pullman, Washington.
Portnoy, S., and M. F. Willson. 1992. Seed dispersal curves:
the behavior of the tail of the distribution. Evolutionary
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Rogers, L. L. 1987. Effects of food supply and kinship on
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bears on seed germination of fleshy-fruited plants in tem-
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Traveset, A., and M. F. Willson. 1998. Ecology of the fruit-
colour polymorphism in Rubus spectabilis. Evolutionary
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Traveset, A., T. Bermejo, and M. F. Willson. 2001. Effect of
manure composition on seedling emergence and growth of
two common shrub species of southeastern Alaska. Plant
Ecology 155: 29-34.
Traveset, A., M. F. Willson, and M. Verdi. 2004. Charac-
teristics of fleshy fruits in southeastern Alaska: Phyloge-
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Vellend, M., J. A. Myers, S. Gardescu, and P. L. Marks.
2003. Dispersal of Trillium seeds by deer: implications for
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Received 15 July 2003
Accepted 23 October 2004
A Mapping of the Present and Past Forest-types of Prince Edward Island
D. G. SoBey! AND W. M. GLEN?
! School of Applied Biological and Chemical Sciences, University of Ulster, Jordanstown, Northern Ireland BT37 OQB United
Kingdom. (Research Associate of the Institute of Island Studies, University of Prince Edward Island, Charlottetown,
Prince Edward Island)
2 Natural Resources Division, Department of Agriculture and Forestry, PO Box 2000, Charlottetown, Prince Edward Island
C1A 7N8 Canada
Sobey, D. G., and W. M. Glen. 2004. A mapping of the present and past forest-types of Prince Edward Island. Canadian
Field-Naturalist 118(4): 504-520.
Our aim was to produce maps showing the distribution on Prince Edward Island of five forest-types previously identified
from a TWINSPAN analysis of ground flora data collected at 1200 sampling points in a field survey. For this purpose we
had available two databases: one on the composition of the tree canopy of 82 957 forest stands, as determined by photo-
interpretation of a 1990 aerial, photographic survey of the island; the other on the drainage properties of the same stands
from a published soil survey. The tree canopy and drainage criteria for sorting these stands into five stand-types were chosen
in the light of the equivalent properties of the TWINSPAN forest-types as evident from the field survey. These criteria were
perfected in four trial computer-sortings, followed by the computer-printing of maps showing the distribution of the stand-
types. These maps, which were then evaluated by comparing them with the properties of the TWINSPAN forest-types, are the
first fine-scale maps of the main forest-types of the island. They reveal that, of the three “primary” forest-types, the upland
hardwood forest occurs especially in the central and south-eastern hill-lands, as well as in scattered parcels elsewhere,
whereas the Black Spruce forest and the wet species-rich woodland occur primarily in areas of lower elevation in the east
and west of the island. The two forest-types resulting from human disturbance, the White Spruce woods and the “disturbed
forest”, have a more scattered distribution, with the White Spruce woods being found especially in the central and eastern
parts of the island and the disturbed forest in the west and east of the island. A secondary aim was to map the conjectured
distribution before European settlement of the three primary forest-types: two maps have been produced, one showing the
distribution of upland hardwood forest, the other of the wet forest-types.
Key Words: forest classification, forest mapping, forest history, Prince Edward Island.
Between 1990 and 1992 the Prince Edward Island
Forestry Division carried out a comprehensive Forest
Biomass Inventory of the province, a component of
which was a field survey in 1991 at 240 randomly-
selected forest sites. At each of the sites the percentage
cover of the ground flora species in 4-m? plots was
recorded at five sampling points. The availability of
such ground flora data from such a large number of
plots (1200 in total) presented an unprecedented oppor-
tunity for the study and analysis of the woodland
ground vegetation and forest-types of Prince Edward
Island.
An earlier paper (Sobey and Glen 2002) presented
an analysis of the ground flora data in 1127 of the
plots using two multivariate techniques: TWINSPAN
— two-way indicator species analysis (a classification
technique), and DECORANA -— detrended correspon-
dence analysis (an ordination technique). TWINSPAN
led to the recognition of five forest-types, each char-
acterized by particular tree species and soil drainage
properties: (1) a wet species-rich swamp-type wood-
land, (2) upland hardwood forest, (3) Black Spruce
(Picea mariana) forest, (4) old field White Spruce
(Picea glauca) woods, and (5) disturbed conifer-dom-
inated forest. It was conjectured that the first three of
these forest-types were heavily modified descendants
of forest-types occurring at the time of European set-
tlement, while the two latter appeared to be largely the
product of successional processes associated with the
effects of human disturbance and forest clearance.
The DECORANA ordination provided further sup-
port for the overall importance of soil drainage and
human disturbance as the principal factors responsi-
ble for the differences between the five forest-types.
The aim of this paper is to expand the results of the
plant community analysis beyond the 1200 sampling
points to include the whole forested area of the island,
in the form of maps showing the total distribution of the
five forest-types on the island. Since the forest-types
were initially segregated and defined by TWINSPAN
on the basis of the composition of their ground flora,
the ideal mapping approach would have been to use
the ground flora composition of all forest stands on the
island as the basis for mapping the distribution of the
forest-types. However, such data are not available for
the whole forested area of the island and are never
likely to be. The forest-types thus had to be mapped
using data that showed a correlation with the ground
flora composition (1.e., data on the composition of
the tree canopy) and also for some, data on soil
drainage properties. It is fortunate that there were avail-
able two comprehensive relevant databases for the
504
2004
whole island: the more important was a database on the
tree species composition of all forest stands on the
island, based on an aerial photographic survey carried
out in mid-summer 1990; the other was the Prince
Edward Island Soil Survey (MacDougall et al. 1988)
which classified the soils of the island into 44 soil series
and mapped their distribution (at a scale of 1:10 000)
over the whole island. The soil survey proved useful in
the forest mapping because some of the TWINSPAN
forest-types had high levels of association with partic-
ular soil drainage properties.
It should be noted that none of the previous attempts
at forest classification and mapping that include Prince
Edward Island (Stilgenbauer 1929; Halliday 1937;
Rowe 1959; Loucks 1962) aimed to map what was
actually present on specific sites, nor do they contain a
high level of detail or accuracy. Halliday’s and Rowe’s
maps, being part of national studies, show no internal
differentiation at all in the forests of the island. Loucks
(working at the level of Maritime forests), did sub-
divide the island’s forests: he placed them in three
“forest districts” but the boundaries of these are very
generalized on his map. One comprised the hardwood
areas of the central and eastern parts of the island; the
other two were coniferous districts: one in the west
along the shores of Northumberland Strait, the other
running along the length of the northern shore. The
map showing the greatest detail (Stilgenbauer 1929)
is actually the earliest of the four, but Stilgenbauer’s
descriptions of his “forest belts” are brief and quali-
tative and the criteria he used for delimiting them are
not given. In addition to these mapping studies, there
is a useful descriptive summary of the forest-types of
the island in Erskine (1960), and in Appendix 1 the
stand-types emerging from this study are equated with
Erskine’s descriptions.
The principal objective of this study was thus, mak-
ing use of two comprehensive databases, to map the
total distribution on Prince Edward Island of the five
forest-types recognized in a TWINSPAN analysis, and
to further verify the validity of the maps by comparing
the properties of the mapped stands with those of the
TWINSPAN forest-types. Such a mapping will not only
give us a clear picture of the current actual distribution
on the ground of the main forest-types on the island,
but should also assist us in understanding the factors
responsible for their distributions. A secondary objective
(on the basis of any stand and soil relationships that
might emerge) was to attempt to extend the mapping
back into historical time in order to obtain a picture of
the possible distribution of the forest-types before the
advent of the large scale forest clearance that began
in the eighteenth century with the beginning of Euro-
pean settlement on the island.
Methods
The methodology leading to the description of the
forest-types and their mapping makes use of several
SOBEY AND GLEN: PRESENT AND PAST FOREST-TYPES OF P.E.I.
large independently obtained databases and involves
a number of different stages in processing and analysing
the data they contain. Figure | shows these databases
and stages in diagrammatic form. The end-product,
computer-produced maps of the five forest-types, is
the result of a computer-sorting of 82 957 demarcated
stands of “high forest” (i.e., excluding alder woods,
plantations, clear-cut and burned areas) into five forest-
types on specific tree canopy and soil drainage criteria.
In the description of the various steps in the analysis, the
text that follows is linked to the stages shown in Fig-
ure | by Roman numerals in square brackets, e.g.: [I].
The databases:
1. The 1991 field survey: ground flora and tree canopy
data
Of the vast amount of data collected at the 1200 sam-
pling points in the 1991 field survey, two data sets,
one on the ground flora [II], the other on the tree can-
opy [III], are of relevance to this report. We present
here only a summary of the methods used to collect
these data — full field methods are given in Sobey and
Glen (2002).
The data were collected between June and Sep-
tember 1991 at 1200 ground flora plots located at
240 randomly-selected forest sites. At each sampling
point the tree canopy was assessed using a “point
sampling” technique involving the use of a “variable-
radius plot” centred on the sampling point (Watts
1983). From these field data, the percentage contribu-
tion of each tree species to the total woody biomass (to
the nearest 10%) in each variable radius plot was cal-
culated [III]. The ground flora species were assessed
within a circular 4-m? plot, with each species being
given a percentage cover value to the nearest 10%,
with a minimum value of 5% [II].
The TWINSPAN classification and the recognition of
five forest-types
The TWINSPAN classification of 1127 of the 1200
ground flora plots (based on the species composition
and percentage cover of their ground flora species)
resulted in the recognition of 11 ground flora plot
groups or community-types [V] (see Sobey and Glen
(2002) for a full description of the methodology —
note that 73 plots were omitted from the analysis
either because no trees were recorded in the area of
the sampling point, or because no ground flora species
were present in the 4-m* plot). These plot groups
were then examined in terms of the species composi-
tion of the tree canopy and other properties at the sam-
pling sites (especially soil drainage), and as a result
five major forest-types were recognized [VII]. (See
Sobey and Glen (2002) for summary descriptions of
each of these forest-types and maps showing the dis-
tribution of their sampling points on the island.)
2. The 1990 aerial survey: the forest stand database
Complete aerial photographic coverage of the
island was carried out in mid-summer 1990 as part of
506
1990 AERIAL
PHOTO SURVEY:
1:17 500-scale photos
of the whole Island
IV
PHOTO-INTERPRETATION:
demarcation and description
of 82 957 forest stands:
= Stand database
XI
THE CANADIAN FIELD-NATURALIST
a Il
1991 FIELD SURVEY:
Ground flora data from
4-m plots at 1200
sampling points
TWINSPAN
CLASSIFICATION:
=» Recognition of
11 ground flora
community-types
VII ANALYSIS of
TWINSPAN GROUPS
with the aid of tree canopy
and soil series data
for the 1200 points:
=» Recognition of five
forest-types
VIE SELECTION of
TREE CANOPY & SOIL
DRAINAGE CRITERIA
for classification of 82 957
stands into five forest-types
COMPUTER SORTING
of the 82 957 forest stands corresponding to
the five forest-types, using the selected tree
canopy and soil drainage criteria
COMPUTER MAPPING
of the stands corresponding to each
of the island's five 1990 forest-types
Vol. 118
1991 FIELD SURVEY:
Tree species data from
‘variable-radius’ plots at
1200 sampling points
Vi 1988 P.E.I.
SOIL SURVEY:
Description and
mapping of 44
soil series for
the Island
IX DATABASE of
SOIL SERIES &
DRAINAGE CLASS
for the 1200
sampling points
x
DATABASE of SOIL
DRAINAGE CLASS
for 82 957 forest
stands
FIGURE 1. The stages leading to the mapping of the 1990 forest-types on Prince Edward Island: a flow diagram showing the
databases used (in the boxes with heavy borders) and the analyses carried out.
the 1990-1992 Prince Edward Island Forest Biomass
Inventory [I]. The false-colour infra-red photographs
resulting from the survey (scale c. 1:17 500) were
analysed by trained photo-interpreters in the Forestry
Division with the purpose of dividing the total forest-
ed area into “stands” which were then recorded on a
map as “polygons” [IV]. For the purpose of the
photo-interpretation, a stand was taken to be a group
of trees having a relatively uniform visual appearance
from the air as evident in the aerial photograph.
Stands could comprise a single species or several or
many species, but they are generally of a uniform
species composition, height and density. For each of
the 82 957 stands, up to five tree species, each con-
2004
SOBEY AND GLEN: PRESENT AND PAST FOREST-TYPES OF P.E.I.
507
FIGURE 2. The distribution of “high forest”, based on photo-interpretation of the 1990 aerial photographic survey of the
island. (High forest excludes Speckled Alder woods, plantations, and clear-cut and burned areas.)
tributing greater than 5% crown closure to the canopy,
were recorded, with the percentage contribution of
each species being estimated to the nearest 10%. The
database resulting from the photo-interpretation was
computerised, and the stand boundaries were linked
to the Geographic Information System (G.LS.) for the
province, enabling the direct plotting onto maps of
stand boundaries and areas, as well as the extraction
of data on their tree species make-up.
3. The 1988 soil survey of Prince Edward Island: a soil
series database
The most recent major soil survey of the island
(MacDougall et al.1988) has resulted in the classifi-
cation of the island’s soils into 44 soil types or “series”,
and the mapping (scale: 1:10 000) of the distribution
of these series over the whole island [VI]. The soil
maps have been digitized in the G.I.S. for the island,
such that the soil series at each of the sampling points
in the 1991 field survey [IX], as well as for each forest
stand polygon in the aerial stand database [X], are
accessible by computer. For this study it was decided
that it would also be useful to group the 44 soil series
into six drainage classes: rapidly-drained, well-
drained (coarse-textured parent materials), well-
drained (medium-textured parent materials), imperfect-
ly-drained, poorly-drained, and organic soils.
Selection of the tree canopy and soil drainage criteria.
The selection of the criteria for dividing the 82 957
stands of high forest (i.e., the area shown in Figure 2)
into the five forest-types [VII] (or “stand-types” as
they will be termed to distinguish them from the
TWINSPAN-defined forest-types), was based on the
tree canopy and soil drainage properties of the five
TWINSPAN forest-types as evident from the 1991
field survey (Sobey and Glen 2002). Four trial com-
puter sortings on selected criteria were carried out in
succession; the results of each trial were evaluated
and the criteria for each of the five stand-types were
then redefined and a new sorting was carried out.
Eventually the perfected criteria were chosen (Table
1), and all of the stands in the database were comput-
er-sorted on these criteria [XI], followed by the com-
puter-printing of maps showing the distribution of
each stand-type on the island [XII]. It should be
noted that in any of the sortings the order of the sort
(i.e., of the selecting and removal of each stand-type)
is important, since once a stand has been sorted it is
normally no longer available for inclusion in subse-
quent stand-types even if it should meet their particu-
lar criteria. The following is a more detailed discus-
sion of the criteria used for each of the five
forest-types, as well as of some of the changes made
as a result of the trial sortings:
I. Upland hardwood forest. In the TWINSPAN classi-
fication Sugar Maple (Acer saccharum) and American
Beech (Fagus grandifolia) had been virtually restrict-
ed to sampling points belonging to the upland hard-
wood forest-type (Sobey and Glen 2002). Yellow
508
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 1. The criteria used in the sorting of 82 957 stands of “high forest” on Prince Edward Island into five stand-types
corresponding to the five forest-types recognized in a TWINSPAN classification of 1127 ground flora plots.
SELECT AND REMOVE: stands designated as clear-cut, burned, plantation, windfall, or alder. This leaves 82 957 stands of
“high forest”
First Sort: Excluding any stands containing White Ash, Eastern White Cedar or White Elm, select all stands containing
Sugar Maple, American Beech or Eastern Hemlock, plus all stands with Yellow Birch, but for the last species excluding
those stands on poorly-drained, imperfectly-drained or organic soils.
1. Upland hardwood forest
SECOND Sort: Excluding any stands containing White Ash, Eastern White Cedar or White Elm, select all stands containing
Black Spruce with crown closure 2 50%.
2. Black Spruce forest
THIRD Sort: Select all stands containing White Elm, White Ash, or Eastern White Cedar, and/or classed as ‘swampy’, plus
all stands with a crown closure of total hardwoods = 50% and occurring on poorly-drained or imperfectly-drained soils.
3. Wet rich woodland
FourTH Sort: Select all stands containing White Spruce with crown closure = 40%.
4. White Spruce woods
RESIDUAL STANDS:
Birch (Betula alleghaniensis) had a somewhat wider
distribution, also occurring at a rather high level at
wet rich woodland sampling points. In the initial trial
sortings all stands containing any presence of Sugar
Maple, American Beech and Yellow Birch were select-
ed; however, for the final sorting it was decided to
exclude those stands selected due to the presence of
Yellow Birch that occurred on poorly-drained, imper-
fectly-drained or organic soils, soils more characteristic
of wet rich woodland than of upland hardwood forest.
Also, in the final sort, Eastern Hemlock (Tsuga
canadensis) was included as a selecting species, and
stands containing American Elm (Ulmus americana),
Eastern White Cedar (Thuja occidentalis) and White
Ash (Fraxinus americana), all characteristic of wet rich
woodland, were specifically excluded.
2. Black Spruce forest. The problem in segregating
stands of this forest-type was choosing a minimum
percentage crown closure for Black Spruce. Since the
mean percentage woody biomass contribution of
Black Spruce at the Black Spruce forest sampling
points was 53.1% (Sobey and Glen 2002), it was decid-
ed to set both a high value and also one that made ecolog-
ical sense: the criterion used in the final sort was that
for a stand to be assigned to Black Spruce forest, at
least 50% of its canopy had to be Black Spruce.
From the earlier trial sortings it had also become evi-
dent that it was necessary to exclude any stands con-
taining American Elm, White Ash or Eastern White
Cedar, species virtually absent from this forest-type.
3. Wet rich woodland. In the early trial sortings an
attempt was made to select stands of this forest-type
on the percentage crown closure of its most impor-
tant tree species: Red Maple (Acer rubrum) — a mini-
mum crown closure of = 25% was set. However, the
problem was that Red Maple was also present at high
5. “Disturbed forest”
levels in the still unsorted “disturbed conifer-dominated
forest’. It was thus decided to make use of the fact
that 80.2% of the sampling points of the TWINSPAN
wet rich woodland occurred on imperfectly- and
poorly-drained soil series (Sobey and Glen 2002). In
the end the criterion used was firstly to select all stands
containing the minor tree species diagnostic of this for-
est-type (as evident in the TWINSPAN classification):
ie., White Ash, American Elm and EasternWhite Cedar,
as well as all stands classified as “swampy” by the
photo-interpreters. Then, since an overall factor dis-
tinguishing the TWINSPAN wet rich woodland sam-
pling points from the disturbed conifer-dominated
forest was a higher level of total hardwoods (Sobey
and Glen 2002), we selected all stands with a minimum
total hardwood crown closure of 50%, in combina-
tion with a requirement that all such stands be on
poorly- and imperfectly-drained soils.
Having selected the stands that appear to be derived
from pre-European settlement forest-types, the next step
was to separate the remaining stands into the two types
of successional and disturbed forest: i.e., White Spruce
woods and disturbed conifer-dominated forest.
4. White Spruce woods. Here it was a matter of selecting
the minimum percentage crown closure of White
Spruce for a stand to be assigned to White Spruce
woods. Given the fact that the mean percentage contri-
bution of White Spruce to the woody biomass of
TWINSPAN White Spruce woods sampling points was
62.2 % and in the disturbed conifer-dominated forest it
was 16.7% (Sobey and Glen 2002), a middle level
(40%) was chosen.
5. Disturbed conifer-dominated forest (or simply
“disturbed forest”). The residual stands should by
default correspond to the remaining TWINSPAN for-
est-type (disturbed conifer-dominated forest), even if
2004
SOBEY AND GLEN: PRESENT AND PAST FOREST-TYPES OF P.E.I.
509
TABLE 2. The number of hectares and stands (also as percentages) assigned to each stand-type in the computer-sorting. A
percentage breakdown of the stand area by drainage class is also given, as is its status in 1935 as either forest-covered or
cleared land as determined from a 1935 aerial photographic survey of the whole island. (In brackets after the forested per-
centage is the equivalent parameter for the TWINSPAN forest-type sampling points of the 1991 field survey — those bolded are
within + 20% of the stand value.)
STAND-TYPES
Upland Black
Hardwood Spruce
Forest Forest
HECTARES 55 043 33 106
Percentage of area Dei 13.1
NUMBER OF STANDS 16 170 8 049
Percentage of stands 19.5 9.7
DRAINAGE CLASS (% of area)
Organic 0.04 6.8
Poorly-drained 5.8 54.8
Imperfectly-drained 39 16.8
Well-drained (medium) LG) 1.1
Well-drained (coarse) 74.4 9.0
Rapidly-drained 12.9 10.2
Unclassified 0.28 s3
STATUS in 1935 (% of area)
Forested 93.8 TP
(86.4) (67.5)
Cleared land 6.2 22.8
all are not in fact dominated by conifers. In the trial
sortings an additional fifth sort was carried out in
order to separate out the residual stands that were
indeed conifer-dominated. This was done by sorting
on a minimum conifer crown closure of = 50% — this
selected 42% of the residual stands. The other group
was thus termed “disturbed hardwood-dominated for-
est’, i.e., comprising residual stands with hardwoods >
50% crown closure. However, in the end, the distinc-
tion between hardwood and softwood domination in
the residuals was not considered important and these
stands have been simply termed “disturbed forest”.
Results
Table 2 presents the results of the final computer
sorting, expressed in terms of the area in hectares and
the number of aerial stands assigned to each stand-
type, both also expressed as percentages. Table 2 also
gives a breakdown of the soil drainage classes for
each of the stand-types and their status in 1935 (as
“cleared land” or “forested”), as determined from
analysis of the earliest aerial photographic survey of
the island (see Glen 1997). The tree species make-up
of the five stand-types is shown in Table 3 and the
computer-printed maps showing their distribution on
the island are shown in Figures 3 to 7.
In the sorting, the 1990 “high forest” of the island
was divided into five stand-types — see Appendix | for
summary descriptions of each of these stand-types.
These fall naturally into two groups, each of which
occupies about half of the island’s forested area: (1)
White
Wet Rich Spruce Disturbed
Woodland Woods Forest TOTALS
42 192 57 982 65 259 253 582
16.6 22.9 Dwi 100
13 863 22 709 22 166 82 957
16.7 27.4 26.7 100
0.78 0.58 0.86 1.4
70.1 11.6 14.5 25.8
24.6 8.1 7.8 10.7
0.74 2.8 5.0 2.4
2D) 48.3 46.2 35.6
13 213 24.1 14.9
0.18 IED eS) 0.93
75.8 37.6 67.4 69.0
(79.5) (24.4) (74.2) (69.5)
24.2 62.4 32.6 31.0
the three stand-types which appear to be recognizable
descendants (even if heavily-modified) of pre-European
settlement forest-types (upland hardwood forest,
Black Spruce forest and wet rich woodland) — these
make up 51.4% of the area under high forest; (2) the
two other stand-types (old field White Spruce woods
and “disturbed forest’), representing more disturbed
and/or successional types not likely to have been impor-
tant in the pre-European forest — these make up the
other 48.6%. It is likely that before the period of
European settlement, land surfaces now under these
two latter stand-types would have been covered by
one of the three “primary” stand-types.
Evaluating the validity of the stand-types
One way of assessing the validity of the products of
the sorting is to compare, as in Table 3, the tree species
composition of each stand-type (in the form of per-
centage crown closure) with the equivalent parameters
of the corresponding TWINSPAN forest-type: the per-
centage contribution to woody biomass in the 1200
variable-radius plots of the ground survey, and the con-
tribution of each of the tree species to the percentage
crown closure in those stand polygons in which the
1200 variable-radius plots were located. Another way
to assess the validity of the sorting is to compare the
drainage properties and the status in 1935 of the aerial
stand-types with those of the TWINSPAN-based forest-
types (Tables 2 and 4). The data required for these
comparisons were extracted using the Database pro-
gram “FoxPro” from the 1991 field survey database
510 THE CANADIAN FIELD-NATURALIST Vol. 118
TABLE 3. The mean percentage crown closure (+ S.E.) of the principal tree species in each stand-type (based on all the
stand-polygons of each stand-type including those in which the species was not recorded). To enable comparison of these
values with the equivalent parameters for the TWINSPAN forest-types, placed below in round brackets is the mean percentage
contribution (+ S.E.) of each tree species to the total tree biomass in the variable-radius plots of the corresponding
TWINSPAN forest-type; and in square brackets the mean percentage crown closure of the tree species (+ S.E.) in those stand-
polygons in which the variable-radius plots were located. For crown closure values (unbracketed) > 10%, a bolded percent-
age within the brackets indicates that there is “good agreement” between the two values (i.e., the bracketed value lies within
+ 20% of the unbracketed value), while an italicized bolded percentage indicates a “notable discrepancy” between the two
values (i.e., the bracketed value is > + 50% of the unbracketed value); where crown closures (unbracketed) were < 10%, the
differences were assessed subjectively on the basis of their relative magnitudes.
STAND-TYPES
ALL STANDS
Upland Black Wet White (All 1200 plots +)
Hardwood Spruce Rich Spruce Disturbed [AIl 1200 sampling
Forest Forest Woodland Woods Forest point stands]
CONIFERS:
Picea mariana 0.22+0.020 71.4+0.18 9.9+0.13 1.1 + 0.034 5.3 + 0.079 10.4 + 0.080
(0.72+0.35) (53.1 +4.9) (3.8 + 1.2) (4.3 + 1.5) (10.1 + 1.4) (5.4 + 0.57)
[0.79 + 0.28] [39.6 + 3.8] [13.3 + 1.7] [4.1 + 1.1] [12.4 + 1.3] [9.1 + 0.59]
Picea rubens 0.59+ 0.032 0.69 + 0.042 2.9 + 0.072 0.47+0.021 7.1 +0.096 2.7 + 0.036
(0.88 + 0.27) (17.3 +3.8) (0.51 + 0.30) (4.6 + 1.2) (Gfe Wien bi) (2.8 + 0.32)
[0.98 + 0.28] [3:3 1:2] (5.4 + 1.1] [3.0 + 1.1] [3.6 + 0.66] [2.6 + 0.28]
Picea glauca 4.8 + 0.086 1.6 + 0.068 8.2+0.11 68.1+0.13 10.4+0.078 24.2+0.11
(8.6 + 0.92) (32 £723) (18.0 + 2.2) (62.2+3.4) (16.7+ 1.5) (17.0 + 1.0)
[10.3+0.94] [25.1 + 3.4] [7.3 + 0.98] ATDE3:01 ) 7a 13) [17.5 + 0.76]
Abies balsamea 9.0 + 0.093 4.8 + 0.086 5.6 + 0.072 3.8 + 0.053 9.0 + 0.089 6.6 + 0.037
(18.9 + 1.2) (6.9 + 1.9) (13.5 + 1.5) (8.4 + 1.7) (24.9 + 1.6) (17.6 + 0.75)
[10.2 + 0.60] [7-32] [7.8 + 1.0] [5.6+ 0.77] [11.1 + 0.67] [8.9 + 0.33]
Tsuga canadensis 0.12 + 0.012 0 0 0 0 0.023 + 0.0023
(0.32 + 0.16) (0) (0) (0.81 40.54) (0.42+0.25) (0.40 + 0.14)
[0] [0] [0] [0] [0] [0]
Larix laricina 0.082 +0.0097 8520.11 5.4 + 0.075 6.0 + 0.075 12.8 + 0.16 7.1 + 0.052
(0.48 + 0.18) (9.0+2.1) (7.3 + 1.7) (3.7+0.84) (3.84 0.69) (2.6 + 0.31)
[1.5 + 0.35] [9.5 + 1.5] [7.8 + 1.2] [8.8 + 1.6] [7.6 + 0.81] [5.3 + 0.37]
Thuja occidentalis 0 0) 1.2 + 0.037 0 0 0.20 + 0.0064
(0.42+0.25) (0.12 + 0.13) (TET) (0) (0.64+0.32) (0.93 + 0.23)
[0.023 + — ] [0] [0.38 +— ] [0.15+-] [0.39+0.14] [0.17 + 0.041]
TOTAL CONIFERS 14.9 87.3 34.9 80.4 46.3 51.4
(30.4) (94.4) (50.0) (84.1) (64.5) (47.3)
[23.8] [84.7] [42.0] [69.6] [52.4] [44.4]
BROAD-LEAVES:
Acer rubrum Sysifas OBL 4.8 + 0.086 25) 210a3 5.4 + 0.061 20.1 + 0.12 18.7 + 0.063
(33.3+41.4) (2.5 +0.77) (24.6 + 2.4) (4.6 + 1.1) (19.0 + 1.5) (Bales 1)
[30.4 + 0.73] [5.1 + 1.1] [26.3 + 1.5] [8341.1] [18.9+0.92] [21.7+0.52]
Acer saccharum 21.6+0.10 0 0.45 + 0.030 0 0 4.3 + 0.036
(9.7 + 0.89) (0) (1.7+0.56) (0.59+0.46) (0.28 +0.13) (4.9 + 0.54)
[16.7 + 0.76] [0.5 +-] [2.1 + 0.55] [20160] [35.053] [7.7 + 0.38]
Betula alleghaniensis 7.8 + 0.070 0) 0.22+0.016 0.013 + 0.0026 0.090 + 0.0024 1.6+0.017
(5.6 + 0.62) (0) (3.3 + 0.84) (0.22+0.13) (1.4+0.40) (3.9 + 0.39)
[6.7 + 0.41] [0] (0.71+0.22] [1.0+0.35] [0.92 + 0.23] (3.0 + 0.19]
Betula papyrifera 137+ 01087, 2:5 = 01059 12.7 + 0.089 6.3+0.059 13.4+0.088 10.3 + 0.039
(9.2+0.74) (0.63 + 0.36) (5.6 + 0.94) (3.6+0.78) (41+0.60) (7.3 + 0.50)
{13.1+ 0.53] [2.5 + 0.65] (11.9+0.97] [6.9+0.85] [11.4+0.66] [10.8 + 0.33]
Fagus grandifolia 1.5 + 0.036 0 0.017 + 0.0044 0 0 0.30 + 0.0073
(4.1 + 0.58) (0) (0) (0.37+0.24) (0.23+0.11) (2.7+0.37)
[1.1 + 0.19] [0] [0.19 +—] (0.074+-—] [0.21+0.10] [0.49 + 0.074]
(continued) on next page
2004 SOBEY AND GLEN: PRESENT AND PAST FOREST-TYPES OF P.E.I. S51]
TABLE 3. (continued from previous page)
STAND-TYPES
ALL STANDS
Upland Black Wet White (All 1200 plots +)
Hardwood Spruce Rich Spruce “Disturbed [AIl 1200 sampling
Forest Forest Woodland Woods Forest” point stands]
Populus spp. ¢ 4.6 + 0.075 5.0 + 0.090 21.4+0.15 7.6+0.070 18.8+0.14 I23:2.0/057
(4.1 + 0.65) (1.1 + 1.0) (7.8 + 1.6) (4.7 + 1.2) (7.4 + 1.1) (6.6 + 0.62)
[6.9 + 0.53] [6.8 + 1.2] {11.2+1.0] [10.7+1.1] [10.9+0.80] [9.6 + 0.39]
Fraxinus americana 0 0 0.32 + 0.019 0 0 0.053 + 0.0031
(0.40 + 0.21) (0) (1.6 + 0.75) (0) (O) (0.46 + 0.16 )
[0] [0] [0] [0] [0] [0]
Ulmus americana 0 0 0.84 + 0.035 0 0 0.14 + 0.0058
(0.26 + 0.14) (O) G2 saie1) (0) (0) (0.57 + 0.17)
[0.47+ — | [0] (0.13 +-] [0] [0.035+-—] [0.042 + 0.019]
Alnus incana 0.047 + 0.011 0.26 + 0.027 4.8+0.11 201039" Os 01052 6.4 + 0.071
(-) (-) (-) (-) (-) (-)
[0.16 + 0.12] [0] (4.0+1.2] [1.1+0.63] [0.85 + 0.38] [et e10:22]
TOTAL BROAD-LEAVES 85.1 12.5 65.1 19.6 3 47.8
(excluding Alnus) (70.0) (5.3) (50.0) (16.5) (35.0) (52.7)
[75.6] [14.9] [56.7] [30.3] [46.9] [55.6]
Number of Stands 16,170 8,049 13,863 22,709 22,166 82,957
¥ For “all 1200 plots” the value in round brackets is the percentage contribution to the total above ground biomass (oven-
dry tonnes per hectare) in all 1200 variable-radius plots.
+ Because it is impossible to distinguish the three native poplar species in aerial photographs (Populus tremuloides, P.
balsamifera, P. grandidentata) they were grouped as “Populus spp.” — however almost all of this is likely to have been
P. tremuloides (Trembling Aspen).
FIGURE 3. The distribution of stands of upland hardwood forest in 1990.
a2 THE CANADIAN FIELD-NATURALIST Vol. 118
Ficure 4. The distribution of stands of Black Spruce forest in 1990.
FicureE 5. The distribution of stands of wet rich woodland in 1990.
2004
SOBEY AND GLEN: PRESENT AND PAST FOREST-TYPES OF P.E.I.
FIGuRE 6. The distribution of stands of White Spruce woods in 1990.
FIGURE 7. The distribution of stands of “‘disturbed forest” in 1990.
514
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 4. The soil drainage classes of the stand-types (derived from the 1:10 000 soil series maps of MacDougall et al.
(1988)) expressed as the percentage of the stand-type’s total area in each drainage class, ignoring the area of unclassified
drainage. These are compared with the drainage classes of the corresponding TWINsPAN forest-types: (1) (in round brackets)
the soil drainage class at the sampling points of the 1991 field survey as determined from soil pits, and (2) [in square brack-
ets] the drainage class of those soil series polygons in which the sampling points were located, derived also from Mac-
Dougall et al. (1988), both values being expressed as the percentage of the total area or of the sampling points in each
drainage class. *
STAND-TYPES
Upland Black
Hardwood Spruce
SOIL DRAINAGE CLASS Forest Forest
Poorly- and imperfectly- 9.8 79.4
drained soils (+ organic)(%) (1.9) (66.3)
[12.9] [73.8]
Well- and rapidly- 90.2 20.6
drained soils (%) (98.1) (33.8)
[87.1] [26.3]
White ALL
Wet Rich Spruce “Disturbed STANDS
Woodland Woods Forest” —_ (or points)
95.7 20.6 23.6 39.2
(58.3) (1.5) (15.9) (18.4)
[80.3] [14.0] [37.5] [33.6]
4.3 79.4 76.4 60.8
(41.6) (98.5) (84.1) (81.6)
[19.9] [85.9] [62.5] [66.4]
*For the meaning of the bolding and italicizing see the caption of Table 3.
and the 1990 aerial stand database, and then linked to
the “MapInfo” G.LS. for the province.
(1) Comparing the composition of the tree canopy
To facilitate the overall interpretation of the many
comparisons being made, indices were selected for
assessing the closeness of the two values: if the equiv-
alent parameter for the TWINSPAN-based forest-type
lay within + 20% of the aerial-stand value, this was
taken to indicate “good agreement” between the two
values, whereas if the parameter was greater than + 50%
of the aerial-stand value this was considered a “notable
discrepancy”. On the basis of these criteria, it is evident
that in overall terms there is a reasonably good fit
between the mean tree canopy composition of the
stand-types based on all of the stand polygons (Table
3), and the canopy composition of those stand poly-
gons that contained the 1200 variable-radius plots: there
are 29 “good agreements” and only two “notable dis-
crepancies” for the crown closure of individual species.
However, when the mean tree canopy composition for
all of the stand polygons is compared with the per-
centage contribution to woody biomass in the variable-
radius plots, the match is not as good: here there were
15 “good agreements” and 17 “notable discrepancies”.
This greater level of discrepancy is not surprising
considering that this latter comparison is between
plots of different size (i.e., forest stands of variable size,
but measured mostly in hectares (the mean stand area
was about 3 hectares) and variable-radius plots with a
mean size of about 100 m7), as well as different parame-
ters (percentage crown closure as determined from an
aerial photograph, with the percentage contribution to
woody biomass based on the trunk diameter of the
trees within the variable-radius plots).
Also relevant here is the greater difficulty in identi-
fying tree species from an aerial photograph compared
with the examination of actual specimens in a field
survey. The photo-identification was based on such
characters as texture, shape, colour and site (e.g., wheth-
er on upland or lowland). The conifers in particular
presented problems: Balsam Fir (Abies balsamea) when
present as an understorey species may not be apparent
from the air; the three spruce species were frequently
identified from their site: i.e., if in upland forest, it
was listed as Red Spruce (Picea rubens), in lowland,
Black Spruce, and on old-field sites, White Spruce, but
this was not an infallible approach. Thus the photo-
identification was not 100% accurate: the standard re-
quired for the 1990 aerial survey, confirmed by ground
checks, was that at least 70% of the species-cover
identification in a stand be correct for at least 90% of
the time. Bearing these points in mind we observe
the following:
Upland hardwood stands. In almost all of the compar-
isons (Table 3) there is generally a good correspondence
between the parameters of the aerial stand-type and
those of the TWINSPAN-defined forest-type.
Black Spruce stands. There are problems with the
spruces (perhaps due to the problem in identifying the
spruces, discussed above): in Table 3 the most notable
discrepancy is the very low Red Spruce contribution
to the aerial stand-type (<1%) compared with its level
in the variable-radius plots (17%). Also evident is the
fact that Black Spruce is at a somewhat higher level in
the aerial stand-type (71%) compared with either of the
values for the TWINSPAN-defined forest-type. This is
presumably due to the high crown closure level (i.e.,
50%) that was set as the criterion for inclusion of Black
Spruce stands in this group.
Wet rich woodland stands. The chief species, Red
Maple, shows no difference in either of the comparisons
2004
(Tables 3). However, there are some discrepancies: the
use of a sorting criterion of 2 50% hardwoods must be
the reason for the higher overall hardwood contribution
in the aerial stand-type compared with the TWINSPAN
forest-type, as well as the higher individual contribu-
tions of Trembling Aspen (Populus tremuloides) and
White Birch (Betula papyrifera), though there is no dis-
crepancy for the latter species in the comparison of the
crown closures. Concomitantly, the conifer contribution
is less in the aerial stand-type than in the variable-radius
plots, but again there is less discrepancy for the crown
closure comparison.
White Spruce stands. In overall terms there is a good
correspondence between the two classifications, with
the main species, White Spruce, giving a reasonably
good fit — this time the better fit is for the variable-
radius plot comparison (Table 3).
“Disturbed forest” stands. This residual group has a
smaller total conifer component than the TWINSPAN
“disturbed conifer-dominated forest” (this discrepancy
is less evident in the comparison of the crown closures
— Table 3), and this is reflected especially in the levels
of Balsam Fir (for the variable-radius plot comparison
only), and to a smaller degree, in White Spruce and
Black Spruce. Oddly, Tamarack (Larix laricina) is con-
siderably higher in the aerial stand-type than it is in the
variable-radius plots. Concomitantly, the hardwoods
(notably Trembling Aspen) are higher in the aerial
stand-type, while there is no difference for the levels of
Red Maple.
(2) Comparing the soil drainage classes and the 1935
Status
There is a reasonably good agreement between the
aerial stand-types and the TWINSPAN forest-types
in their drainage class breakdown (Table 4), especially
for the drainage classes as determined from the soil
series at the 1200 sampling points. There is less agree-
ment with the drainage classes as determined from the
soil pits dug at the sampling points during the field
inventory. The one showing the least correspondence is
the wet rich woodland which has higher levels of poor-
ly- and imperfectly-drained soils in the aerial stands,
due to the direct use of these drainage classes as a
sorting criterion. The status of the stands and sam-
pling points in 1935 (1.e., whether they were forested
or cleared land at that time) is in broad agreement for
most of the forest-types (Table 2), with the greatest
discrepancy being for the White Spruce woods.
Discussion
The TWINSPAN analysis of the 1991 field survey
data (Sobey and Glen 2002) indicated the presence of
five main forest-types on Prince Edward Island, three
of these showing a relationship with pre-European
settlement forest-types and two appearing to largely
owe their presence to human influences. The objective
of the current paper was the production of maps show-
SOBEY AND GLEN: PRESENT AND PAST FOREST-TYPES OF P.E.I.
S15
ing the total distribution of these five forest-types. This
objective has been achieved, and for the first time ever
we have fine-scale whole-island maps showing the
distribution of the main forest-types. Furthermore, these
maps have been produced using largely objective cri-
teria and methods, and they are based on the actual for-
est present at a specific time (in the summer of 1990),
with every mapped stand being locatable on the ground
and thus potentially verifiable.
How valid are the maps as a picture of the distribu-
tion of the five forest-types on the island? Firstly, the
maps appear to make ecological and geographical sense:
the upland hardwood forest (Figure 3) occurs in areas of
higher elevation (in island terms), and on soils having
good drainage (Tables 2 and 4). In such areas the map-
ping indicates that it is present either as small woodlots
surrounded by farmland, or as larger connected parcels
(at the back end of farms) — especially in the central
and south-eastern hill-lands, where steeper slopes and
shallow soils placed restrictions on forest clearance
in the past.
It is also evident that the Black Spruce forest and the
wet rich woodland, which occur primarily on soils with
poorer drainage (Tables 2 and 4), are segregated geo-
graphically from the upland hardwood forest. These
predominate in areas of lower elevation, notably in parts
of the east and west of the island (Figures 4 and 5).
Though both of these forest-types occur in the same
geographical areas, the TWINSPAN analysis indicated
that they have very different ground and tree vegetation
(Sobey and Glen 2002). They also have very different
soil chemical properties — the wet rich woodland has
soils that are comparatively base-rich and of higher
pH with a lower C/N (carbon-nitrogen) ratio, than the
soils of Black Spruce forest, more acid and base-poor
with a higher C/N ratio. This dissimilarity was also
evident from the fact that there was no overlap in
their graphical distributions in the DECORANA ordi-
nation (Sobey and Glen 2002). Given their similar geo-
graphical distribution on the island, the question is
whether in the mapping we have been able, using tree
and soil criteria alone, to separate the stands of these
two wet forest-types from each other. The differences in
their tree composition parameters, evident in Table 3,
suggest that we have.
Stands of the other two forest-types, the White Spruce
woods and the disturbed forest, have a wider and more
scattered distribution (Figures 6 and 7), occurring
less as larger connected parcels, than as individual small
stands, which is consistent with the fact that their occur-
rence is largely the product of human activity, which
will tend to occur at a scale determined by the own-
ership of blocks of land. At the same time there is a
geographical aspect to their distribution, with the White
Spruce woods prevalent in the central hill-lands and
in the eastern part of the island, its spatial distribution
evidently determined by the geography of field and
farm abandonment, while the disturbed forest is con-
516
THE CANADIAN FIELD-NATURALIST
Vol. 118
TABLE 5. For each soil drainage class, the total area (in hectares) under the three ‘primary’ forest stand-types in 1990, and
the percentage of this area assigned in the computer-sorting to each stand-type is shown.
DRAINAGE CLASS
PRIMARY FOREST Poorly- _ Imperfectly Well-drained Well-drained
STAND-TYPES Organic drained drained (medium textured) (coarse textured) Rapidly-drained
Upland Hardwood Forest 0.88 6.2 12.0 68.7 91.2 64.4
Black Spruce Forest 86.5 35.6 30.7 16.7 6.7 30.6
Wet Rich Woodland 12.6 58.2 57:3 14.6 2a 5.0
Total Hectares 2 620 50 912 18 089 Zl Si 44 865 11 073
centrated largely in the far west and in the east of the
island.
Although a significant and meaningful ecological
picture has emerged from the sorting and mapping, at
the same time it is important to point out some limi-
tations: a basic one is that any sorting of forest stands
into forest-types is a classification procedure, and any
process of classification is a simplification. Compound-
ing this was the fact that the stand sorting was reliant
on the products of three other classification procedures:
TWINSPAN, stand delineation (strictly-speaking not
a classification procedure, but involving demarcation
of the forest area into individual stands), and the soil
series classification for the province. Each of these
three prior procedures will have their own particular
limitations.
It should also be pointed out that although three cen-
turies of forest destruction and exploitation by Euro-
peans have undoubtedly generalized and simplified
the island’s forest cover, the five maps are still a sim-
plification of what was present in 1990. As noted in
Sobey and Glen (2002) there are likely to have been
other forest-types present but so uncommon as not to
have been picked up in the 1991 field survey in suffi-
cient quantity to be recognized as separate types (e.g.,
areas under Hemlock, White Pine, Eastern White Cedar
and White Ash, now occurring as only a few small
stands, but likely to have been more widespread in the
past). Also, each of the five forest-types that has been
recognized may have had sub-types that have been
overlooked: e.g., the TWINSPAN classification sub-
divided the Black Spruce forest plots into wetter and
dryer variants (Sobey 1995), but an attempt in the sort-
ing to separate stands of these on their tree canopy com-
position was not successful. The upland hardwood
may also have variants dominated by particular tree
species. The only solution to this problem of both rare
and more refined forest-types, is firstly to define them,
and then to locate them on the ground and map them
separately.
It should also be noted that the maps produced
present a picture of the forest as it was at one particular
time: in the summer of 1990 at the time of the aerial
photographic survey. But the forests of Prince Edward
Island, like forests the world over, are not fixed and
static. Apart from natural factors, they are subject to the
effects of continual human interference, for example,
clear- and partial-cutting, forest clearance for agricul-
ture, fire, and farm abandonment, as well as the natural
successional processes resulting from these effects.
On the other hand, although the three pre-European
settlement woodland types may vary over time in the
amount and proportion of the island’s area that they
occupy, we should not expect the general pattern of
their distributions to change, related as this is to innate
soil properties. However, the two successional forest-
types (White Spruce woods and disturbed forest) are
likely to be only transitional on a site, and we may
presume that given sufficient time, most of their sites
would develop into one of the primary woodland types.
Mapping the pre-European settlement forest of the
island
Despite the above limitations in the methodology,
it is of interest to generalize the results even further by
considering the potential for extending the mapping
to areas without forest cover in 1990, incidentally, an
aspect of all earlier attempts at mapping the province’s
forests (Stilgenbauer 1929; Halliday 1937; Rowe 1959;
Loucks 1962). Such a mapping may have either of
two objectives: (1) the reconstruction of the type of
forest likely to have occurred before forest clearance,
i.e., the “original-natural” forest sensu Peterken (1996);
and/or (2) the prediction of the type of forest that would
ultimately occur over the whole island if all areas were
allowed to revert naturally to climax forest in the future;
i.e., the “future-natural” forest sensu Peterken (1996).
Either of these objectives involves trying to predict the
climax forest-type on the land area now occupied by
White Spruce woodland and the “disturbed forest’, as
well as the forest cover on land which in 1990 was clear
of forest, i.e., the non-forested area evident in Figure 2,
comprising some 43% of the island’s land area
(Anonymous 1992).
The easiest approach to such a mapping is to take
advantage of the close relationship existing between
natural vegetation and soils, by utilizing data derived
from the comprehensive and fine-scale maps produced
by the Prince Edward Island Soil Survey (MacDougall
et al. 1988). We need first to examine any associations
2004 SOBEY AND GLEN: PRESENT AND PAST FOREST-TYPES OF P.E.I. S197,
FIGURE 8. The conjectured distribution of upland hardwood forest prior to European settlement — based on combining the
distribution of upland hardwood stands in 1990 with that of well-drained soils as mapped by the Soil Survey of
Prince Edward Island (MacDougall et al. 1988).
FIGURE 9. The conjectured distribution of wet rich woodland and Black Spruce forest prior to European settlement — based
on combining the distribution of stands of these two forest-types in 1990 with the distribution of imperfectly- and
poorly-drained soils (excluding stream complexes) as mapped by the Soil Survey of Prince Edward Island (Mac-
Dougall et al. 1988).
518
occurring between the three pre-settlkement forest-
types and the soils of different drainage properties:
Table 5 shows for each drainage class the percentage
of its “primary forest’ component contributed by each
of the three primary forest-types.
From Table 5 it is evident that well-drained coarse-
textured soils (and to a less extent well-drained medium-
textured soils) have a strong association with upland
hardwood forest (some 91% of the well-drained coarse
soils and 69% of the medium soils have such a forest
cover). By contrast, poorly and imperfectly drained
soils are strongly associated with the two other pre-
settlement forest types (wet rich woodland and Black
Spruce forest) — some 94% of poorly-drained and
88% of imperfectly-drained sites carry such forests.
However, although these two “wet” forest-types (as
noted in Sobey and Glen (2002) and above), occupy
soils of markedly differing chemical properties (in
terms of pH, base status and C/N ratios), such chemi-
cal properties were not criteria used to characterize
the soil series in the 1988 Soil Survey, and thus the
soil series maps cannot be used to differentiate these
two forest-types. Then there is the problem presented
by the remaining soil drainage class, rapidly-drained
soils (Table 5): 64% of such soils carry upland hard-
wood forest, but a significant proportion (30%) has a
cover of Black Spruce forest, more likely the dryer vari-
ant of the Black Spruce forest, shown in the TWINSPAN
analysis (Sobey 1995) to have some association with
rapidly-drained soils.
On the basis of the above relationships, Figure 8 is
an attempt to show the approximate distribution of
the pre-settlement upland hardwood forest, and pre-
sumably also the area that is capable of reverting to
such forest in future. The map has been constructed by
taking the 1990 distribution of upland hardwood forest
(Figure 3) and adding to it the area occupied by well-
drained soils (both coarse and medium-textured parent
materials). It is likely that additional areas under rapid-
ly-drained soils, particularly in the south-eastern hill-
lands, would also have carried some form of upland
hardwood forest, but given the present state of our
information, it is not possible at this stage to distinguish
the hardwood-bearing areas of such soils from the
Black Spruce areas.
Figure 9 is an attempt to show the area occupied
before European settlement by the two wet forest-types
(the wet rich woodland and the Black Spruce forest).
It has been constructed by adding to the 1990 distri-
bution of these forest-types (i.e., Figures 4 and 5), the
combined distribution of poorly- and imperfectly-
drained soils. Given the present state of the informa-
tion incorporated within the G.I.S. database for the
province, this is about as far as we can go for wet wood-
land. Distinguishing between these two woodland types
would require data on the chemical properties of the
soils. And, as noted above, Table 5 indicates that Black
Spruce forest (presumably the dryer variant) will have
also occurred on land having rapidly-drained soils. It is
THE CANADIAN FIELD-NATURALIST
Vol. 118
also likely that it is on such soils that the now largely
extirpated pine forests of the island would have occurred
in the past.
The picture that emerges from these maps is of an
island that was mostly covered by upland hardwood
forest, which formed a large continuous block in the
central part of the island, with smaller but significant
blocks in the western and eastern parts. By contrast,
the wetter forest-types occurred at lower elevations in
specific areas in the west and in a more scattered mosaic
pattern in the east. It is thus on these lowland sites
that the boreal element of the island’s forests, in the
form of Black Spruce forest, had a greater occurrence.
Such a division of the landscape, based on soil mois-
ture levels, between the northern hardwood forest and
the boreal forest, appears to be typical in the boreal-
broadleaf ecotone (Pastor and Mladenoff 1992; Scott
1995).
It should be noted that compared with earlier attempts
at mapping the pre-settlement forest (e.g., Stilgenbauer
1929; Loucks 1962) the maps presented here have a
much finer scale of detail in their boundary lines.
Also, the validity of the maps, as showing the forest
distribution before European settlement, can be test-
ed by comparing them with early historical descrip-
tions of the forest, especially from the data contained
in early maps and surveyors’ field notebooks in the
provincial archives. Not only would such a compari-
son allow us to ascertain the forest-types that actually
occurred on many sites before forest clearance, it
may also provide data on the fine-scale differences in
the forests of such sites, in some cases even as to par-
ticular tree species. However this is beyond the scope
of the present study. By contrast, the validity of the
maps as pictures of the “future-natural” forest will only
be testable from what happens if such areas revert to
forest in future.
Acknowledgments
Doug Sobey thanks Professor Gerry McKenna, then
Dean of Science at the University of Ulster, for en-
abling him to take six months leave from University
duties in 1996 so that he could continue his research
into the forests of Prince Edward Island, and the P.E.I.
Department of Agriculture and Forestry, Forestry Divi-
sion, for allowing full access to the 1990-1992 Forest
Inventory data. He also thanks Harry Baglole of the
Institute of Island Studies at the University of Prince
Edward Island for supporting the continuance of the
research associateship which enabled the use of library
facilities at the University. Both authors thank Delmar
Holmstrom of Agriculture Canada, Charlottetown, for
providing advice on the grouping of the soil series
into drainage classes.
Literature Cited
Anonymous. 1992. 1990/1992 Prince Edward Island forest
inventory: Summary. Forestry Branch, P.E.I. Department
of Energy and Forestry, Charlottetown, Prince Edward
Island.
2004
Erskine, D. S. 1960. The plants of Prince Edward Island.
Publication 1088. Canada Department of Agriculture.
Glen, W. M. 1997. Prince Edward Island 1935/1936 forest
cover type mapping. Forestry Division, P.E.I. Department
of Agriculture and Forestry, Charlottetown, Prince Edward
Island.
Halliday, W. E. D. 1937. A forest classification for Canada.
Canada Department of Mines & Resources, Ottawa.
Loucks, O. L. 1962. A forest classification for the Maritime
Provinces. Proceedings of the Nova Scotia Institute of
Science 25: 85-167.
MacDougall, J. L., C. Veer, and F. Wilson. 1988. Soils of
Prince Edward Island. Agriculture Canada, Charlotte-
town, Prince Edward Island.
Pastor, J., and D. J. Mladenoff. 1992. The southern boreal-
northern hardwood border. Pages 216-240 in A systems
analysis of the global boreal forest. Edited by H. H. Shugart,
R. Leemans, and G. B. Bonan. Cambridge University Press,
Cambridge, England.
Peterken, G. F. 1996. Natural woodland — ecology and con-
servation in northern temperate regions. Cambridge Uni-
versity Press, Cambridge, England.
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Rowe, J. S. 1959. Forest regions of Canada. Canada Depart-
ment of Northern Affairs and Natural Resources, Forestry
Branch, Bulletin 123 [Reprinted 1972 with minor revisions
as: Publication No. 1300, Canadian Forestry Service, Depart-
ment of the Environment, Ottawa].
Scott, G. A. J. 1995. Canada’s vegetation — a world perspec-
tive. McGill—Queen’s University, Montreal and Kingston.
Sobey, D. G. 1995. Analysis of the ground flora and other
data collected during the 1991 Prince Edward Island forest
inventory. II. Plant community analysis. Prince Edward
Island Department of Agriculture, Fisheries and Forestry,
Charlottetown, Prince Edward Island.
Sobey, D. G., and W. M. Glen. 2002. The forests of Prince
Edward Island: A classification and ordination using multi-
variate methods. Canadian Field-Naturalist 116: 585-602.
Stilgenbauer, F. A. 1929. The geography of Prince Edward
Island. Ph.D. dissertation, University of Michigan, Ann
Arbor, Michigan.
Watts, S. B. 1983. Forestry handbook for British Columbia
(Fourth edition). University of British Columbia, Vancou-
ver, British Columbia.
Received 20 May 2003
Accepted 4 November 2004
APPENDIX 1. Summary descriptions of the five forest stand-types arising from the computer-
sorting of 82 957 forest stands.
UPLAND HARDWOOD FOREST 16 170 stands (19.5%);
55 043 ha (21.7%)
A stand-type of widespread occurrence on well-drained
soils (77% of its area is on such soils — plus an additional
13% on rapidly-drained soils), especially away from the
coast and further back from roads, in the central and south-
eastern hill-lands, in the north-east peninsula, and in small-
er specific areas in the east and west of the island. 94% of
its area had a forest cover in 1935. The tree canopy is domi-
nated by hardwoods (accounting for 85% of crown closure)
— particularly Red Maple (36%), with a notable contribution
by Sugar Maple (22%), and smaller amounts of Yellow Birch
(8%) and American Beech (2%). There is also a significant
component of White Birch (14%) and Trembling Aspen (5%).
The minority conifer component (15%) consists largely of
Balsam Fir (9%), with some White Spruce (5%). The high
contribution to crown closure by Red Maple, and the pres-
ence of White Birch and Trembling Aspen, are indicative of
a high level of past, and we may presume, continuing, human
disturbance. This stand-type is the direct descendant of the
pre-European settlement upland hardwood forest postulated
by Erskine (1960), though subject to varying levels of past
and current human disturbance.
BLACK SPRUCE FOREST 8 049 stands (9.7%):
33 106 ha (13.1%)
A rather localized stand-type occurring primarily on areas
with poor and imperfect drainage — 78% of its area is on
such soils — especially in specific parts of the west and east
of the island. The tree canopy is dominated by conifers (com-
prising 87% of crown closure), above all Black Spruce (71%)
— with small contributions by Tamarack (9%) and Balsam
Fir (5%). The 13% contributed by hardwoods comes largely
from Red Maple (5%) and Trembling Aspen (5%). Most of
the area (77%) had a forest cover in 1935. This ‘stand-type
corresponds to the pre-settlement lowland Black Spruce
forest of Erskine (1960).
WET RICH WOODLAND 13 863 stands (16.7%);
42 192 ha (16.6%)
A stand-type almost completely confined to areas of poorly-
and imperfectly-drained soils (95% by ground area) espe-
cially in the west of the island, as well as parts of the east.
The tree canopy is dominated by hardwoods (making up
65% of crown closure), but there is also a notable conifer
contribution (35%). The chief hardwood species are Red
Maple (26%), Trembling Aspen (21%) and White Birch
(13%). (White Cedar, American Elm and White Ash are
present at low levels). The main conifers are Black Spruce
(10%), White Spruce (8%), Balsam Fir (6%) and Tamarack
(5%). 76% of its area was under forest cover in 1935. This
stand-type appears to be a derivative of the pre-settlement
lowland Red Maple forest of Erskine (1960) — though with
considerable effects due to cutting and other disturbances.
22 709 stands (27.4%):
57 982 ha (22.9%)
A widely scattered stand-type occurring as small often field-
shaped parcels on well- and rapidly- drained soils (78% by
area is on such soils). It is prevalent in the central hill-lands
and even more towards the east of the island. A high pro-
portion of its area (62%) was cleared land in 1935. The tree
canopy is dominated by a single species, White Spruce, at a
high level of crown closure (68%). The remaining species
contribute only small amounts: Trembling Aspen (8%),
White Birch (6%), Tamarack (6%), Red Maple (5%) and
Balsam Fir (4%). This stand-type corresponds to the succes-
sional “old field” White Spruce woods of Erskine (1960).
WHITE SPRUCE Woops
520
“Disturbed Forest’ 22 166 stands (26.7%):
65 259 ha (25.7%)
This residual stand-type (i.e., that left over after the stands
of the other four types had been selected) is widely scattered,
generally as small individual parcels (rather than large blocks),
especially in the east and west of the island, notably on well-
and rapidly-drained soils (75% by area occurred on such
soils). The tree canopy has a slight predominance of hard-
woods (54%) — the principal species being Red Maple (20%),
THE CANADIAN FIELD-NATURALIST
Vol. 118
Trembling Aspen (19%) and White Birch (13%). Its large
conifer component (46%) is made up of Tamarack (13%),
White Spruce (10%), Balsam Fir (9%), Red Spruce (7%) and
Black Spruce (5%). 33% of its area was cleared land in 1935.
This stand-type does not equate with any of Erskine’s pre-
European forest-types — its species make-up and distribution
suggest rather that it is largely a successional community
heavily affected by past and continuing human exploitation.
Inventaire printanier d’une frayere multispécifique : l’ichtyofaune des
rapides de la riviere Gatineau, Québec
ANNIE Comto!s!, FRANCOIS CHAPLEAU!, CLAUDE B. RENAUD?, HENRI FOURNIER*, BRENT CAMPBELL’,
et RICHARD PARISEAU?
'Département de biologie, Université d’ Ottawa, Ottawa, Ontario KIN 6N5 Canada
Division de la recherche, Musée canadien de la nature, Casier Postal 3443, Succursale D, Ottawa, Ontario K1P 6P4 Canada
3Direction de l’aménagement de la faune de I’ Outaouais, Société de la faune et des parcs du Québec, Gatineau, Québec J8Y 3R7
Canada
Comtois, Annie, Frangois Chapleau, Claude B. Renaud, Henri Fournier, Brent Campbell, et Richard Pariseau. 2004. Inventaire
printanier d’une frayére multispécifique : ichtyofaune des rapides de la riviere Gatineau, Québec. Canadian Field-
Naturalist 118(4): 521-529.
Un inventaire ichtyologique printanier a été réalisé dans la riviere Gatineau, dans le premier rapide a l’amont de son embou-
chure dans la riviere des Outaouais, pour établir la chronoséquence d’utilisation du site par les especes s’y reproduisant, dont trois
espéces de chevaliers. L’échantillonnage des rapides a permis de capturer 2388 poissons répartis en 13 familles et 39 espeéces,
dont six ayant fait ’ objet d’une évaluation par le COSEPAC. Seize espéces étaient en état de se reproduire lors de |’ échantil-
lonnage. Nous avons observé une reproduction plus ou moins simultanée pour le Chevalier blanc et le Chevalier rouge, suivie
de celle du Chevalier de riviére. Egalement, pour ces trois espéces, nous avons observé la capture des miles de stade V plus
tot que les femelles, et nous les retrouvons en plus grand nombre. Ceci pourrait s’expliquer du fait que les males précedent
les femelles sur les frayeéres, que celles-ci sont reconnues pour rester tres peu de temps sur les sites de fraie et qu’un
minimum de deux males par femelle est requis pour la reproduction. Cette étude démontre que les rapides de la riviére
Gatineau doivent étre protégés puisqu’ils sont habités par trois especes qui ont obtenu un statut spécial du COSEPAC
(Menacée: Fouille-roche gris; situation préoccupante : Lamproie du nord et Chevalier de riviere) en plus de constituer une
frayére multispécifique importante.
Mots-clés: Rapides, Riviere Gatineau, Outaouais, Fraie, Chevalier blanc, Moxostoma anisurum, Chevalier de riviére, Moxostoma
carinatum, Chevalier rouge, Moxostoma macrolepidotum, Lamproie du nord, [chthyomyzon fossor, Fouille-roche gris,
Percina copelandi.
A spring survey of fishes was conducted in the Gatineau River (Quebec), in the first rapids upstream of its confluence with
the Ottawa River, to establish the fish spawning chronosequence, especially for the three species of redhorses. The sampling
resulted in the capture of 2388 fish belonging to 13 families and 39 species. Six of these species have been assessed by
COSEWIC. Sixteen species were in spawning readiness. Spawning of the Silver Redhorse and Shorthead Redhorse occurred
first, followed by the River Redhorse. Stage V males of the three redhorse species were captured earlier and in greater numbers
than females. These observations are consistent with other studies which suggest that males precede females to the spawning
grounds, that females remain there for a short period and that a minimum two males per female is required for reproduction.
This study shows that the Gatineau River rapids must be protected because they harbor three species that have obtained a status
by COSEWIC (Threatened: Channel Darter; Special concern: Northern Brook Lamprey and River Redhorse) as well as being
an important multi-species spawning ground.
Key Words: Rapids, Gatineau River, Outaouais, spawning, Silver Redhorse, Moxostoma anisurum, River Redhorse, Moxostoma
carinatum, Shorthead Redhorse, Moxostoma macrolepidotum, Northern Brook Lamprey, Ichthyomyzon fossor,
Channel Darter, Percina copelandi.
Un inventaire réalisé au printemps 1989 a l’aide de
filets de dérive a permis de constater que les rapides
de la riviére Gatineau en aval du barrage hydroélec-
trique de Farmer’s Point (Gatineau, Québec) (Figure 1)
sont utilisés pour la reproduction de I’ Esturgeon jaune,
des Percidae (Sander spp. et Perca flavescens), et des
Catostomidae (Catostomus spp. et Moxostoma spp.)
(Houde et Fournier 1992). Une péche expérimentale
réalisée en 1998 (données non publiées) a révélé la
présence a ce site d’une concentration exceptionnelle
de Chevalier de riviére. Des travaux furent donc entre-
pris en 1999 pour décrire cette population et son utili-
sation du rapide Farmer’s.
L étude ichtyologique de ce secteur de la riviere revét
un intérét particulier parce que le barrage agit comme
barriére au déplacement des poissons vers l’amont. Ceci
pourrait occasionner une concentration de poissons dans
le secteur des rapides en aval du barrage, en particu-
lier au printemps, lors des migrations reproductrices.
Ainsi, le secteur en aval du barrage pourrait étre un site
privilégié pour la reproduction des poissons provenant
des riviéres Gatineau et des Outaouais.
Le but de notre étude est de présenter |’inventaire
printanier des espéces de poissons de ce secteur de la
riviére alors que plusieurs de celles-ci sont normale-
ment en période de fraie. De plus, une attention particu-
521
522
45° 29'21"N
75° 45'17°O
t
po Sz
AUX
THE CANADIAN FIELD-NATURALIST
Vol. 118
45°28'42°N
75°44'13°O
outa
ONTARIO
Figure 1. Site de la riviere Gatineau prés du pont Alonzo-Wright, se trouvant a 5,2 km de la
jonction avec la riviére des Outaouais.
liere sera portée sur la répartition dans le temps de la
reproduction des trois especes de chevalier (Moxos-
toma spp.) qui utilisent le secteur des rapides pour
frayer.
Site d’échantillonnage
La section de la riviére Gatineau (45°29'N,
75°44'O) échantillonnée se trouve entre 6,0 et 5,2 km
de l’embouchure sur la riviere des Outaouais (Figure
1). La zone d’échantillonnage couvre une longueur de
800 m et est délimitée en amont par le pont Alonzo-
Wright et a l’aval par l’extrémité d’une ile localisée prés
de la rive ouest de la riviére. La largeur de la riviére
dans ce secteur varie de 170 m en amont 4 330 m en
aval et couvre une superficie d’environ 22 ha. La pro-
fondeur de |’eau varie de 0,5 a 5 m. Le courant est
particuliérement rapide sur une distance d’environ
400 m a l’aval du pont et la vitesse devient beaucoup
plus lente par la suite alors que la riviére s’élargit et
devient plus profonde.
Dans les eaux rapides, le substrat est composé de
galets, de cailloux et de gros blocs épars dans le centre
de la riviére et de gravier en rive ouest. La rive est a
été largement modifiée par des remblayages et la
construction de quais et murs de soutenement. En
aval, ot la riviére est plus large et le courant plus
lent, le fond est constitué de gravier, de cailloux et de
galets; en rive ouest, le substrat est composé de sable
2004 CoMTOIS ET AL. : L- ICHTYOFAUNE DE LA RIVIERE GATINEAU 523
TABLEAU I. Espéces recensées lors de l’échantillonnage du rapide Farmer’s, riviére Gatineau, au printemps 1999.
Famille Nom latin (Espeéce) Nom commun frangais Nombre
d’individus
Petromyzontidae Ichthyomyzon unicuspis Lamproie argentée 8
Ichthyomyzon fossor Lamproie du nord |
Lampetra appendix Lamproie de I’est 3]
Acipenseridae Acipenser fulvescens Esturgeon jaune 19
Hiodontidae Hiodon tergisus Laquaiche argentée 276
Anguillidae Anguilla rostrata Anguille d’ Amérique |
Cyprinidae Luxilus cornutus Méné a nageoires rouges 4
Notemigonus crysoleucas Méné jaune D)
Notropis atherinoides Méné émeraude 309
Notropis hudsonius Queue a tache noire 2
Rhinichthys cataractae Naseux des rapides |
Semotilus corporalis Ouitouche 52
Catostomidae Carpiodes cyprinus Couette 68
Catostomus commersoni Meunier noir 33
Moxostoma anisurum Chevalier blanc 223
Moxostoma carinatum Chevalier de riviere 270
Moxostoma macrolepidotum Chevalier rouge 254
Ictaluridae Ameiurus nebulosus Barbotte brune 9
Ictalurus punctatus Barbue de riviére ay
Noturus insignis Chat-fou liséré 3
Esocidae Esox lucius Grand brochet l
Esox masquinongy Maskinongé 4
Salmonidae Salmo trutta Truite brune |
Salvelinus namaycush Touladi l
Percopsidae Percopsis omiscomaycus Omisco 5
Centrarchidae Ambloplites rupestris Crapet de roche 116
Lepomis gibbosus Crapet-soleil 9
Lepomis macrochirus Crapet arlequin 4
Micropterus dolomieu Achigan a petite bouche 17
Micropterus salmoides Achigan a grande bouche 1
Pomoxis nigromaculatus Marigane noire 22
Percidae Etheostoma nigrum Raseux-de-terre noir 1
Etheostoma olmstedi Raseux-de-terre gris 12
Perca flavescens Perchaude 79
Percina caprodes Fouille-roche zébré 315
Percina copelandi Fouille-roche gris 76
Sander canadensis Doré noir 16
Sander vitreus Doré jaune 80
Sciaenidae Aplodinotus grunniens Malachigan 5
et de limon alors que la rive est a aussi été largement
modifiée par les activités humaines.
Méthodes
Léchantillonnage s’est effectué a intervalle de 1 a
5 jours, du 29 avril au 23 juin 1999, entre 19:00 h et
01:00 h. Il s’est fait a aide d’un bateau de péche élec-
trique de marque Smith Root 16R. Des voltages de
250 a 1000 V et des ampérages de 0,25 a 3,00 A ont
été utilisés selon la conductivité de l'eau. La péche
débutait a 20 m des piliers du pont Alonzo-Wright.
Une dérive contrélée du bateau était faite sur des tran-
sects de 400 a 800 m le long des rives et au centre de
la riviere. La période de péche active (lorsque le courant
était émis dans |’ eau) variait de 320 4 1732 s. Les pois-
sons capturés étaient déposés dans un vivier installé sur
le pont du bateau. Une fois le vivier rempli, la péche
active était arrétée et les poissons étaient examinés et
relachés, sauf pour quelques spécimens qui ont été
conservés pour des études ultérieures.
Les poissons étaient identifiés, dénombrés et le sexe
ainsi que le stade de reproduction étaient déterminés
lorsque cela était possible. Pour les chevaliers, le sexe
était établi a partir de la présence de tubercules nuptiaux
(Scott et Crossman 1974). Le stade de reproduction
était déterminé par des caractéristiques morphologiques
externes et selon l’index de maturité des gonades de
Nikolsky (1963). Celui-ci classe les stades en six
catégories. Les stades I, II et Ill, ne sont pas
identifiables puisqu ils refletent des états de maturation
des gonades qui ne montrent pas de signes externes.
Le stade IV est caractérisé par l’identification de
gonades fermes et gonflées au toucher de la paroi
abdominale sans expulsion d’ceufs ou de sperme. Le
stade V est identifié lorsqu’il y a expulsion de produits
sexuels par simple pression de l’abdomen.
524
20
—
on
Nombre d'espéces capturées
3
THE CANADIAN FIELD-NATURALIST
0 0,0
Vol. 118
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29-avr 3-mai 6-mai 10-mai 13-mai 17-mai 20-mai 25-mai 27-mai 31-mai 3-juin 7-juin 10-juin 14-juin 16-juin 17-juin 21-juin 23-juin
Date
FicuRE 2. Evolution temporelle du nombre d’espéces capturées et de la température de l’eau (m) au rapide Farmer’s,
printemps 1999.
Un poisson au stade VI a un abdomen relativement
flasque et sans expulsion massive de produits sexuels
par pression abdominale.
L’échantillonnage ciblant surtout les chevaliers, |’a-
bondance des espéces de petite taille est probablement
une sous-estimation de leur présence dans le milieu.
Résultats
Familles et espéces capturées
L’échantillonnage des rapides de la riviére Gatineau
a permis de capturer 2388 poissons en 12 heures de
péche active réparties sur 18 jours entre le 29 avril et
le 23 juin 1999. Les captures se répartissent en 13 fa-
milles et 39 espéces (Tableau 1). Les Percidae dominent
pour le nombre d’espéces capturées (sept espéces).
Les Cyprinidae et les Centrarchidae sont représentés
par six espéces chacune. Les Catostomidae dominent
pour le nombre de spécimens (848), les chevaliers
constituant 88% des captures. Un seul spécimen des
Anguillidae (Anguilla rostrata) a été capturé (Tableau
1). D’ailleurs, un seul spécimen a été capturé pour huit
especes (Tableau 1) alors que plus de 300 spécimens
ont été capturés pour le Méné émeraude (309) et le
Fouille-roche zébré (315).
Six des espéces capturées ont fait l’objet d’une
évaluation par le Comité sur la situation des espéces
en péril au Canada (COSEPAC 2003) : l’Esturgeon
jaune (non en péril; 1986), le Chevalier de riviére (situ-
ation préoccupante; 1987), le Chat-fou liséré (menacé;
1989 et données insuffisantes lors de la révision de
2002), la Lamproie du nord (situation préoccupante;
1991), le Fouille-roche gris (menacé; 1993, 2002) et
le Raseux-de-terre gris (non en péril; 1993). Deux de
ces especes, le Chevalier de riviére et le Fouille-roche
gris ont été capturés en grand nombre dans la riviere
Gatineau, soit 270 et 76 individus respectivement
(Tableau 1).
Comme nous pouvons le constater a la Figure 2, le
plus petit nombre d’espéces capturées a été de dix
lors de la premiere sortie, le 29 avril. Il a augmenté
graduellement pour atteindre un maximum de 21 es-
peces le 27 mai. Par la suite, le nombre a diminué, vari-
ant de 12 a 17 espéces par sortie.
Reproduction
Des individus de 16 des espéces capturées étaient
au stade V du cycle de reproduction et semblent donc
y avoir frayé (Tableau 2). Pour plusieurs de ces espéces,
nos captures permettent de délimiter une période de
reproduction probable et les températures auxquelles
elle se serait produite. Pour quelques espéces, des in-
dividus en état de fraie (stade V) étaient présents dés
la premiere journée d’échantillonnage ou encore pré-
sents la derniére journée. Dans ces cas, il est possible
que la période de reproduction s’étende au-dela de la
période d’échantillonnage. Des individus des deux
sexes de tous les stades avancés de développement des
gonades (stades IV, V, VI) ont été observés pour cing
especes seulement : le Chevalier blanc (Moxostoma
anisurum), le Chevalier de riviere (M. carinatum), le
Chevalier rouge (M. macrolepidotum), la Couette (Car-
piodes cyprinus) et la Laquaiche argentée (Hiodon
tergisus).
Reproduction des trois espéces de chevalier
L’abondance des captures permet d’établir la chro-
noséquence des périodes de reproduction des trois
especes de chevaliers dans la riviére Gatineau (Figures
3 et 4). Pour toutes les espéces, des spécimens de
2004
COMTOIS ET AL. : L;: ICHTYOFAUNE DE LA RIVIERE GATINEAU
Nn
i)
Nn
TABLEAU 2. Période de capture d’individus en fraie (stade V), selon le sexe et ’espece, au rapide Farmer’s, printemps 1999.
Espéce Nombre d’individus
fe) Q
Ambloplites rupestris 2 3
Aplodinotus grunniens | |
Carpiodes cyprinus 35 7
Catostomus commersoni 8 5
Hiodon tergisus 198 2
Ichthyomyzon fossor 0 |
Ichthyomyzon unicuspis 2
Lampetra appendix 5 3
Moxostoma anisurum 89 6
Moxostoma carinatum 96 16
Moxostoma macrolepidotum 67 7
Percina caprodes 10 0
Percina copelandi d/ 1
Percopsis omiscomaycus 0 2
Pomoxis nigromaculatus 3 3
1 1
Période de capture Température de
eau (°C)!
27 mai — 10 juin 13,5 — 18,5
3— 6 mai 9,0 — 10,0
29 avril — 3 juin 7,0 — 18,0
29 avril — 27 mai 7,0 — 13,5
10 mai — 23 juin 12,5 — 19,0
23 juin 19,0
13 mai — 23 juin 12,5 — 19,0
3 — 20 mai 9,0 — 14,0
3 — 31 mai 9,0 — 17,0
10 mai — 23 juin 12,5 — 19,0
29 avril — 21 juin 7,0 — 19,0
6 — 25 mai 10,0 — 14,0
20 mai — 21 juin 14,0 — 19,0
6 mai 10,0
3 — 13 mai 9,0 — 12,5
3 — 20 mai 9,0 — 14,0
Semotilus corporalis
' Température de l’eau au début et a la fin de la période de capture.
stade de maturité IV étaient présents au début de la
période d’échantillonnage, le 29 avril, sauf pour les
femelles du Chevalier rouge et les males du Cheva-
lier de riviere. Pour ceux-ci, les individus au stade [V
sont apparus le 3 et le 6 mai respectivement (Figure
3). Des males de stade IV ont été capturés jusqu’au
17 mai dans le cas du Chevalier rouge, jusqu’au 27
mai pour le Chevalier blanc et jusqu’au 7 juin pour le
Chevalier de riviere. Les dernieres femelles de stade
IV de Chevaliers rouge et blanc ont été capturées le
17 mai, alors qu’elles ont été présentes sur le site
jusqu’au 17 juin pour le Chevalier de riviere.
(8 enna
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26-avr 1-mai 6-mai 11-mai 16-mai 21-mai 26-mai 31-mai 5-juin 10-juin 15-juin 20-juin 25-juin
Date
FIGURE 3. Période de reproduction des trois espéces de chevalier selon l’index de maturité de Nikolsky (1963) dans la riviére
Gatineau, au printemps 1999. Le carré représente le Chevalier blanc (Mi), le losange, le Chevalier de riviére (@) et le
triangle, le Chevalier rouge (a). Les symboles pleins désignent les femelles tandis que les vides représentent les males.
Le nombre d’individus capturés est indiqué entre parenthéses. Les lignes verticales correspondent au début et a la fin
de la période d’échantillonnage. Le pointillé 4 l’extérieur de la période d’échantillonnage signifie que des individus
appartenant aux stades indiqués ont pu se retrouver sur la frayére avant ou apres cette période.
526
Des males au stade V sont apparus dans les cap-
tures le 3 mai pour le Chevalier blanc et le 10 mai
pour le Chevalier de riviére, 4 une température de 9,0
et 12,5 °C respectivement. Les males Chevalier rouge
de ce stade de maturité étaient présents des le début de
l’échantillonnage. Les femelles de stade V sont appa-
rues le 10 mai pour le Chevalier blanc et le Chevalier
rouge (12,5 °C) et le 3 juin pour le Chevalier de rivi-
ére (18,0 °C). Les captures de males au stade V sont
toujours nettement plus abondantes que celles des fe-
melles. Aucune femelle de stade V n’a été capturée
aprés le 20 mai dans le cas du Chevalier blanc (14,0 °C)
et le 7 juin dans le cas du Chevalier rouge (18,5 °C)
alors qu’elles étaient toujours présentes a la fin de I’é-
chantillonnage, le 23 juin, dans le cas du Chevalier de
riviere, 4 une température de 19,0 °C.
Des femelles au stade VI apparaissent dans les cap-
tures le 17 mai pour le Chevalier blanc et le Chevalier
rouge (12,5 °C) alors qu’elles sont présentes pour le
Chevalier de riviére 4 compter du 10 juin (18,5 °C).
Les dernieres femelles de stade VI ont été capturées
le 31 mai pour le Chevalier blanc (17,0 °C) et le 17 juin
pour le Chevalier rouge (19,0 °C), alors qu’elles étaient
toujours présentes a la derniere date d’échantillonnage
pour le Chevalier de riviere (19,0 °C).
Discussion
Si l’on ajoute aux 16 espéces citées dans le Tableau
2 celles rapportées par Houde et Fournier (1992), il est
probable qu’environ 20 espéces se reproduisent dans le
rapide Farmer’s. D’autres espéces capturées pourraient
potentiellement utiliser le secteur échantillonné de la
riviere Gatineau pour frayer (Scott et Crossman 1974;
Bernatchez et Giroux 2000) : le Méné émeraude, le
Naseux des rapides, et possiblement le Méné a nage-
oires rouges et le Raseux-de-terre gris. Toutefois, la
période d’échantillonnage ne correspondait pas a la
période de fraie pour certaines espéces (e.g. Méné
émeraude) alors que trop peu de spécimens ont été cap-
turés pour d’autres afin de déterminer |’ état reproduc-
tif (e.g. Naseux des rapides).
La frayére multispécifique des rapides de la riviére
Gatineau compte autant d’espéces que celle de la
riviere aux Pins, a Boucherville (Massé et al. 1988).
Les deux frayeres ont toutefois des caractéristiques trés
différentes; la frayére de la riviére aux Pins constitue
un habitat d’eau calme utilisé particuliérement par
les espéces phytophyles. D’ailleurs, seulement trois
especes sont communes aux deux frayéres : la Oui-
touche, le Meunier noir et le Crapet de roche. Dans
les eaux vives, Massé et al. (1988) mentionnent cing
autres frayéres entre Carillon (riviére des Outaouais)
et la riviere des Prairies qui comptent entre 8 et 27
especes reproductrices. La riviére Gatineau se situe
donc dans le milieu du peloton quant a son utilisation
multispécifique.
Des femelles en état de fraie de Chevaliers rouge et
blanc sont apparues sur le site en méme temps le 10
THE CANADIAN FIELD-NATURALIST
Vol. 118
mai. Elles y ont été capturées pendant une période de
10 jours dans le cas du Chevalier blanc et de 28 jours
dans le cas du Chevalier rouge. La fraie des deux es-
peces a donc été en partie simultanée (Figures 3 et 4).
Contrairement a nos résultats, Curry et Spacie (1984)
ont noté que le Chevalier blanc a amorcé la reproduc-
tion une semaine avant le Chevalier rouge dans le Deer
Creek, Indiana, en 1979. Toutefois, Mongeau et al.
(1986, 1992) ont également observé une simultanéité
de la reproduction du Chevalier blanc et du Chevalier
rouge dans leur étude sur la riviere Richelieu. En effet,
ils ont observé que la reproduction de ces deux espéces
débutait 4 la mi-mai pour se terminer a la mi-juin. Nos
données semblent tendre vers le méme résultat puisque
des individus de stade VI ont été capturés du 17 mai
au 21 juin pour les deux espéces (Figure 3). Mongeau
et al. (1986, 1992) ont noté que le Chevalier rouge et
le Chevalier blanc commengaient a déposer des ceufs
a une température de 10,7 °C. Meyer (1962) a indiqué
que la température a laquelle la reproduction débutait
pour le Chevalier rouge et le Chevalier blanc sur la
riviere Des Moines, en Iowa, était 11,1°C et 13,3°C
respectivement. Par contre, Burr et Morris (1977) ont
observé une température de 16,0°C pour la reproduc-
tion du Chevalier rouge dans le ruisseau Big Rock,
en Illinois et Hackney et al. (1970), une température
de 14,4°C pour le Chevalier blanc dans la riviere Flint,
en Alabama. La Figure 2 montre que la température
de l’eau au 17 mai était a 12,5°C, ce qui correspond
relativement bien aux données de Meyer (1962) et de
Mongeau et al. (1986, 1992).
Burr et Morris (1977) indiquent que plusieurs es-
peces de chevaliers pourraient possiblement frayer a
des périodes et des températures similaires et sur des
substrats comparables. II peut toutefois y avoir de la
ségrégation spatiale entre les espéces. En effet, le Che-
valier rouge et le Chevalier doré (Moxostoma erythru-
rum) ont été observés en train de frayer simultanément
au méme site, mais le Chevalier doré avait une dis-
tribution plus étendue en amont, ce qui lui fournissait
un habitat non utilisé par le Chevalier rouge (Curry et
Spacie 1984). Par ailleurs, une étude comparant la fraie
chez le Chevalier doré et le Chevalier noir (Moxostoma
duquesnei) a démontré que ces deux espéces se repro-
duisaient au méme moment et dans la méme section
du Stony Creek, en Illinois (Kwak et Skelly 1992).
Les auteurs mentionnent toutefois qu’il existe des dif-
férences dans le choix des microhabitats de fraie et dans
le comportement reproducteur et que celles-ci servi-
raient possiblement a réduire la compétition entre ces
espeéces. Bien qu’une étude plus approfondie de l’habi-
tat et du comportement reproductif soit nécessaire, il
est possible qu’une ségrégation spatiale et/ou compor-
tementale se produise pour le Chevalier blanc et le
Chevalier rouge dans la riviére Gatineau.
Des femelles de stade V du Chevalier de rivieére ont
été capturées pour la premiere fois le 3 juin et ce,
jusqu’a la derniére journée d’échantillonnage. Sa re-
2004. COMTOIS ET AL. : L;- ICHTYOFAUNE DE LA RIVIERE GATINEAU ayy
35 +
Chevalier blanc
| Femelle: n= 51
30 7 Male: n= 94
25 Individus non sexés: n= 78
—
nn
a
i Femelle
[_] Male
Ue eee
25 7 Chevalier de riviére
Femelle: n = 110
Male: n = 133
w”
@
ie
= 20
e | Individus non sexés: n = 27
a) j
3 15
2
GT =
= 1055;
5 i
§
£ Sy
6 ;
Zz ]
0
20 7 Chevalier rouge
Femelle: n= 70
Male: n= 108
15 - Individus non sexés: n= 76
| 1
10
| ae
Oo on
cs eee
peipiccos nace
DS rae are ae)
| Sea
=
i
i
ke
juin
[Cl |e ee]
a Ln lan
=> OCG G cs eS - SS SS Ss =
gee ee eo Ssocas
is
A Se SAAN: SAN
FiGurE 4. Nombre d’individus capturés par jour selon le sexe pour les trois espéces de chevalier, rivi¢re Gatineau, printemps,
1999.
528
production débute donc plus tard, soit autour du 10
juin (Figure 3) a une température de 18,5 °C. Mongeau
et al. (1986, 1992) ont obtenu plus ou moins les mémes
résultats puisqu’ils indiquent que le Chevalier de riviere
amorce la fraie autour de Ja deuxi¢me semaine de juin
a une température de 17,7 °C, une conclusion fondée
sur la capture de deux spécimens au stade VI. Hackney
et al. (1970) mentionnent également que le Chevalier de
riviére a une reproduction tardive vis-a-vis de celle
du Chevalier blanc dans la riviére Duck, au Tennessee.
La différence entre la période de reproduction de cette
espece et celles des deux autres chevaliers présents
dans les rapides de la riviére Gatineau est probablement
due au fait que le Chevalier de riviére nécessite une
température de |’eau plus élevée pour débuter sa
reproduction.
Par ailleurs, pour ces trois espéces, nous observons
des males de stade V a une date plus hative que les
femelles au méme stade (Figure 3). Ceci s’explique par le
fait que les males du Chevalier blanc, du Chevalier rouge
et du Chevalier de riviere précédent les femelles sur
les frayeres (Meyer 1962; Hackney et al. 1968, 1970;
Scott et Crossman 1974). Ce phénoméne est d’ailleurs
observé chez d’autres chevaliers et chez plusieurs
autres Catostomidae (Meyer 1962; Scott et Crossman
1974; Jenkins et Jenkins 1980; Page et Johnston 1990;
Kwak et Skelly 1992; Cooke et Bunt 1999),
Dans nos captures, le nombre de males de stade V est
plus grand que celui de femelles pour les trois espéces
de chevalier. Ceci n’est pas inhabituel. Hackney et al.
(1970) ont observé un rapport des sexes de 4 males : |
femelle sur une frayére de Chevalier blanc. De plus,
Meyer (1962) note que chez les Chevaliers rouge et
blanc, les femelles demeurent sur les sites de fraie
beaucoup moins longtemps que les males. La fraie chez
les chevaliers, et chez la plupart des Catostomidae, se
fait généralement en présence de deux males et d’une
femelle (Hackney et al. 1968; Burr et Morris 1977;
Jenkins et Jenkins 1980; Page et Johnston 1990; Kwak
et Skelly 1992; Cooke et Bunt 1999), d’ot la nécessité
d’une présence en plus grand nombre de males sur la
frayére tel que nous l’avons observé pour chacune des
trois espéces présentes au rapide Farmer’s.
Nos travaux ont permis de découvrir le site de re-
production de l’une des plus importantes populations
de Chevalier de riviére. Un échantillonnage sur quel-
ques années serait nécessaire pour préciser la chrono-
séquence de fraie de cette espéce et des autres che-
valiers utilisant le site. Un échantillonnage sur une
plus longue période aurait probablement pu permettre
de confirmer la fraie au rapide Farmer’s d’un plus grand
nombre d’espéces.
Cette étude démontre donc que le rapide Farmer’s
constitue une frayére multispécifique importante tant
par le nombre d’espéces qui s’y reproduisent que par la
présence d’espéces évaluées par le COSEPAC comme
ayant une situation préoccupante (Lamproie du nord,
Chevalier de riviére) ou méme menacée (Fouille-roche
gris). Localisés en plein coeur d’une zone urbaine, ces
THE CANADIAN FIELD-NATURALIST
Vol. 118
rapides ont une grande valeur écologique et doivent
étre protégés.
Remerciements
Nous remercions Anne Phelps, Annie-Chantal Gui-
bord et Kevin Moon pour leur aide sur le terrain. Cette
recherche a été partiellement subventionnée par une
subvention a la découverte du Conseil de recherches en
sciences naturelles et en genie du Canada (CRSNG)
[Frangois Chapleau].
Littérature Citée
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douce du Québec et, leur répartition dans l’Est du
Canada. Broquet, Boucherville, Québec. 350 pages.
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Shorthead Redhorse, Moxostoma macrolepidotum, in Big
Rock Creek, Illinois. Transactions of the American Fish-
eries Society 106: 80-82.
Cooke, S. J., et C. M. Bunt. 1999. Spawning and reproduc-
tive biology of the Greater Redhorse, Moxostoma valen-
ciennesi, in the Grand River, Ontario. Canadian Field-
Naturalist 113: 497-502.
COSEPAC. 2003. Résultats des évaluations du COSEPAC,
novembre 2003. Comité sur la situation des espéces en
péril au Canada, Ottawa, Ontario. 54 pages.
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habitat by spawning catostomids. American Midland Nat-
uralist 111: 267-279.
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tory study of the River Redhorse, Moxostoma carinatum
(Cope), in the Cahaba River, Alabama, with notes on the
management of the species as a sport fish. Proceedings of
the Annual Conference of the Southeastern Association
of Game and Fish Commissioners 21: 324-332.
Hackney, P. A., G. R. Hooper, et J. F. Webb. 1970. Spawn-
ing behavior, age and growth, and sport fishery for the
Silver Redhorse, Moxostoma anisurum (Rafinesque), in the
Flint River, Alabama. Proceedings of the Twenty-Fourth
Annual Conference, Southeastern Association of Game
and Fish Commissioners 1970: 569-576.
Houde, P. et H. Fournier. 1992. Travaux de recherche de
frayéres dans la riviére des Outaouais et ses principaux
affluents au cours du printemps 1989. Ministére du Loisir,
de la Chasse et de la Péche, Service de l’aménagement et
de l’exploitation de la faune, Hull. 28 pages.
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of the Greater Redhorse, Moxostoma valenciennesi, in the
Thousand Islands region. Canadian Field-Naturalist 94:
426-430.
Kwak, T. J., et T. M. Skelly. 1992. Spawning habitat, behav-
ior, and morphology as isolating mechanisms of the Gol-
den Redhorse, Moxostoma erythrurum, and the Black Red-
horse, M. duquesnei, two syntopic fishes. Environmental
Biology of Fishes 34: 127-137.
Massé, G., R. Fortin, P. Dumont, et J. Ferraris. 1988. Etude
et aménagement de la frayere multispécifique de la rivi-
ére aux Pins et dynamique de la population de Grand bro-
chet, Esox lucius L., du fleuve Saint-Laurent, Boucher-
ville, Québec. Ministére du Loisir, de la Chasse et de la
Péche, Service de l’aménagement et de l’exploitation de
la faune, Montréal, Québec, Rapport technique 06-40.
224 pages.
2004
Meyer, W. H. 1962. Life history of three species of redhorse
(Moxostoma) in the Des Moines River, Iowa. Transactions
of the American Fisheries Society 91: 412-419.
Mongeau, J.-R., P. Dumont, et L. Cloutier. 1986. La biolo-
gie du Suceur cuivré, Moxostoma hubbsi, une espeéce rare
et endémique a la région de Montréal, Québec, Canada.
Ministére du Loisir, de la Chasse et de la Péche, Service
de l’aménagement et de l’exploitation de la faune,
Montréal, Québec, Rapport technique 06-39. 137 pages.
Mongeau, J.-R., P. Dumont, et L. Cloutier. 1992. La biolo-
gie du Suceur cuivré (Moxostoma hubbsi) comparée a celle
de quatre autres espéces de Moxostoma (M. anisurum, M.
carinatum, M. macrolepidotum, M. valenciennesi). Revue
canadienne de zoologie 70: 1354-1363.
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529
Nikolsky, G. V. 1963. The ecology of fishes. Traduit par L.
Birkett. Academic Press, New York. 352 pages.
Page, L. M., et C. E. Johnston. 1990. Spawning in the Creek
Chubsucker, Erimyzon oblongus, with a review of spawn-
ing behavior in suckers (Catostomidae). Environmental
Biology of Fishes 27: 265-272.
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du Canada. Office des recherches sur les pécheries du
Canada Bulletin 184. 1026 pages.
Received 3 October 2003
Accepted 21 June 2004
Moths and Butterflies (Lepidoptera) of the Boreal Mixedwood Forest
near Lac La Biche, Alberta, Including New Provincial Records
Grea R. Pout!, Davip W. LANGor!, JEAN-FRANCOIS LANDRY’, and JOHN R. SPENCE?
' Natural Resources Canada, Canadian Forest Service, 5320 - 122 St., Edmonton, Alberta T6H 3S5 Canada
> Agriculture and Agrifood Canada, Eastern Cereal and Oilseed Research Centre, 960 Carling Avenue, Ottawa, Ontario
K1A 0C6 Canada
> Department of Renewable Resources, University of Alberta, Edmonton, Alberta T6G 2H1 Canada
Pohl, Greg R., David W. Langor, Jean-Francois Landry, and John R. Spence. 2004. Moths and Butterflies (Lepidoptera) of
the boreal mixedwood forest near Lac La Biche, Alberta, including new provincial records. Canadian Field-Naturalist
118(4): 530-549.
Lepidoptera were collected, primarily via UV light trap, for three seasons in the boreal mixedwood forest near Lac La
Biche, Alberta. A total of 11 111 specimens were collected, representing 41 families and 438 species. A species list with
flight times is presented. The total Lepidoptera community was estimated to be 546 +23.34 species. Abundance and species
richness peaked in late July. Thirty-five species constitute new records for Alberta, while one species, Acanthopteroctetes
bimaculata, is a new record for Canada, and the first record of the family Acanthopteroctetidae in Canada.
Key Words: Moths, butterflies, Lepidoptera, Lac La Biche, Alberta, flight times, Acanthopteroctetes bimaculata, new to
Canada.
Alberta is blessed with an abundance and variety
of forested lands. A large portion of the province is
covered by the boreal mixedwood (Figure |) domi-
nated by Trembling Aspen (Populus tremuloides),
Balsam Poplar (P. balsamifera), and White Spruce
(Picea glauca) and containing lesser amounts of White
Birch (Betula papyrifera), Balsam Fir (Abies bal-
samea), and other species (Beckingham and Archibald
1996). Over the last 15 years Trembling Aspen has
increased greatly in value as a commercial tree species
and there has been a large increase in forestry activity
centered on this resource. A large portion of Alberta’s
aspen mixedwood forest is now scheduled for har-
vesting over the next 30-40 years (Pratt and Urquhart
1994). It is a major concern that our knowledge of these
forests is relatively poor and there is little empirical
basis for predicting the impacts of harvesting and other
development on non-timber values such as biodiversity.
In an effort to obtain baseline data for assessing
impacts of forestry practices on biodiversity, and to
determine whether old aspen stands in mixedwood
forests contain unique species, a multi-agency team
of scientists studied the structure and composition of
biotic assemblages in aspen-dominated forests of
various ages in the vicinity of Lac La Biche, Alberta,
between 1993 and 1995. This work is among the most
comprehensive biotic inventories in aspen forests in
the province. Lists of plants, birds, amphibians, and
mammals have been published by Stelfox (1995) and
those of ground-dwelling beetles and dead wood-
inhabiting beetles by Spence et al. (1997) and Ham-
mond (1997), respectively. As part of that study, but-
terflies and moths were also sampled. This represents
the first concerted effort to inventory Lepidoptera,
especially moths, in aspen forests in western Canada.
Lepidoptera constitute a major component of boreal
forest biodiversity (Danks and Foottit 1989), and are
important herbivores and pollinators (Scoble 1992).
The abundance of new provincial records among micro-
moths (defined here as the primitive and monotrysian
groups, and the lower ditrysian superfamilies up to
and including the Pyraloidea and Thyridoidea sensu
Kristensen 1999) indicates how poorly sampled these
groups have been. The attached checklist and flight
times provide baseline information for comparison to
other studies and to aid in future research.
Materials and Methods
The study area (Figure 1) is located in Lakeland
Provincial Park near Touchwood Lake, east of Lac
La Biche (54°51'N, 111°27'W) in the Central Mixed-
wood subregion of the Boreal Forest Natural Region
(Beckingham and Archibald 1996). Lepidoptera were
sampled in two stands: a 65-year-old (“mature”) stand
of 269 Ha, containing 83% cover of Trembling Aspen,
15% Balsam Poplar, 2% willow (Salix spp.), and 1%
White Birch, and a stand over 130 years old (“old”)
of 148 Ha, containing 54% cover of Trembling Aspen,
32% White Birch, 11% Balsam Poplar, and 3% willow.
An inventory of vascular plants found around these
study sites is included in the lists published by Stelfox
(1995). Both stands were of fire origin, and were largely
undisturbed by humans. The mature stand is consid-
ered to be of rotation age and the old stand is much
530
2004. POHL, LANGOR, LANDRY, and SPENCE:
‘ ae ies - : e
cat Edmonton waa
ALBERTA
100 km
boreal
mixedwood
Ficure |. Extent of the boreal mixed wood ecoregion in
Alberta and location of the study area.
older than the planned stand rotation age (60-70 years)
for Alberta aspen forests. A comparison between these
two stands, based on the light trap catches of Lepi-
doptera described here, has been done elsewhere (Pohl
et al. 2004).
Two 30 watt UV traps were run in each stand, from
dusk to dawn for one night approximately every two
weeks, from 16 June to 16 September in 1993, 3 May
TABLE |. Abundance and diversity of three groups of Lepi-
doptera collected near Touchwood Lake, Alberta. Butterflies
include the superfamilies Hesperioidea and Papilionoidea;
macro-moths include the superfamilies Lasiocampoidea,
Bombycoidea, Drepanoidea, Geometroidea, and Noctuoidea;
micro-moths comprise all other superfamilies.
Group Number of Specimens Number of Species
(Proportion) (Proportion)
micro-moths 3897 (0350) 201 (0.470)
macro-moths 7163 (0.643) 229 (0.523)
butterflies 51 (0.005) 8 (0.018)
total TOE a GL 438
LEPIDOPTERA NEAR LAC LA BICHE
to 5 October in 1994, and 28 May to 28 August in
1995. Traps were hung at approximately 1.6 m from
the ground, and activated from dusk until dawn. These
samples were augmented by periodic hand collecting
at portable UV lights, and a small amount of net col-
lecting of day-flying species. Specimens were identi-
fied using a wide array of taxonomic publications, and
by comparing to specimens in the Canadian Forest
Service’s Northern Forestry Centre Research Collec-
tion (NFRC) in Edmonton, Alberta, and the Canadian
National Collection (CNC) in Ottawa, Ontario. Vouch-
er specimens have been deposited at the NFRC and
CNC.
To obtain an estimate of the total size of the Lepi-
doptera community in the study area, a Chao-1 estimate
of diversity (Chao and Lee 1992) was calculated as
described by Colwell and Coddington (1994).
Results
A total of 11 111 specimens were collected, repre-
senting 41 families and 438 species (Table 1). A list of
all species collected appears in Table 2. Some species,
particularly micro-moths, are identified here merely as
morphospecies, reflecting the lack of knowledge of
the group, and the difficulty in making species identi-
fications. Examples of some of the micro-moth species
collected appear in Figure 2; some of the macro-moths
are illustrated in Figures 3 and 4. The Chao-1 calcula-
tion estimated the total size of the Lepidoptera com-
munity in the study area to be 546 + 23.34.
The 1994 data is examined in detail here, since it
was the most extensively sampled year and there were
no trap failures. In 1994, both abundance (Figure 5)
and species richness (Figure 6) peaked dramatically
in late July. A major flush of Noctuidae occurred in
late July, with the highest species richness occurring
throughout July and into early August. There were
modest peaks of noctuid species that overwinter as
adults, in early May and mid-September. The Geo-
metridae and other macro-moths peaked slightly earlier
than the Noctuidae, exhibiting maximum abundance
in early July, and the greatest richness from mid-June
to late July. The abundance of micro-moths peaked in
late July, although most of this dramatic peak was a
single species, Scoparia biplagialis, with 846 speci-
mens. The greatest micro-moth richness occurred
throughout July. More modest peaks in micro-moth
abundance and richness occurred in mid-June and
mid-September.
Discussion
This study likely did not collect all the species pres-
ent in the study area; the Chao-1 estimator suggests
that approximately 110 species were missed. Many
of these are undoubtedly species that are not easily
sampled via light traps. For example, the amount of
effort spent collecting butterflies and day-flying moths
was minimal and many of these taxa were likely missed.
THE CANADIAN FIELD-NATURALIST Vol. 118
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2004
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Ajng prtu — oung oR] ¢ ysnouunqojy Djjasoaavsod Déoydoajoy
Ayn piu — sung ae] p (ysnouunqoy\) pjjaiuojduos vioydoajoy
Ajng oye] — oung pri v yoseir g apyofiujp pioydoajoy
Ang ae] v susWa[D pyayofysso0o vpsoydoajoy
oung aje] — oun pr , ysnouunqgsjN pyjaxajduisiad pioydoajoy
Ayn aye] — oung prur Suda) pyjaiunaid paoydoajog aeplioydoajod
Ajng aye] — Apne pr (YjIOMPH) psnsuvavid DAPIYIDAIDG aeplipayov.ye gq
Ajng a1] (WIRYSUIS[eA ) DIJAPVAOJOI XYOg aeplioydosa9
oune Aye ¢ (sdaquuiey)) DIJAIUIPIAANI DUIDPOISY]G
APY 21°] I ;satoeds nys1yoo]y
Ajne oe] Z josuq Dyandvoig]V VISIYIVD)A
sn3ny Ayia — Ang prur Z uneig DI dwapv VISIYIP] A
snsny avy — ysnsny Ajrea (yosng) DIJA[NIAq SATIN
Avy] Pru WRYSUISTeAA pypusoul sidoosonuas
ounr ae] — oung Ajiea (WIBYSUIS|eAA ) D]JAUI]ID VIQUvsIDGLg
snsny Aiea — Avy pr (1O]]9Z, 29 S1urlaq) DyJauoyiu1d sapoivssaidaq
ysnsny Aye (yosng) DIJapijas XiMajdouosy oepysiyory
Ajng pru Jouqny Dyjayofiunsd DIaUuony ovpinouody]
Ayng aye] (snovuury) DIJISO]AX D]JAIN]d
ABI 2}P] (WIeYSUIS|eA ) DIANALAJUI S1JSOUOS1YY aepl{foand
ysnsny Ie] (WIeYSUIS|eA ) Dijasafuyuap vydojosdx
ysnsny Ajreo — Ane pr (WuvYsUIS[e ) Dyjaispuvo pydojosdx oeprydojosd x,
polag 1sl4 JoyINYV satoads snuay Ajrure
‘Apnjs IwaK-ddIY) BY) JOAO IPRUI SUOTDET[OI UO pase SI POLlad IYSILf “ISIPIOYS (CQ6T) ‘Te 19 SOSPOH YI SMOTIOF
exe] Joysry uryytM douanbas satoadg ‘(6GG]) UASUDISLLY JO JY) SMOT[OJ UONROYTISsL[O JOYSIY “vIAQ[Y ‘ayeT] poomyYonoy, 1eau pajda]]oo sardads vsajdopideyT jo isvqJ (panuyuor) *7 AAV,
THE CANADIAN FIELD-NATURALIST Vol. 118
534
ysndny Ayiwo — Apne aye] (pyeus.s) DUDIADA SIAaJIV
oune Ape ([919[D) DUDIBO] S1UAJIY
Jaquuajdag piu — jsnsny Aj.ira YOpwdy DIUUDJIAG S1AAJIV.
sung Ape (uosuIqoy) DUDA) SIMAJIV
Joquiajdag piu — jsnsny 9)e| (snaevuul']) DUDIAA]JVYIS SUA]IV
oung prul (ysnouunqgoj\) DUDS AGAOL SIAAJIV
Avy oyey — Avyy pr IYSMOZEY 2 Ye DILOJDS1]GO S1AaJIV
Alne ae] (SUSI) DUDUOIIG]D S1AaJIV IVUIOLIIO], — IPPIOLNAO],
Ayn pr ([99q) ADIUIGOL SNJSAXOUOL
Ajng aye] — ounr ye] (ADT) yndod snssooy
ysnsny Apiwo — oune aye] (aouqur'T) SISUALIJUAI SNSSOIY aepissod
ysnony Aiwa — Ajne ae] (sayAy) DI]JASIAI] SIAAWOYIIG
oung prul (josng) D[Jap|VUsa{ DIUWDASOJSKIJAH
Ajng oye] — oune ae] vd (1d¥TeA) pijasnjquo) sisdupopuy
Ajng 93e] I sSatseds puiapdoouks
oun aye] — Avy oye] G (@>Alae)) DIJaIIVGD DUNY]L]
ysn3ny Apes — Avy prt (WOp.IvIN) DIJajNgvUuUUNUAA] SAPOUOIY,D
ysnsny Ajiva — sung ye] (yjosng 2 souieg) sniajdopisd sapouoiyy
Ajng oye] — oune oye] (uneig) snsnja20 Sapouolyy
Ayng prt — Avyy oye] (sudtuayD) pyjaosnfolpaul sapouolyy
ysnsny Ajreo — oune piu (snioliqe,]) DIJadqnsn] Sapouolyy
ysnsny Ape sospoH 119]JJDS Sapouolyy
Ayn piu (19]]97,) DIJaNUyUoI Sapouolyy
Ayn 91] 76 uneig WNIYISDA MIU SatIdads YUIAYISOUNAOUH)
sSNsny Ie] vd soyAy DJaUuoLsuajdas DUAYISOUNOUL
Ajng avy — Apne pr rd II] [IZ DJaaqud] pIyIajayH
Jaquiaydag piu — jsnsny Apa a yosng DiJadvAp vIyIajaH
Ajng oyey — oun 91e] I soreds pydosjoKg
aune aye] — oune Ayia Z Jouqny pyjauuxosd sapoiajay.
Ayn aye] I jsa1deds , piydajouals,,
oun piu — Aepy Apa (poomysa 29 SAoryduuny) sdoiyjav piyaajouax
ysnsny Ajivo — Ayn pri (uneig) pxyapid psnydjajoan
Ajng ajey — Avyy pr € ;Sarseds Mau aouis
Ayn pre (ojeay) pyjavaaid sajiuyIajoajoy
Avy Aj.ieo (UvLUd9.1]) avAOLf SajluyIajoajo)
oune Ayrwa — Avy prt $ (poo'JoW) DAOAYSD]G SajuyIajoajoy
ysnsny Ayo Z (2191) DYajndnAqy SajuyIajoIajo) aepllysojoyH
isnsny Aye ~ UOJUILIS pyjajnuspsyd pIDAVUUTT aepisiiajdouso)
pollog IWSI[q SOION Jloyiny satoads snuan Ayrurey
‘Apnjs IaXK-JdIY} IY} JQAO VPLU SUOTDIT[OO UO paseg SI poltad JYSIpy “ISIP{IOYS (€Q6T) “[e 19 SASPpOH IY} SMOTIOJ
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535
IRA NEAR LAC LA BICHE
iPIDOPTI
NCE: LE
iOR, LANDRY, and SPE
POHL, LANG
2004
{yn avy — oun piu (Gueltte)ie)) punjoiospf puilouosd&y)
snsny Ayia — Ayn ae] (WURYSUIS|e A ) DUDUIUJNI DIJAIOJON
ARIA] OR] Z (ysnouunqop) DUDBAIAUOD DJBUDY
Ayn ae] © (SUOLU]D) puppulipd vjaupyd
oune prw G (Oya) DupawamD AIwau saidods DIaUvY_
Ayng pru (OJ.vay,) DupayAng DIUNAY
Ayng piu — ounr aye] (YIOMLH) DUDINUIUIP S1JKOUY
oung av] (4o1]O.14) punjdwoo syaouy
Ayng pr — sung ae] Z (SUdUO]D) pupmplooasnf rweau soroods sijdouy
oun aye] — oun piu TZ (19][97,) DUuvINIIV] WedU Satoads syAouy
aune aye] — Aepy qe] (19][97,) pupnbapgns syaouy
oung oye] — dune pr (souqny) DUDIIIDJAU SaNasysa|Q
isnsny Ayiea — sung pri (J9TYOSO\) DUDIIDIS SaNadyja|Q
Ayn piu (UIBYSUIS|eAA ) xajdnp vjiydpiosopnas q
ysnsny Apiva — Ayn aye] (WOJIvIy) pupaouas smuojody
Ajng pri — sung aye] (USTIUIOH) ppyful snuojody
ysnsny Ayia (OJIN) puvjdasap siuojody
ysnsny Ayjieva — Ane Apiea (aouqnH) puvasdps snuojody
Ayng pruu (OJ.1vay) DUDAUIO]D DAUD. — IVUTJNIAYJOTO — IePIOL.AAO],
ysnsny ov] — oune pr (Gelttc)ie)) DUDISAMA Sisda])
Ajng aie] — oun pru (AD4[VMA) pDuvonapjaut sisda])
Ajng ae] (pyeusa) pupisuauia]o sisda]y
ysnsny Ayivo — sung oye] (you) puvoisiad sisdayy
AVI AP] (19q[RMA) puvjoyfy snuapuas
Ayng aye] — Apne piu (TO4[PAA) DIdsosk8AV SAIYMY
Ayng pr (SUOWI[D) puvsafnlunf{ DANIUOISIAOYD
Ayn piu — sung 29] (JO4TRMA) DUDJIIJUOI DANAUOJSIAOYD
Avy 23¥] (ADq[RMA) DUDIUDG]D DANIUOISIAOYD
ysnony Ayres — A[ne oye] (SLB) DUDAIVDSOA DANIUOJSIAOY,
ysnsny Apia — Ang pr NOsAVIyY DUDPVUDI SuUaPUD
ysnony ae — Apne pr (ADYTVMA) SIDSnavp! VIOUAID] J
Ajng 33e] | /Satoeds sryjouns.ivdg
ysnsny Ajiea (SUSU9]-)) DUVIDINIVas Siyjouvssvdsy
ysn3ny Ajiea (JOY[PAMA) saployjupx s1yjouvnssvds
oun pru (snovuurT) DUDAJSIUMU DIN
qsnsny Aiea — A[ng oye] ig (UOSUIqOY) puvjdwuosd sayjay
oune 3je] (YIOMe}) puvu syayIo)
Jaquiaydag piu (snto1ige4) DUDSADULA SIAAJIV
oung Aiea — Jsnsny ae] (uosuIqoYy) DAUIJOABIU SIAAJIV
poled IsIf4 Sd1ION JouNYy soroads snuay Ayre]
‘Apnys IWIK-IdIY} OY} IOAO IpRUL SUOT}DIT[OD UO pase SI POLlod IYSIP “ISIPJOOYS (E86) ‘[e 19 SOSPpOH IY} SMOT[OJ
Bxe] JOYSIY UTYIM BdUANbas sa1dadg “(GHG ) UBSUAISTLY JO VY) SMO[[OJ UONROYISSe]O JOYSIP{ “eLIOq[Yy ‘aye poomyYonoL, Iau pojoa[joo saroeds vsaydopidey Jo isi] (panuyuod) *Z ATAV |,
Vol. 118
THE CANADIAN FIELD-NATURALIST
536
Ayn ae] (sudua]a) DIJA8VAI3 NA YjYdlss3y
Ajng oe] (13 [9Z) DIJAJOIANA DALY AUSY
snsny Ayre p (udyourz) SN]JAYIVA] SNQUIDAD
snsny oie] — Apne oye] (1jodo9s) snpjajsad snquivsg
ysnsny Ajaewo — A[ng prut (aehq) SIDj4aqV viuopny
ysnsny avy — Apne prut IOC sypisvidig viapdoos aepriquivig
ysndny Ayes — sung aye] (19][97Z) DIJAIUOAPIAYIO VISOINT
sung Ajiwa — Avy Ay.eo (douqnH ) DIJA1AVINSSO1s DIpoydoz
ysnony Apres — sung aye] dolUNY 2 BNNINIAY Saplopjanauad DIAJICAOIG
ysnony Aiwa — Avyy Oe] (jouosey) Dyjaoiajajqns sisdojakpy
Ajng aye] G \S[NH DiJajniag ‘qoid ‘ds sispqgoioy
Ayng pruu (1OYIPAA) SIpsnjaucy] DIUOYINOG oeprypeskg
Avy Ape (UIeYsuUIs|eAA ) DIJajuagSa1d DIpUuOg oeprursodieg
Avy Ape (WIBYSUIS|eAA ) void pyyddjquy
Ayng pri (AD4[VAA) SnjAJavpouloy VisUul]|ay] aeploydosaid
Av] prul Alpue’] 29 Arpuey louuryey Buon] y oepnionyy
oun ae] — sung Ayre vd (puenig) Dyjajoundi.sadsp V1IyIOM depIpoly)
Ajng ae] (1ouqnH) DuvIp S1jnasoyy
oune pr (aekq) DJauaplgIgo SVALO]DI aepynai0yg
Ayng pr (YOLIUIoH ) pnbopixayf vps)
Ayn ajey — Avyy aie] (josng) puvjndod pips)
Avy, oie] — Avy Ape WUBYSUISTeAA pupjoun] DyoydviH,
Joquiaydag piw — jsnsny ary] (peut) puppul] pyouldy
ysnsny ary — Apne aye] Z (Hoyeay) pupuowou pyouldy
Ajng prtu — oun oye] (1OYIPAA) DUDSsusUudA] DYOUIAT
Jaquiaydag piu (ojIvay) pubajppi4o pyouldy
Jaquiajydag piu — Avy aye] (o19]D) pijasiu pyouldy
Ayn avy — Avyy avy] (WIeYSUIS|eA ) puvoydijzaa pyouldy
qsnsny Ajrea — Ayn pr (WIeYSsUIS|eM ) Duvaupjspo pyouldy
Jaquiaydag piu — Ayn aye] (snavuurq) puplipuvjos pijouldy
ysnsny avy — Ang pr (snovuur’y) pyjauosisy vyouldy
Joquiaydag piu YOLulay] DUDIIPDA DPJASUH)
Avy plu — Avy Ay.tea (WUeYSUIS|eAA ) DUOSALO DAaJUaXapNnas
Ayng oe] []oMog pupunjs0fun DAIYADAAZ
Jaquiaydag pri Z (Woy.way) puounjiof piaydv.i1az
Ayn aie] URLUdd1 2 BAINNIN sisuappuvs v1aydvs1aZ
oun ae] — oune piu YOLIULOH, pjoun[pp piuouosdéy
A[ng oye] Z (SUdUa[D) pupjoo1ayps puouosdk&y
Ajng aye] — oung pri YOU sluoynjysqns puouosdéH
pollog 14314 So]ION Joyny saioads snuan Aprurey
“Apnys 1edX-99.1Y) OY} QAO ape SUOTDAT[OI UO pase SI PoLiad WYSIPY “ISIP{IOYS (E€8H]) [B19 SOSPOH OY} SMOTI[OJ
exe) JOYSIY UIYM IoUANbas satdadg “(GGG ) UISUIISIFY] JO IVY} SMOT[OJ UONLIYISsL]d JOYSIH “VUOG]Y ‘Oye poomyYoNoOL, Aeau payda][oo satoeds viaydopidayq jo si] (panunyuos) *Z ATAVL,
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LEPIDOPTERA NEAR LAC LA BICHE
POHL, LANGOR, LANDRY, and SPENCE
2004
Avy] Ay.rea (TDYTVM ) DIADSAN DIIKT
Ayng prtu — sung pr (snovuur’y) DIADINJAG UOISI
Isnsny Apia — oune ey] (aquany) DIADIJAIOd DIUUADOGOJOLd
aun Apiea — Avy pr (ADT[NULIIFFIYIS wz stusq) piapnosndasd sidosjoq
Ajng prt — Aeyy oye] (souany) DIADAAD] SISdOPIA]
Av], prul (194[BMA ) DIXAJAIJU VDAN|DYJaV
oung Apiva — Avy pr (TDATCAA) ppusoxa DIUOpyoyliCQ
oun aye] (jayouodnq) piuvjsaddi DIUWPASIG
Ayng pruu — sung Apiea (aouqnH) DIADUSIS DIADIDIN
Ayng prtu — Aeyy pri ({jes1eog) DIDAIIS]N DIADIDW
isnsny Apiea — oune aye] (1dYIVAA ) DIVIIDIIG VIADIDW
ysnony Ayia — Ayne prw (UBLUSIOAq) DIADIIAO] DIADIDIN
Ayng ayey — Apne pr (S1aquny,) DIVIUUNAG VIVID
Ayn prtu — sung prut (as[ny) SIVUIGAIA AUDIO! — WUILUOUU — depLNOWIOIH
Ajng prut — ounr 3e] (JOyTeAA) DASOA VIALCQ
Ajng pri — Aevyy oye] (preyoed) pvauipig vuvdas1q
ysnsny Apiva — Aevyy aye] JONTCAA vypno1v Duddaq
oune Ayiwa — Avy] prul (aguany) suapnd paypaying
Ang prut (a9uany) saplosoydoJDUkd DANDAYIJOPNAS J
Ayng prtu — sung pr (asson) DIdIUIS AUKSOAGDH oeprurdaiqg
ysnsny Ayiewo — oune aye] (Ainiq) SIUMAYIAD DIYIAD]ISDG
snsny av] — oune ae] (qepoy) 1AIg] NU SIDISY
aun aye] — 19q0190 Aye (snovuury) pdoyup sijpyduan
Avy] prt — Aeyy Ay.ea (spreMpy) SNAKIDS DIUOSA]Og oepryeyduAnyy
oune ae] ({BAnpsiog) DINJUAUD SaL1aagq ovpiuaroh']
aunf 31e] sLuey DaIVAsI]O SAI PL
Aqng aye] — Avy oe] ueplor 2 P[LYOsyIOY sisuappuvo o1piddg ovprluorideg
ounf oe] (sted) uowanppod snjpydados1ajADD oepruiodsay
ysnsny Aiwa — A[ng pr (pyeusaj) ajpusisoquinjd Dwus1JSOjJsltoy)
qsnony Aiea — oung ye] (AAV) SISA] DAP|
Ajng Ajiva — Avyy oye] pieyorg Sypas1og DISNDAKG
oune Ayia (9]01D) sypoiu visnvskg
Ajng pruu — sung pru (jasvujny) DIDUOLOD DIUAVJIA] Yd
oune ae] IO]]9Z, sypynoave vyspdsisad
Aqne oe] (jaseujny) DIDpINd SISassaaq
ounf prut (susua[D) sypnovu xudodvsvg
ysnsny Ayiea — oun pr (TDyTeM ) sypsaqygo vyyouas
Ajng aye] — Ayng pr (OJIeay) Dyjajoundissop visvipad
polled Ws Joyny sotoads snuan Ayre]
‘Apnys IeaK-daIY} IY) JOAO IPL SUOTIDAT[OI UO pase SI PoLtad IYSI]T4 “ISIP{IOYS (€86]) ‘Te 19 SOSPOH oy} SMOT[OF
BXe] JOYSIY UIYIIM Jouanbas satdadg (GGG) UdSUDISITY JO JY] SMOT[OF UONVOYISse[O JOYSIF{ ‘eMOQLY ‘axe poomyonoy Ieau payda]joo sorseds esajdoprdayqT Jo ysvq (panuyjuod) J ATAVL,
THE CANADIAN FIELD-NATURALIST Vol. 118
538
Aq ae] = Avy Oe] OMS” DIIDALJad DUBWIOLIPA FT
isnsny Ayre qS[0H NB1093 DIAKWA]
Ajng piu — ounr Apvo (AO][NULIDJJIYIS wz stusq) pvaappis piadoydyoy
ysnony Ajiwo — Ayne pre (as]nH) DUIJAX S1YJ1NGY
ysnsny ae] — Ayn pr (JOP) pypupjdxa siyyjng
ysnsny Apia — Apne pr (AOTB AA) pivsndoad siyjyjny
ysnsny Ayes — oune prt (s[ny) DSOWAOL DULOAJSSKG
ysnony Apiva — Avy aye] (aguony) DIVDIJISAIY VUOAISSKG
ysnsny oe] — ounr oyv] ({[esae9d) DIVIIYIDM DUOASSKG
Ajng piu (jadvujny) DIDIUNA] DULOASSKG.
Joquiajdag piu — ysnsny Ayia (snovuury) DIDANI DUOAISSKG — DVUTUDIB'T — aepLauoayH
ysnony Apiwo — oung pruu (A9[YOSOP) piuppisidf pjndorsy
Ayng ajyey — oung oye] (JOP) piapjount pindoog
Ayn piu (as[ny) pypjjaoup vindoos
qsnony Ayteo — Ayn pr (YIoMeH) pippunoquyy vjndoasy
Ayn aye — Avyy oe] (sguony) piupulnpuad psoydojrKy
oune aq] (paeyord) pypuUuadopunjod Dapp] —-—- IWULY.ID}S — 9epLNawUo0ayH
ysnsny Apes — Apne aye] (AdJJBYOS-YSLIOH ) DIADISISAL DAWVIOIVUAN
qsnony Ayre — Apne prt (SLI) DIADNIDUL DKIIS
Jaquiaydag pit — jsnsny aye] (s9uaND) DIAD]JAISY DUIPQuUIVT
Ayn prtu — Avyy aye] (a9uany) DIADAOAIMIND Yulsag
Ayng ayey — oung pr TOYIRAA vIvsiAlp VjaduUvy
oung aye] — Avyy ov] (aguany) DIADJOOID SIPOSY]
sung oye] — Avy pri (souony) DIADSOSO]Yyd SIPOSV]
ABA OR] (snovuurq) pidpsaapnd siposv]d
aun aye] — oune Apvo JOYICAA DIVUNUAAap DUAaUDIaW
ysnsny Apiwo — Avy aye] douany DIADUOIDUI DUAUDIaW
oune Apwo — Avy pr IOYIRA piapaydig]p piuajas
Joquiajdag pri — ysnsny Avo souany DIADUSDU SOWOUUT
ysnsny oye] — Apne pr (souany) vypjsad papduvy
Ayn Ajrwo — oung prtu (JO4[CM ) DIADISAUOY OLA
ysnsny Ayes — Ang pri (Ain.iq) pjadsos adxjoyjuvx
ysnsny Apiea — oune avy] (aauany) DIADUIAS 1] DUAD]YIN|
Av IR] (our) DIADUISADU DUAD]YINA
Ayn piu (touqnH) DIADSNIGO DUAVDJYINT
Ayn piu — oung pr sauany DIADJOIIDA DABQDI
ysnsny Ajiea — oune pr aouany DIADUAYJAAA DIAQDI
19q0190 Aj.rea — Jaquiaydag prur (SLR H) DIADIPY SIUUDAT
poliog ISIy SO]ON Joyny satoads snuan ATTUue,y
“Apnys IdA-da.1Y} OY} IOAO pel SUOTIAT[OI UO pase ST polad IYSIPY “ISIPJIIY (€Q6]) ‘Te 39 SASPOH IY) SMOT[OJ
BXL] JOYSIY UIIIM BoUONbas sarsadg ‘(GGG |) UASUAISLFY JO JY) SMOT[OF UONVOYTISsL]O JOYSIF{ “eOqLY ‘Oye poomyonoy, teau payoay[oo saroads vsaidopideyq jo asi] (panuyuor) ‘7 ATA],
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POHL, LANGOR, LANDRY, and SPENCE: LEPIDOPTERA NEAR LAC LA BICHE
2004
Ayn Ayrea — Avyy prut (SLI H) DUDILIAWUD DUISapo]]|AYq oepiduresoise’']
isnsny Apes — oune pr pieyorg DIDAOUWD DIZZ1]]VIJ aeprUuRsip
oune av] IOYICA pIdIIBIAIU DAOYdOGOT
oune pri — Ary Apiea (1OMTVAA ) DIDANJYOAID DAVPYID
ounr Ayiea — Avyy pr (1O¥TVAA ) DIADIUN] DADPVID
Avy piu (preyord) DIDPIAIA SISDIV
ounr Ayiea — Aevyy prul pieyorg DIVIVISOIOADA DIDAYNAN|
oun ae] — sung pr JOYE piavoyup pigayndny
ysnsny oye] — une pr (as[nH) DID Jas vioayndny
Ayng prtu — ounr Ayiea (as[nH) pasnfsad pigaynldny
ysnsny Apiva — Avyy oye] Aepolqnoqg ppjiuissy pigayydny
Ajng ayey — Avypy 21] (touqnH) DIDAAIDS DIDAYIAN|A
oun ae] — Aeyy oye] (YJIOMP}) pyposnfqns visayjidny
Av P| (aehq) pipiquinjoo pivayndny
ysnony Aiea — oung aye] (JD4TPAA) poipuau aydpqny
19q0}90Q Ape (as[nH) pypaonag vsajydosad¢Q
Jaquiajdag piu (Uasneyyog) pipuumnynd vylssdy
Ajng prt — Aryl 312] (s9uaND) DIDIPAOG]D DIZAPOYIIAT,
Ayng pri — Avyy pr (aeAq) 1jpsavad pisnua,
ysnsny avy — Avy oye] sing DIIAQUIDI DISNUAA
ouny 9}e] (1O4TRM) DAiafiqyy DYAaIpAH
isnsny ae] — Ang pru OulsseZ pypuidjp sdajydouaz
Aqng aye] — Avy pr (aguond)) vypipawaaqur pidydny
Ajng oye] — ung pr (JOT [NJA) vpUsayp aoyssdy
ysndny Ajiwa — Avyy pru (aguany) DIDAJSNIVD] OYLOYJUDX
Ajng piu — Avy oye] (PID) DIDSNALA, POYAOYJUDX
isnsny Ayiea — Ang piu (aadsq) DIADAO]OIAP BOYAOYJUDX
isnsny Aiea — oung AT Ivo IO[ARL, DIADSSOL JOYAOYIUDX
Ayng ae] (gouaNy) DIVNp1 aOYsOYJUDX
ysnany Aiea — sung aye] (1dJJVYOS-YSLLIOH ) DIADSDAQD AOYAOYJUDX
ARIA AL] (TOTEM) Dpsafyjnul vajayUy
oune Ay.rea — Avy pr souony DIVIPISDA DAJIYUY
Ajng aye — Aqne Ayaea (JOC ) DIVIDSDG YULOZ1A Aq
Ajng prut — sung pru (AD][NULIAJJIYIS 2 studsq) DIpNjan] viuvs.ivds
Ajng piu — Avy Apivo (suony) DIDIPLIYNA DINA|OSAW
Jaqo1oQ Aira — Jaquiaydag piu (aguony) pypyisapy vsoydisy,
ysnsny ae] — Apne aye] (Siaquny,) DIDIAN{ DUAULOLIPAH]
Ajng ayey — Avyy oe] (194014) DIpAAGNA DUAUWIOLI PAL]
Ajng aye] — Avyy oe] (ADT ) pIpIOUNUAL DUAWOLIPAL
pollog SI SO}ON JouNy satoads snuan Ayre]
‘ApNys IdK-9dAY} DY} JOAO IPLUT SUOTIITTOS UO pase st PoLtad IYSIpy “ISIP{IOYS (ERG) ‘Te 19 SOSPpOH oy) SMOT[OF
BXe] JOYSsIY UTyIIM doUENbas satdadg (666) UASUIISITY JO IVY) SMOT[OJ UOTVOYISse]O OSI “ViOq[Yy ‘Oye poomyonoy, 1wau pajoa][09 sardeds vsgydopidsy jo jsv] (panuyuod) *7 AAV,
Vol. 118
THE CANADIAN FIELD-NATURALIST
540
Ayn oyey — Apne pra aauany sypnbuidosd pinay OVUI[NALY — oepINIoON
ysn3ny Apiewo — Apne pro (UIUS “g'f) pauliyovisf sapouadiy seurueutsdans — aepmnjoony
Ajng piu — sung oye] (aauqnH) SYDINBUD SIYI]Vq
Ajng prut dauany SIPULIpvADI Duldalg
Ajng a1] vd (UIs “g'f) NUDYUDY VjOISOUay|PUd
ysnsny Aiea — Avy] oe] 01D sypasjad vINOIKYD
ysnsny Ayivo — Apne pr (yt “g‘f) pq]vIN] VYyIwUsO]IUDZ
Ayn prt — Avy oye] (IDTV) sypsnupskd punydouanjpyd
ysn3ny Ajiwo — A[ng prut ¢€ Jouqny pinwav eau saisads Mau VIP]
ysnsny Ayia — Ayn pr Jouqny pinuav VIP]
ysnsny Apieo — suns oye] (aguany) SIJDIIAAWUD DIP] BUNULULIOF — OepInjoOoN
ysnony avy — Avy pr (TDAP) puppisidf DjoajotN — seuldt1yjo.LIeg — aepinjooN
Ayn ayy — Apne pra (TDYIPMA ) pypispyd palyIksvg
Ajng oyey — Apne pri (ysnouunqgdsyy 2p soureg) SUDBDA DAIYIASDG depILUeULAT
oun aye] — oun piu SLLIeH ppjnoput vduma20ydoT
Ayng piu — oune pru (SLLIeH) souayjipd DYIAVID]
oune a}e] — Avy ae] JORMA SUD]IUNSSD DIGOJDUSDAY
qsnsny Ayiea — Ayn piu (O[[IAQUSAJ-ULIOND ) 1ajuoza] vojdpy
ysnsny Apivo — Ang prur pieyord DID|G]Y vIsuauia]D
ysn3ny Ayres — Ang pr (2}01D) 4OJONIG DUA] oeplyno1y
ysnsny Ajiewa — une aye] (01) saplouyda] vanziyos
Ajng Ay.ea (yyUIS “A‘f) STUAODIUN DANZIYIS
oune ae] (uospny) DISAPOU DINIANA
oune ae] — Aeyy ae] (eAnpsiog) pUulApuadojoos VINIANA
oun aye] — Avy oye] (touquUr'T) SIDJUAPIIIO VINIAN
Avy Ayivo (01D) laujuy pisiydnjpH
Avy, RY] — Avyy pre uospny pynopuan visiydn]H
ysnsny Ajava — Aeyy ey] IONE stuoluajdas visiydn]y
oun Ajrea — Avyy oye] jovin pip) dus DJUOPOJON
Aqne piu — Avy prur pieyorg DSOUL DISOAY
oune pruu (YJIWIS “A'f) DSOgq1s DIDPPN
oung aye] — Ary oie] (IOyTRM) sypo1dv p1ajsoj]D
sung aye] — Avy oye] (01D) DSOBIAJS DAAJSO]D
Ajng avy — Avy ayy you DUSISOG]D DAAISO]D oepnuUopo}ON
oun ae] (Sinquia}0y) mp8 Saja
isnsny Aiwa — Avy pr AQAry IAS1499 SNYJULLAWUS oeprsuryds
ysnsny Apiewo — Apne pra JouqnH DIAISSIP DULOSOIDIVDIN
pollag IWSIpy SION Joyny satoads snuan ATTUre.y
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54]
IRA NEAR LAC LA BICHE
NCE: LEPIDOPTI
4
POHL, LANGOR, LANDRY, and SPE
2004
ISNSNY av]
(aakads)
pupoiiauy paodiyduy
Isnsny ayey — Ayn pr (aouqn}) DIIAUSNS SUYINSDADE
Jaquiajidag prw — jsnsny ar] (JOYIVAA) VIDIO}! DISCO
Jaquiaydag piu — ysnsny aye] (sauany) DIVIIDU DISICQ
snsny Ayiea — Ayng ae] (ujTwIS) pID]IBOI Daubdy
Ayng aqey — Avyy Ayiea (JOMTeAA) ppowuos vaupdy avuluapeH — oepinjooN
jsnsny ae] — Apne ey] (JOMPA\) pxiful Duapoyouoryy
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ounr piu (TOYTR A) DIDUSISIA] DUUAULISIAAD FY]
aune piu — Aryl aye] JORMA DSSatdull DIJUOLIY
oun ae] — sung Area JOYE Djajdul vjgU0LIy
snsny Aiea — APY] Ae] (aguany) SIS DAL DIDIUOLIY
Ajng piu — Aevyy aye] JOYE VASUs DIMUOLIY
snsny Ajiea — oun pr aguony DIDIJOUUL DIIIUOLIY
aune ae] — dune Aye douony DUldna DIIUOLIY
Ayng aqyey — Aryl ore] OID Jawdf viydvy —- aeua1uosdVy — ovpIndd0N
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ysn3ny Apia — une ae] douonh nupujnd pisn}d
Ajng pr (AqIry) vinsuvpjoad DyddAsUuKsS,
Aqng aye] — Apne pr (Insusjongd) spyp pydvssuasy
ysnsny avy — Apne aye] (Q]01D) DUB ISIPIA1A DYADABUKS
A[ng ae] (9019) pidiagsoja0 pydvssuasy
Ayn ayey — oung aie] (1DYTRAA) pidup pydvisoiny
Ajng prt — oune oye] (UOSUTGOY 2 901) pddpu vydpisojny
ysnony ary — Ang aye] (suoydays) pypnovuig vydpssoiny
oun aye] — oun pru Insud;OnNO ppigqna pydpasojny
Ayn ae] (sound) saproskyoay) XKsajdosoydsogq
Ayn ae] (Q101D) psowsof pyduicuvsKy)
ysnsny Ajiea (anyioqQ) DP]alauUsa DISKAYIA] Og
Ajng ae] (9101D) saploasav DISKAYIVDIG.
Ayn prt — oun 39e] aouonty S1JUAIN DIOISOAGY avuUlIsN[d — sepInjooN
snsny ae] — snsny Ajies 01D DIIYAAMUIS DIVIOIDD
Jaquiajdag piu — jsnsny Ayiea spiempy SIASIAG DIDIOIDD
Jaqo1oQ Apiea — Apne aye] JOC pentiun pjps0jvyD
Jaquiajdag prut —ysnsny Ayieo JOC DJIAL DIDIOIDD
ARYA] IE] (WJIOMeH) DINISNISSDAI DULIBANUID IVUT[RIOJVD — OepINIION
Avy pruu STeY ynuny Duaday
isnsny aye] — Ang pra (Aye ) sypjoipa puaddy
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polled ISt14 loyny soroads snuan Ayre
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Vol. 118
THE CANADIAN FIELD-NATURALIST
542
Ayng oye] — Apne prow
ysnsny Ajiva — Apne pr
ysnsny yey — Ayn pri
oun Aj.ro
oun Ay.eo — Avy plu
oune Ayrea — Avyy Apieo
Avy pr
oun Ayre — Avy pra
oune ae]
Ayne ayey — Apne prot
ysn3ny Ajiea — sung aye]
Ayng pra
Ajng ae] — oune aye]
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oung pri
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snsny oe] — Isnsny Aj.ea
ysnsny aye] — Isnsny Ayia
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Jaquiaydag piu
snsny ae]
Jaquiajdag piu
Jaquiajdag prt — ysnsny Aya
oung Aye
oung Ape
oung Ajiva — Jaquiajdag piu
19q0}9Q Aj.iea
Jaquiaydag pr — \sndny ae]
Avy] plu — Joquiajdag pri
oun ayey — Avy oe]
Ayn pr — oung prut
snsny Ie]
Ajng piu — Avyy oye]
ysnsny oe] — snsny Ay.ea
Jaquiaydag piu — A[ng prur
Joquiajdag piu — Ajng oye]
isnsny Ajaiva — Ayn pr
oune aye] — oun Avo
polled 1Yyst[4
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(91019)
(yMUIS)
(Q]01D)
(aguany)
(21019)
(aguany)
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(Q]01D)
(s9uony)
(suaydays)
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(01D)
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(suoydays)
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543
AR LAC LA BICHE
4
IRA NE
PIDOPTI
POHL, LANGOR, LANDRY, and SPENCE: LE
2004
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isnsny aye] — Apne aye]
snsny Aiea — Avy Aprea
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(UOSTLIOJ{)
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544
THE CANADIAN FIELD-NATURALIST
Vol. 118
Gelechia lynceella
FicureE 2. Microlepidoptera collected near Touchwood Lake, Alberta. All are new Alberta records. (ruler = lcm).
The study site lies within the ranges of 67 butterfly
species (Bird et al. 1995); many of these certainly occur
in the mixedwood habitat but were not collected there.
Some nocturnal moths, including some species of
Gelechiidae and Oecophoridae (Hodges 1974; Miller
2000), are not attracted to UV light so they would be
undersampled as well. If other moth species occur in
the area but were not collected, they are probably quite
rare, or may be extremely localized in particular micro-
habitats, which were not adequately sampled in this
study.
Macro-moths comprised a greater proportion of
individuals than of species, whereas the micro-moths
were particularly species-rich, comprising a greater
proportion of species than of individuals. These pro-
portions (Table 1) were similar to those previously
reported for the province of Alberta. In his list of
Lepidoptera of Alberta, Bowman (1951) reported 40.8%
micro-moths (779 species), 50.9% macro-moths (973
species), and 8.3% butterflies (159 species). In the most
recent list of Lepidoptera of North America, Poole
(1996) listed 49.3% micro-moths (5743 species), 43.9%
macro-moths (5114 species), and 6.9% butterflies (801
species). The proportionally higher representation of
micro-moth species in the current study compared to
Bowman’s 1951 list reflects the recent increase in
knowledge of the group, including the description of
many new species.
A total of 35 positively identified species are new
records for the province, and one (Acanthopteroctetes
bimaculata) is a new record for Canada (Table 2).
Micro-moths (Figure 2) make up 34 of these new
records; a further five micro-moth species and one
macro-moth species represent undescribed species.
Details for some of these new records and new species
appear below.
Acanthopteroctetes bimaculata Davis (Acanthopteroctetidae):
This primitive moth is known previously from California
and Oregon (Davis 1978). The current record represents the
first report of this moth, and of the family Acanthopte-
roctetidae, occurring in Canada. Nothing is known of its
biology.
Caloptilia anthobaphes (Meyrick) (Gracillariidae):
Previously reported from northern Ontario (Forbes 1923).
Nothing is known of its biology.
Caloptilia betulivora McDunnough (Gracillariidae) (Figure 2):
Previously reported first only from Nova Scotia (McDun-
nough 1946) and since been reported from Quebec (Hand-
field et al. 1997). It likely occurs across the boreal zone in
Canada. Larvae feed in the folded leaves of birch.
2004
POHL, LANGOR, LANDRY, and SPENCE: LEPIDOPTERA NEAR LAC LA BICHE
Chytonix palliatricula
FiGurE 3. An assortment of macrolepidoptera collected from mature aspen forest near Touchwood Lake, Alberta (ruler = 1 cm).
Caloptilia canadensisella (McDunnough) (Gracillariidae)
(Figure 2):
Originally described from Nova Scotia (McDunnough
1956). It has since been reported in Quebec (Handfield et al.
1997; Landry and Landry 1992), and is probably widely dis-
tributed but uncollected across the boreal forest. The larvae
make large blotch mines on the leaves of Bunchberry (Cor-
nus canadensis).
Caloptilia coroniella (Clemens) (Gracillariidae):
Previously known only from the midwestern U.S.A.
(Forbes 1923). Larvae feed on birch.
Caloptilia stigmatella (Fabricius) (Gracillariidae):
Not reported from western Canada, but GRP [Greg R.
Pohl] has collected it quite commonly in Alberta and Saska-
tchewan. Larvae feed on willow (Forbes 1923).
Argyresthia abies Freeman (Yponomeutidae):
Reported in eastern Canada only as far west as northern
Ontario (Freeman 1972) but is probably widely distributed
across western North America in the boreal forest. It is a
twig borer on Balsam Fir (Abies balsamea).
Coleophora corylifoliella Clemens (Coleophoridae):
Previously reported only in eastern North America (Forbes
1923). Larvae there feed on Corylus americana; in the west
they probably feed on Beaked Hazelnut (Corylus cornuta).
Coleophora duplicis Braun (Coleophoridae):
Previously known from eastern Canada and the midwestern
United States (Forbes 1923: Handfield et al. 1997). It feeds
on the seeds of Aster (Aster spp.) and Goldenrod (Solidago
spp.).
Limnaecia phragmitella Stainton (Cosmopterigidae) (Fig-
ure 2):
A holarctic species. The closest it has been reported to
Alberta is Wyoming (Hodges 1978). However, collection
records (CNC, NFRC) indicate that the species is transamer-
ican. Recent collections made by GRP indicate that it is com-
mon in western Canada, at sites where its host plant, Com-
546
THE CANADIAN FIELD-NATURALIST
Vol. 118
cronicta innotata
Ficure 4. An assortment of macrolepidoptera collected from old growth aspen forest near Touchwood Lake, Alberta (ruler
—yluemi)®
mon Caitail (Typha latifolia), is available. Larvae feed on
the flowers and seeds.
Coleotechnites blastivora (McLeod) (Gelechiidae):
Reported only from the type locality of Gaspe, Quebec
(McLeod 1962). It probably occurs across the boreal zone.
2000
Noctuidae
HB Geometridae
other macro-moths
{) micro-moths
no. specimens
_
oa
o
o
June July Aug. Sept.
trapping date
FiGure 5. Abundance of major Lepidoptera groups collect-
ed in UV traps through the 1994 trapping season.
Larvae are needle webbers of White Spruce, occasionally
mining within the needles.
Gnorimoschema septentrionella Fyles (Gelechiidae):
Miller (2000) reports this species only in eastern North
America, as far west as Minnesota. It is a stem-gall maker
on asters (Aster spp.).
160
©) Noctuidae
GN Geometridae
__| other macro-moths
{) micro-moths
120
no. species
co
oO
sy
Oo
June July
trapping date
Aug. Sept.
FiGure 6. Species richness of major Lepidoptera groups
collected in UV traps through the 1994 trapping
season.
|
2004
Aethes promptana (Robinson) (Tortricidae — Tortricinae):
The Touchwood Lake record represents the first record of
this species from western Canada. It was previously known
from eastern North America as far west as Wisconsin (Sabourin
et al. 2002). A prevoius record from Washington (Razowski
1997) was based on a misidentification. Nothing is known of
it’s feeding habits.
Wockia asperipunctella (Bruand) (Urodidae):
As noted by Landry (1998), this Touchwood Lake record
represents the first report of this species, and the family Uro-
didae, in Alberta. This family is a recently recognised addition
to the North American fauna (Heppner 1997). Larvae feed on
Trembling Aspen; adults tend to fly during the day or early
evening.
Alucita lalannei Landry & Landry (Alucitidae):
Until recently, this species had been combined with two
other species in the genus, and referred to collectively as Alu-
cita hexadactyla (Linnaeus) (Bowman 1951; Hodges et al.
1983; Poole 1996). However, the true A. hexadactyla 1s restrict-
ed to the Old World. In their description and treatment of A.
lalannei, Landry and Landry (2004) designate a specimen
from the current study as a paratype. This species is known
from Ontario, Manitoba, and Alberta. Adults overwinter,
and can be collected from May to September. The larval
host plant is unknown, but Landry and Landry (2004) report
Lonicera spp. and Symphoricarpos spp. as likely candidates.
Parapoynx maculalis (Clemens) (Crambidae):
Previously known from eastern North America, only as
far west as Lake of the Woods, Ontario (Munroe 1972). How-
ever, recent collecting by GRP indicates that it is widespread
but extremely localised in Alberta and Saskatchewan. Its larvae
are aquatic, and are reported by Munroe (1972) to feed on
several species of water lilies (Nuphar, Nymphaea, Brasenia
spp.). It likely feeds on other plants as well, since it has been
collected recently in southern Alberta, outside the distribution
of the aforementioned plants (C. D. Bird, personal commu-
nication).
Idia new species near aemula Hiibner (Noctuidae — Her-
miniinae):
Usually mixed in with /dia aemula Hibner in collections.
It was reported in eastern North America by Rings et al.
(1992), and misidentified as Epizeuxis concisa Walker by
Forbes (1954). It remains undescribed and has not been
reported previously from Alberta, although it is common
across the boreal region. It has been reported to feed on the
needles of a variety of conifers (Rings et al. 1992).
Phalaenostola hanhami (J. B. Smith) (Noctuidae — Her-
miniinae):
Reported from eastern Saskatchewan as far west as Regina
(Hooper 1988). Nothing is known of its feeding habits.
The only similar published study of boreal forest
Lepidoptera that the authors are aware of is that of
Morneau (2002), which sampled primarily macro-moths
near Peace River in northwestern Alberta. In that
study, 293 species were collected over three seasons,
including 278 species of macro-moths. Although most
macro-moth species were common to both studies,
43 species were unique to the present study, and 115
species were unique to the Morneau study. The pres-
ence of so many unique species suggests some habitat
POHL, LANGOR, LANDRY, and SPENCE: LEPIDOPTERA NEAR LAC LA BICHE
547
specialization within the boreal mixedwood region.
Several of the species unique to the Morneau study,
most notably some Arctiidae species, represent an
incursion of cordilleran species into that area.
Several Lepidoptera inventories of provincial parks
in the boreal mixedwood forest of northeastern Alberta
have been carried out (Schmidt and Pohl 2001*;
Macaulay and Pohl 2002*, 2003*). Although these
studies collected from 138 to 295 species, they were
each based on brief sampling periods, so they missed
significant proportions of the fauna. Catches from the
current study shared approximately 50 to 60% of the
species collected in those studies.
In general, the moth fauna of the boreal forest appears
to be less diverse than that found in other forests.
Summerville and Crist (2002) collected 512 species
of moths in deciduous forests in Ohio. Thomas et al.
(1998) collected 624 species of macro-moths in Fundy
National Park, New Brunswick, which lies in the Aca-
dian Forest Region, as described by Rowe (1972).
Both of these forest types are more diverse botanical-
ly than the boreal forest, and have more moderate cli-
matic conditions (Rowe 1972).
Inventories of this nature are a necessary prerequi-
site to understand impacts of forestry practices and
climate change on biodiversity. However, there is a
paucity of similar studies, largely due to the lack of
required taxonomic expertise. This argues strongly for
increased support of systematics research in Canada, as
biodiversity issues continue to increase in importance.
Acknowledgments
Héctor Carcamo, Tom Clark, James Hammond, Rob
Lucas, Phillippa Rodriguez, Peter Shipley, the late Tim
Spanton, Kevin Sytsma, and Daryl Williams assisted
with field collecting. The Alberta Land and Forest
Service (Lac La Biche Region) provided field acco-
modation, and the Alberta Research Council provided
maps and assisted with site selection. Gary Anweiler,
Klause Bolte, P.-T. Dang, Ron Hodges, Don Lafontaine,
Doug Macaulay, and Jim Troubridge assisted with
identifications. This work was funded by the Canada-
Alberta Partnership Agreement in Forestry and by the
National Science and Engineering Research Council
of Canada (operating grant to JRS).
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548
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Schmidt, B. C., and G. R. Pohl. 2001. Survey of the butter-
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Accepted 27 September 2004
Pilose Braya, Braya pilosa Hooker (Cruciferae; Brassicaceae), an
Enigmatic Endemic of Arctic Canada
JAMES G. HARRIS
Biology Department, Utah Valley State College, 800 West University Parkway, Orem, Utah 84058 USA; e-mail: harrisji@
uvsc.edu
Harris, James G. 2004. Pilose Braya, Braya pilosa Hooker (Cruciferae; Brassicaceae), an enigmatic endemic of Arctic Canada.
Canadian Field-Naturalist 118(4): 550-557.
Braya pilosa Hooker, Pilose Braya, has been poorly understood among North American botanists due to a paucity of fruiting
specimens for study. This has resulted in confusion about the taxonomic position of the taxon within Braya, and has led to
speculation about its generic status. An examination of fruiting specimens from the Royal Botanic Garden Herbarium at
Kew, England reveals that B. pilosa is correctly placed in the genus Braya, and that it is a distinctive member of the genus
deserving recognition at the specific level. I discuss the historical evidence that B. pilosa may not have been collected since
1850 due to its extremely restricted distribution on the Cape Bathurst Peninsula of the Northwest Territories of Canada. I also
present evidence suggesting that B. pilosa is diploid and may be a parent species to some of the more widespread members
of the genus, all of which are polyploid. Its closest living relative is probably B. thorild-wulffii.
Key Words: Braya pilosa, Pilose Braya, discovery, rediscovery, distribution, collections, rare species, Cape Bathurst, North-
west Territories, Canada.
Braya pilosa Hooker (Figure 1) is an extremely rare
endemic of the Northwest Territories of Canada. It is
perhaps the most distinctive and, at the same time, least
understood North American member of a taxonomi-
cally difficult genus. While some botanists (Harris
1985; Argus and Pryer 1990; Rollins 1993; McJannet
et al. 1995) have treated B. pilosa as it was envisioned
and described by Hooker (1830), most have placed it
into synonymy under B. glabella (Polunin 1959; Welsh
1974; Porsild and Cody 1980; Cody 2000; Warwick
et al. 2000*) or B. purpurascens (Scoggan 1978). Oth-
ers have reduced it to infraspecific status within B.
purpurascens (Schultz 1924; Hultén 1970), applied
the name broadly to elements of B. glabella (Porsild
1943, Hultén 1968), or ignored it entirely (Cody 1979;
Mulligan 2002). To the best of my knowledge, there
are no authentic fruiting specimens of B. pilosa in any
North American herbarium. It is this lack of available
fruiting material for study that is primarily responsible
for the taxonomic confusion that has surrounded this
taxon over the past 173 years.
When he described the species, Hooker (1830) had
only a single collection of flowering individuals with
immature silicles from which to work and he was ap-
parently uncertain whether or not the plant was actu-
ally a Braya. He placed a question mark behind the
genus name, lamented the lack of mature fruits that
would allow unequivocal generic placement, and stat-
ed, “...in all probability, it ought to constitute a new
genus.” Without access to mature fruits for examination,
Hooker’s suggestion of a new genus would indeed
seem justified. The flowers are larger than those in
any other Braya species (the petals in some tetraploid
B. humilis are as long but not as broad); the immature
silicles are ovoid-ellipsoid, unlike those in any other
Braya with the exception of B. thorild-wulffii (which
had not been discovered in 1830); and the styles are
exceptionally long for a Braya, measuring over half the
length of the ovary. In addition, Sir John Richardson
(1830), who collected the type specimen in 1826 during
the second Franklin expedition in search of a north-
west passage, described the flowers as fragrant, with
a smell similar to lilac blossoms. Fragrance has not
been associated with any other member of the genus.
Murray (1983*) and Scott et al. (2000*) suggested
that B. pilosa is a misnomer applied in error by Hook-
er (1830) to a Draba, likely D. corymbosa. However,
Hooker’s original description and accompanying illus-
tration of the taxon indicate that he is describing some-
thing quite different from D. corymbosa. Hooker
describes the valves of the immature silicles as “valde
convexis,” and again later as “remarkably convex,”
descriptions that do not accurately describe the dis-
tinctly flattened valves of D. corymbosa.
Fortunately, any doubt about the identity of Hook-
er’s B. pilosa as a legitimate Braya rather than as a
misidentified D. corymbosa 1s resolved by an exami-
nation of authentic fruiting specimens. There is a herb-
arium sheet at the Royal Botanic Gardens Herbarium
(K) in Kew, England (Figure 2) that apparently in-
cludes specimens from three separate collections (Sea
Coast, Arctic, Richardson s.n., 1848; arctic coast, W.
of C. Bathurst, Captn. Pullen s.n., Aug. 1850; and what
are likely part of Richardson’s type collection of 1826).
The herbarium sheet is so congested that it is impos-
sible to be certain which individuals are part of the
various collections represented, but all of them are defi-
nitely members of the same taxon. Mature silicles on
550
2004
HARRIS: PILOSE BRAYA: AN ENDEMIC OF ARCTIC CANADA
Ficure 1: Illustration of Braya pilosa.
55]
Bp
these specimens, even though pressed, are clearly
ovoid-ellipsoid and perfectly match Hooker’s illus-
trations of immature fruits of B. pilosa. In addition to
possessing fruits that are strikingly different from those
of D. corymbosa, the Kew B. pilosa specimens differ
significantly from D. corymbosa in several other attrib-
utes. The leaves are much longer, narrower, thicker,
more obtuse, and less densely pubescent than those in
D. corymbosa; some individuals bear a single cauline
leaf while D. corymbosa lacks cauline leaves; the styles
are much longer than those of D. corymbosa; and most
importantly, the epidermal cells of the silicle septum
are typical Braya epidermal cells, characteristically
thickened and transversely or obliquely elongated
(Harris 1985, Figure 2), in stark contrast to the thin-
walled, irregularly shaped, and essentially isodiametric
septum epidermal cells typical of Draba. Braya pilosa
is unequivocally not a misidentified Draba.
I have not seen any authentic specimens of B. pilosa
that have been collected since 1850. It is possible that
it is extinct, as Argus and Pryer (1990) and McJannet
et al. (1995) have suggested, but I think it more likely
that its distribution is so limited that it has simply been
overlooked by botanists. Hooker’s (1830) description
of the type locality of B. pilosa, “Mouth of Macken-
zie River, lat. 70°” may be somewhat misleading to
those who have looked for B. pilosa over the last cen-
tury or so. Porsild, for example, made several collec-
tions of Braya between the mouth of the Mackenzie
River and Nicholson Island in Liverpool Bay, where
Hooker’s location description suggests that B. pilosa
should be found. Although Porsild initially identified
his collections as B. pilosa (Porsild 1943), none of them
show the distinctive ovoid-ellipsoid silicles, exception-
ally long styles, and large flowers of this taxon and
fall instead within the normal range of diversity in B.
glabella.
There is evidence that Hooker’s description of the
type locality may be his interpretation of Richardson’s
broad conception of the Mackenzie Delta rather than a
precise description of Richardson’s collection location.
In his account of the 1826 journey from the Mackenzie
River to Cape Bathurst, Richardson (1828) repeatedly
commented on the alluvial deposits and sandbars his
party encountered in the area, and correctly attributed
them to outwash from the Mackenzie. He clearly
viewed the entire region of the Tuktoyaktuk Peninsula,
Eskimo Lakes, and Liverpool Bay as a product of a
historical Mackenzie Delta. It is likely, however, that
Richardson was actually very near Cape Bathurst rather
than the mouth of the Mackenzie when he collected
the type specimens of B. pilosa. In fact, there is some
evidence that all three known collections of B. pilosa
(Richardson in 1826 and 1848; Pullen in 1850) may
have come from the same stretch of seashore near Cape
Bathurst, roughly 200 km northeast of the mouth of
the Mackenzie River.
John Richardson’s original collection of B. pilosa
almost certainly occurred on 18 July 1826, as the east-
THE CANADIAN FIELD-NATURALIST
Vol. 118
ern detachment of Franklin’s second expedition in
search of a northwest passage was approaching Cape
Bathurst. This eastern detachment, under Richard-
son’s command, was assigned the task of exploring the
arctic sea coast by boat from the Mackenzie River
east to the Coppermine River, then traveling overland
on foot from the Coppermine River to Great Bear Lake.
On 18 July, Richardson (1828) records stopping for
breakfast “about eight miles” from the narrow passage
between Cape Bathurst and the Baillie Islands. He
writes, “The air was perfumed by numerous tufts of a
beautiful phlox, and of a still handsomer and very fra-
grant cruciform flower, of a genus hitherto unde-
scribed.” There is little doubt that the “cruciform”
flower Richardson is describing is B. pilosa. First, 18
July is a date that an arctic Braya would be expected
to be in a flowering rather than a fruiting condition. In
addition, the dense clusters of large flowers on his type
specimens would certainly be “handsome,” and Rich-
ardson’s description of the plant’s fragrance and uncer-
tain generic status matches perfectly with Hooker’s
(1830). No other cruciferous species included in Hook-
er’s Flora Boreali-Americana, which treats all of Rich-
ardson’s collections from this expedition, fits Richard-
son’s 18 July plant description as well as B. pilosa.
Richardson collected B. pilosa a second time in
1848, this time when the plant was in fruit. Captain Sir
John Franklin, along with his ships, the Erebus and
Terror, and their crews disappeared in the Canadian
Arctic in 1845. Franklin’s ships carried sufficient pro-
visions to last until the summer of 1848, but by 1847,
when nothing had been heard from Franklin, the British
Admiralty began mounting search expeditions. In 1848,
John Rae and John Richardson were placed in com-
mand of one of these search parties. Richardson’s
orders were to search the arctic coast and islands east
of the Mackenzie River to the Coppermine River and
then travel overland from the Coppermine to Great Bear
Lake, essentially retracing his 1826 journey. Unfortu-
nately, Richardson did not mention his 1848 collection
of B. pilosa in his published account. However, I think
it is likely that this second collection was made at ex-
actly the same place as the first. On 10 August, Rich-
ardson was approaching Cape Bathurst again, twenty-
two years after his first visit there (Richardson 1851).
This is exactly the right season to find Braya in fruit.
Given Hooker’s uncertainty about the generic status
of B. pilosa due to a lack of fruiting material for exam-
ination, it is inconceivable that Richardson would not
have taken the opportunity to revisit his original col-
lection location to collect fruiting plants which would
allow a definitive identification.
Braya pilosa was collected for a third and apparently
last time in August of 1850 from the “arctic coast, W.
of C. Bathurst” by Captain William J. S. Pullen. In
1850, Pullen, also in command of an expedition in
search of Franklin, attempted to travel from Fort Simp-
son on the Mackenzie River to Cape Bathurst and then
on to Banks Island. In mid-August he was in the vicin-
2004 HARRIS: PILOSE BRAYA: AN ENDEMIC OF ARCTIC CANADA 553
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FiGuRE 2: Photograph of mixed collections of Braya pilosa on a herbarium sheet at the Royal Botanic Gardens Herbarium
(K) in Kew, England. Insert is an enlarged view of mature silicles.
554 THE CANADIAN FIELD-NATURALIST Vol. 118
MSW 129°00W 28°45 WBS SC IBMSW «IBOOW «= 1245W O12S0W SC 121BW12P00W Ss 128°45W «126°
Baillie Islands
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FiGuRE 3: Map of Cape Bathurst Peninsula, Northwest Territories, Canada. The dashed box indicates the probable type
locality of Braya pilosa.
ity of Cape Bathurst, but found dramatically different
ice conditions there than Richardson had two years
previously. The pack ice was still so thick that he was
unable to proceed past Cape Bathurst, and was forced
to retreat back to Fort Simpson. On 8 August, Pullen
(1979) recorded that his party “landed in a small bay
about 7 miles from Cape Bathurst” to eat dinner. They
returned to the same bay about midnight on 10 Au-
gust, after having been turned back by the pack ice at
Cape Bathurst, and remained camped there until 15
August while they waited to see if ice conditions at
the Cape might improve. This places Pullen within
one nautical mile of Richardson’s (1828) estimate of
his position when I believe he made his first collection
of B. pilosa, and at the perfect season to find the plant
in fruit. He describes the small bay as being “the only
place where we could conveniently land,” which sug-
gests that it is likely the same place Richardson had
chosen to land for breakfast in 1826 when he discov-
ered the plant. In addition, Pullen’s steersman was Neil
McLeod, a Hudson’s Bay Company employee who had
also accompanied Richardson in 1848. It is probable
that McLeod would have mentioned Richardson’s
interest in the plant to Pullen and perhaps inspired
him to make his own collection during the four days
they were camped at the site.
If Richardson’s and Pullen’s B. pilosa collections
did come from the same location on Cape Bathurst
Peninsula, the position of that location would most
likely be between about 70° 27' and 70° 28' north lat-
itude along the western coast of the peninsula (Figure
3). Or perhaps slightly farther north if their estimates
of the distance to Cape Bathurst were based on the
distance they actually traveled along the coastline
rather than the direct straight-line distance. This section
of coastline should be searched carefully for extant
populations of B. pilosa.
While the rediscovery of B. pilosa would of itself
be interesting botanically and historically, the avail-
ability of living plants for study would also be tremen-
dously valuable to our understanding of Braya. The
evolution of the genus is intimately tied to hybridiza-
tion and polyploidy (Harris 1985), but that phyloge-
netic history is obscured by the fact that diploidy has
never been reported in Braya. There is some evidence,
however, that B. pilosa may be diploid and, therefore,
could have played a critical role in the evolutionary
history of Braya. Ornduff (1969) listed several attrib-
utes in flowering plants that are correlated with xeno-
gamy and a diploid chromosome number. Among them
are rotate corollas with large petals, exserted styles,
scented flowers, abortive fruits, and a narrow distribu-
tion. Braya pilosa has the largest petals and longest
styles of any Braya, it is the only species in the genus
with scented flowers, it appears to have a fairly high
frequency of abortive silicles, and it has a very narrow
2004 HARRIS: PILOSE BRAYA: AN ENDEMIC OF ARCTIC CANADA
SBP)
FIGURE 4: Photograph of Braya pilosa specimen collected on 24 July 2004 (J. G. Harris and D. L. Taylor 3644).
556
distribution. Large, rotate flowers, allogamy, abortive
fruits, and narrow distributions also have been associ-
ated with lower ploidy levels in B. humilis (Harris 1985),
though these are tetraploids rather than diploids.
Pollen measurements also provide evidence that B.
pilosa may be diploid. Rollins (1953) and Bécher (1956)
noted a correlation of ploidy level and pollen size in
B. humilis, with populations of lower ploidy level
having somewhat smaller pollen grains than those of
higher ploidy level. Pollen sizes in B. pilosa, B. thorild-
wulffii, and B. glabella show a similar correlation. Mea-
surements (Harris 1985) indicate that B. pilosa has
significantly smaller pollen grains than the tetraploid
B. thorild-wulffii, with the largest pollen grains being
found in the octoploid B. glabella.
If B. pilosa is indeed diploid, its extremely limited
distribution may be linked to its ploidy level. Favarger
(1961) and Johnson and Packer (1967) found a corre-
lation between plant ploidy level and habitat stability.
Diploids were more likely to be found on stable habi-
tats, while polyploids were more frequent on habitats
with a history of disturbance. Areas that remained
unglaciated during the Pleistocene, for example, were
found to have a significantly higher percentage of
diploids in their floras than areas that were glaciated
(Favarger 1961; Johnson and Packer 1967). The Cape
Bathurst Peninsula is known to have been unglaciated
during the Pleistocene (Prest 1969) and probably served
as a refugium for plants that moved back onto their
former ranges as the ice receded. Braya pilosa likely
weathered the Pleistocene on the relatively stable habi-
tats available near Cape Bathurst, but it has apparently
been unable to expand its range in recent times. It may,
however, have served as a parent species to some of
the more widespread polyploids in the genus. A like-
ly candidate is B. thorild-wulffii, a high arctic North
American endemic that shares B. pilosa’s ovoid-
ellipsoid fruit shape and fenestrate silicle septae, and
appears to be most closely related to it. Braya tho-
rild-wulffii is a tetraploid (2n=28) (Holmen 1952;
Mulligan 1965, 2002; Bocher 1966; Harris 1985),
which is the lowest reported ploidy level in the genus
(some populations of B. humilis are also tetraploid).
However, Boécher (1966) observed that there appears
to be only a single large pair of chromosomes in B.
thorild-wulffii, so it is probably not simply an autote-
traploid from a single diploid parent.
DNA sequence data (Harris, unpublished data) sug-
gest that B. thorild-wulffii may have served as a parent
to other Braya species of higher ploidy level. If DNA
of B. pilosa were available, and if the species is indeed
a parent to B. thorild-wulffii, it could provide signifi-
cant insight into phylogenetic relationships within Braya
and between Braya and other genera in the Cruciferae.
Acknowledgments
I am indebted to C. Stuart Houston for his help with
historical questions about the second Franklin expe-
THE CANADIAN FIELD-NATURALIST
Vol. 118
dition, Ihsan Al-Shehbaz for his helpful discussions
about the taxonomic status of Braya pilosa, and Alvan
Bregman of the Rare Book Collections Library at Uni-
versity of Illinois at Urbana-Champaign for providing
me with transcripts of Richardson’s annotations to his
personal copy of Flora Boreali-Americana. 1 thank
Sam Rushforth, Renée Van Buren, Kimball Harper,
and JaNae Brown Haas for insightful comments on
previous drafts of this paper and Melinda Woolf Har-
ris for her illustrations of Braya pilosa. Finally, | am
indebted to two anonymous reviewers who provided
valuable comments and suggestions.
Addendum
On 24 July 2004, Daniel L. Taylor and I briefly visit-
ed Richardson’s presumed type locality of Braya pilosa
near Cape Bathurst. We discovered several hundred
B. pilosa individuals growing along the coastline on
sandy, calcareous soils in an area heavily used by Cari-
bou (Ranifer taranclus). The plants were limited to
small, bare patches of soil disturbed by Caribou hoofs.
The plants on Cape Bathurst Peninsula (Figure 4)
are perfect matches for Richardson’s and Pullen’s
19" Century B. pilosa collections (Figure 2). Speci-
mens (J. G. Harris and D. L. Taylor 3644) are deposit-
ed in the Utah Valley State College Herbarium (UVSC),
with duplicate material distributed to the following
herbaria: Agriculture and Agri-Food Canada (DAO),
Canadian Museum of Nature (CAN), Missouri Botan-
ical Garden (MO), New York Botanical Garden (NY).
DNA sequencing and cytological studies are currently
underway (Harris, unpublished data).
Documents Cited (marked * in text)
Mulligan, G. A. 2000. Key to the Brassicaceae (Cruciferae)
of Canada and Alaska. Electronic publication on the inter-
net site, http://members.rogers.com/mulligan4520/key/
Murray, D. F. 1983. in sched., Mouth of River Mackenzie,
Richardson s.n., National Herbarium of Canada (CAN)
64149, Ottawa, Ontario.
Scott, P. J., S. G. Aiken, and M. J. Dallwitz. 2001. Brassi-
caceae of the Canadian Arctic Archipelago: descriptions,
illustrations, identification, and information retrieval. Ver-
sion: 29" June 2001. Electronic publication on the internet
site, http://www.mun.ca/biology/delta/arcticf/
Warwick, S. I., A. Francis, and G. A. Mulligan. 2000. Bras-
sicaceae of Canada. Agriculture and Agri-Food Canada,
Ottawa. Electronic publication on the internet site, http://
sis.agr.gc.ca/brd/brass/
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Canada: our natural heritage. Canadian Museum of Nature,
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Bocher, T. W. 1956. Further studies in Braya humilis and
allied species. Meddelelser om Gronland 124 (7): 1-29.
Bocher, T. W. 1966. Experimental and cytological studies
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Selskab 14(7): 1-74.
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Cody, W. J. 1979. Vascular plants of restricted range in the
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Cody, W. J. 2000. Flora of the Yukon Territory, 2™ edition.
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Favager, C. 1961. Sur ?emploi des nombres de chromo-
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Harris, J. G. 1985. A taxonomic revision of the genus Braya
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land, North Greenland. Meddelelser om Gr@nland 128
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tory of Beringia. Pages 245-265. in D. M. Hopkins, Editor.
The Bering land bridge. Stanford University Press, Stan-
ford, California.
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vascular plants in the Northwest Territories. Canadian
Museum of Nature, Ottawa, Syllogeus (73).
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ralized mustards, Brassicaceae (Cruciferae). Canadian
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HARRIS: PILOSE BRAYA: AN ENDEMIC OF ARCTIC CANADA
a5)
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of Canada, Ottawa.
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Received 20 October 2003
Accepted 6 December 2004
New Records of Vascular Plants in the Yukon Territory VI
WILLIAM J. Copy!, CATHERINE E. KENNEDY”, BRUCE BENNETT’, and PHIL CASWELL?
‘Biodiversity, National Program on Environmental Health, Agriculture and Agri-Food Canada, Wm. Saunders Building (49),
Central Experimental Farm, Ottawa, Ontario KIA 0C6 Canada
*Department of Environment, Government of the Yukon, Box 2703, Whitehorse, Yukon Y1A 2C6 Canada
3P. O. Box 91, Roxbury, New York 12474 USA
Cody, William J., Catherine E. Kennedy, Bruce Bennett, and Phil Caswell. 2004. New records of vascular plants in the Yukon
Territory VI. Canadian Field-Naturalist 118(4): 558-578.
Based on field reconnaissance mainly in 2002 in the southern part of the Yukon and particularly in and adjacent to Kluane National
Park, information is provided on geographically significant plant occurrences. Six native taxa, Atriplex alaskensis, Claytonia
megarrhiza, Corispermum ochotense vat. alaskanum, Oxytropis arctica, Polemonium acutiflorum forma lacteum and Polemo-
nium boreale forma albiflorum, and four introduced taxa. Arabis caucasica, Camelina sativa, Senecio eremophilus, and Setaria
viridis are reported new to the known flora of the Yukon Territory. Significant range extensions for 158 native and 21 introduced
taxa are included. Parrya arctica, Armoracia rusticana, Atriplex patula and Papaver nudicaule ssp. nudicaule are excluded
from the Yukon flora.
Key Words: Vascular plants, Yukon Territory, flora, new records, range extensions, phytogeography.
Since the writing of New Records of Vascular Plants
in the Yukon Territory V (Cody et al. 2003), a consider-
able number of plant specimens have been submitted
to Cody for identification and confirmation. The major
submissions include the following locations and col-
lectors: (1) Kluane National Park and vicinity by Phil
Caswell for the National Park Service as part of on-
going botanical inventories; (2) W. J. Cody and Cath-
erine Kennedy spent four days collecting specimens in
the Fort Selkirk area assessing the flora of that region;
(3) W. J. Cody and Margaret Cody studied changed
vegetation along the southern highways; (4) Bruce Ben-
nett conducted studies adjacent to the North Canol
Road, assisting with rare plant surveys for Yukon-
Charley Rivers National Park and interesting areas
while boating down the Yukon River; (5) Rhonda Rosie
visited sites adjacent to Nisling Lake and Morris Lake
for the Yukon Territory Government and Parks Branch;
(6) Stu Withers visited former mine sites at Atlin Lake
and Deadman Creek in connection with reclamation of
vegetation and soil stabilization; (7) with his continuing
interest in vegetation habitats Greg Brunner collected
plant specimens from areas adjacent to the Klondike
River and Dawson City.
This paper serves to further update the Flora of the
Yukon Territory (Cody 1996) and Flora of the Yukon
Territory, Second Edition (Cody 2000) along with other
records recently published (Cody et al. 1998, 2000,
2001, 2002, 2003). The floristic information presented
earlier and updated here is essential for biological re-
search and ongoing work relating to agriculture, fores-
try, sustainable resource management and wildlife
management. With additions of six native and four
introduced species reported here, the flora now includes
1181 species. The new native species are all rare (as
defined by Douglas et al. 1981).
The taxa addressed in the body of this paper appear
in a synoptic list by Yukon status in alphabetical order.
The taxa are then discussed in taxonomic order, as pre-
sented in the Flora of the Yukon Territory with citation
of specimens and other pertinent information. Common
names follow Cody (1996) and Douglas et al. (1998-
2001).
Synoptic List by Yukon Status
Errata in New Records: (5)
Carex stylosa
Douglasia arctica
Poa nemoralis revised to Poa interior
Armoracia rusticana revised to Rorippa barbareifolia
Papaver nudicaule ssp. nudicaule revised to Papaver croceum
Native Taxa New to the Yukon Territory: (6)
Atriplex alaskensis
Claytonia megarrhiza
Corispermum ochotense var. alaskanum
Oxytropis arctica
Polemonium acutiflorum forma lacteum
Polemonium boreale forma albiflorum
Introduced Taxa New to the Yukon Territory: (4)
Arabis caucasica
Camelina sativa
Senecio eremophilus
Setaria viridis
Range Extensions of Native Taxa within the Yukon
Territory: (158)
Agrostis filiculmis
Allium schoenoprasum ssp. sibiricum
Alyssum obovatum
Amelanchier alnifolia
Arabis holboellii var. retrofracta
Arabis holboellii var. secunda
Aster alpinus ssp. vierhapperi
Aster falcatus
558
Atriplex subspicata
Bromus ciliatus
Callitriche anceps
Cardamine bellidifolia
Carex albo-nigra
Carex athrostachya
Carex atrosquama
Carex capillaris ssp. chlorostachys
Carex crawfordii
Carex eleusinoides
Carex foenea
Carex limosa
Carex loliacea
Carex obtusata
Carex pachystachya
Carex pellita
Carex petasata
Carex praegracilis
Carex rossii
Carex supina ssp. spaniocarpa
Carex sychnocephala
Carex viridula
Cassiope tetragona ssp. saximontana
Cerastium arvense
Chamaerhodos erecta ssp. nuttallii
Chenopodium capitatum
Cicuta maculata var. angustifolia
Cryptogramma crispa vat. acrostichoides
Deschampsia brevifolia
Descurainia incisa vat. incisa
Douglasia alaskana
Draba aurea
Draba corymbosa
Draba crassifolia
Draba glabella
Draba nemorosa
Draba ogilviensis
Draba palanderiana
Draba porsildii
Draba stenoloba
Dryas hookeriana
Eleocharis uniglumis
Elymus alaskanus ssp. alaskanus
Elymus glaucus
Elymus macrourus
Elymus spicatus
Elymus trachycaulus ssp. andinus
Erigeron caespitosus
Erigeron hyperboreus
Eriophorum brachyantherum
Eritrichium aretioides
Eritrichium chamissonis
Euphrasia subarctica
Festuca brachyphylla
Festuca richardsonii
Festuca saximontana
Gentianella tenella
Geum aleppicum ssp. strictum
Geum rossii
Glyceria striata var. stricta
Gymnocarpium jessoense ssp. parvulum
Harrimanella stellariana
Hordeum brachyantherum
Tris setosa ssp. interior
Isoetes echinospora
2004 Copy, KENNEDY, BENNETT, AND CASWELL: PLANTS IN YUKON VI 559
Isoetes ?maritima
Juncus bufonius
Juncus filiformis
Kobresia simpliciuscula
Koeleria macrantha
Lepidium densiflorum var. densiflorum
Lupinus nootkatensis
Luzula arcuata ssp. unalaschkensis
Maianthemum canadense ssp. interius
Mertensia paniculata var. alaskana
Mimulus guttatus
Minuartia dawsonensis
Minuartia elegans
Minuartia macrocarpa
Minuartia yukonensis
Montia fontana
Myriophyllum verticillatum
Nuphar polysepalum
Orobanche fasciculata
Oxytropis campestris ssp. varians
Pedicularis oederi
Phacelia mollis
Phlox hoodii
Phyllodoce glanduliflora
Pinguicula villosa
Pinus contorta ssp. latifolia
Plantago canescens
Plantago maritima
Poa interior
Poa leptocoma
Poa secunda
Podistera macounii
Polygonum lapathifolium
Potamogeton alpinus ssp. tenuifolius
Potamogeton berchtoldii
Potamogeton gramineus
Potamogeton pectinatus
Potamogeton praelongus
Potamogeton subsibiricus
Potamogeton zosteriformis
Potentilla arguta var. convallaria
Primula eximia
Puccinellia interior
Pulsatilla ludoviciana
Pyrola minor
Ranunculus aquatilis var. subrigidus
Ranunculus occidentalis var. brevistylis
Rhinanathus minor ssp. borealis
Ribes oxyacanthoides ssp. oxyacanthoides
Rorippa barbareifolia
Rosa woodsii
Salix alaxensis ssp. longistylis
Salix glauca vat. acutifolia
Salix pseudomyrsinites
Salix rotundifolia ssp. dodgeana
Sambucus racemosa ssp. pubens
Saxifraga caespitosa
Saxifraga eschscholtzii
Saxifraga foliolosa
Saxifraga nelsoniana ssp. pacifica
Saxifraga rufopilosa
Saxifraga tricuspidata
Scirpus rollandii
Silene involucrata ssp. tenella
Silene williamsii
560
Solidago canadensis vat. salebrosa
Spiranthes romanzoffiana
Stellaria umbellata
Stipa comata
Stipa nelsonii ssp. dorei
Stipa richardsonii
Subularia aquatica ssp. americana
Tofieldia coccinea
Trientalis europaea
Triglochin palustre
Typha latifolia
Urtica dioica ssp. gracilis
Utricularia minor
Vaccinium membranaceum
Vahlodea atropurpurea
Valeriana sitchensis
Vicia americana
Viola renifolia var. brainerdii
Woodsia alpina
Woodsia ilvensis
Range Extensions of Introduced Taxa within the
Yukon Territory: (21)
Agropyron pectiniforme
Agropyron sibiricum
Agrostis gigantea
Avena sativa
Brassica rapa
Bromus inermis
Capsella bursa-pastoris
Elytrigia intermedia
Galeopsis tetrahit ssp. bifida
Lepidium densiflorum var. macrocarpum
Myosotis scorpioides
Papaver croceum
Poa annua
Rheum rhabarbarum
Rumex crispus
Silene vulgaris
Sinapis arvensis
Sonchus arvensis ssp. uliginosus
Tanacetum vulgare
Thlaspi arvense
Trifolium pratense
Comments on Native Taxa in the Yukon Flora: (3)
Carex stylosa
Douglasia arctica
Isoetes maritima
Deletions of Native Taxa from the Yukon Flora: (1)
Parrya arctica
Deletions of Introduced Taxa from the Yukon Flora:
(3)
Armoracia rusticana
Atriplex patula
Papaver nudicaule ssp. nudicaule
Annotated Species List
ISOETACEAE
Isoetes echinospora Dut., Bristle-like Quillwort —
YUKON: On stony shore of small pond south of Morris
Lake, 60°20°N 131°40°W, R. Rosie 2030, 8 Sept. 1999
(DAO); washed up on lakeshore, northeast shore of
Nisling Lake, 62°02’00"N_ 137°58’30"W, R. Rosie
THE CANADIAN FIELD-NATURALIST
Vol. 118
02-821, 12 Aug. 2002 (DAO) (determined by D. F.
Brunton).
The first specimen cited above is an extension of the
known range in the Territory (Cody 1996) of about 180 kilo-
meters southwest of the vicinity of Francis Lake. The second
specimen is from a site about 500 kilometers northwest of
Frances Lake and about 430 kilometers northwest of the
Morris Lake site.
Isoetes ?maritima Underw., Maritime Quillwort —
YUKON: washed ashore, WNW side of Trout Lake,
68°49°27"N 138°45'8"W, J. M. Line 2000-72, 28 July
2000 (DAO) (determined by D. F. Brunton & D. M.
Britton).
The fragmented specimens found washed up along the
shore of the lake possessed only immature female spores
which were mostly densely tuberculate but could not defi-
nitely be determined as /. maritima. If this could be verified
by more mature specimens from Trout Lake it would be only
the third known location in the Territory and a range exten-
sion of about 260 kilometers northwest of Vittrewka Lake
(Cody et al. 2001).
Isoetes maritima Underw., Maritime Quillwort — It
has been brought to our attention by Lori Schroeder
(Environment Yukon) that specimen data according
to Greg Brunner’s field notebook for his collection
#39-99 which was published in Cody et al. (2001)
should be: Peel River Wetland Study Turner Lake,
66°11'N 134°14'W, 2 July 1999.
PTERIDACEAE
Cryptogramma crispa (L.) R. Br. var. acrostichoides
(R. Br.) C. B. Clarke, Mountain-parsley — YUKON:
Kluane National Park, south-facing scree slope,
60°06.019'N 137°08.532'W, P. Caswell 026, 6 June
2002 (DAO).
This rare species which was previously known from only
six localities in the Territory is now known from two sites in
southern Kluane National Park.
ASPIDIACEAE
Gymnocarpium jessoense (Koidz.) Koidz. ssp. parvu-
lum Sarvela, Nahanni Oak Fern — YUKON: dry rock out-
crop, lower Beaver River, 60°09'09"N 124°55'16"W,
B. Bennett 97-518, 19 Aug. 1997 (B. Bennett Herbar-
ium, photo DAO).
The specimen cited above of this rare plant in the
Territory is an extension of the known range of about
300 kilometers from a site in the vicinity of Francis
Lake (Cody 1996).
Woodsia alpina (Bolton) S. F. Gray, Northern Woodsia —
YUKON: damp organic soil in rock crevice, Cache Lake,
Kluane National Park, 61°12.586'N 139°03.671'W, P.
Caswell 575, 24 July 2002 (DAO).
The specimen cited above is an extension of the known
range in the Territory of about 45 kilometers southwest of a
site at the north end of Kluane Lake and is new to the flora
of Kluane National Park.
Woodsia ilvensis (L.) R. Br., Rusty Woodsia — YUKON:
steep south-facing bluffs along Klondike River, Dawson
Area, | mile north of 64°02'N 137°41'30"W, G.
Brunner 435, 2 June 2001 (DAO); dry rocky outcrop,
2004
S Fork bluffs, Klondike River, 64°O1'N 138°9'W, G.
Brunner 443-01, 14 July 2001 (DAO).
Douglas et al. (1981) considered this species rare in the
Territory. The specimens cited above are from sites about
60 kilometers southwest of a site adjacent to the Dempster
Highway mapped by Cody (1996).
PINACEAE
Pinus contorta Doug}. ex Loud. ssp. latifolia Engelm.
ex S. Wats., Lodgepole Pine — YUKON: roadside, North
Canol Road KM 284, 62°13'02"N 131°46'10"W, B.
Bennett 02-723, 22 Sept. 2002 (DAO); roadside across
road from large truck dump, North Canol Road Km
380, 62°50'03"N 130°56'24"W, B. Bennett 02-724,
21 Sept. 2002 (DAO).
The specimens cited above are an extension of the known
range in the Territory of about 175 kilometers northeast of a
site adjacent to the South Canol Road. The second specimen
was from a site adjacent to an old house and may have been
planted.
TYPHACEAE
Typha latifolia L., Common Cattail — YUKON: border
of small lake below swimming pool, Takhini Hot
Spring, 60°52'40.7"N 135°21'30.6"W, Cody & Cody
37692, 10 Aug. 2001 (DAO); same locality (fruiting)
Cody 35311, 4 Aug. 2002 (DAO).
Douglas et al. (1981) considered this species rare in the
Territory. Cody (1996) knew it only from the vicinity of
Mayo. Cody et al. (2000, 2001) added additional sites in the
extreme southeast and in the vicinity of Faro. The specimen
cited above which was collected just west of Whitehorse is
now from the fourth site in the Territory.
POTAMOGETONACEAE
Potamogeton alpinus Balbis ssp. tenuifolius (Raf.)
Hultén — YUKON: plant fragments washed ashore, Trout
Lake, 68°50'N 138°45'W, J. M. Line 2000-9, 29 July
2000 (DAO).
The specimen cited above is the northernmost yet found
in the Territory. It is an extension of the known range (Cody
1996) of about 85 kilometers NE of a site north of latitude
68°N.
Potamogeton berchtoldii Fieb. — YUKON: shallow
water of small lake, west side of Dempster Highway
Km 93, 64°39'01"N 138°23'01"W, Cody & Cody
38060, 27 July 2002 (DAO).
The specimen cited above is from a site about 80 kilo-
meters northeast of Dawson City. To the north a single site
was previously known from adjacent to the Peel River (Cody
1996).
Potamogeton gramineus L., Variable-leaved Pondweed
— YUKON: slough off Yukon River with old sunken
dredge, 61°56'35"N 135°12'17"W, B. Bennett 02-299,
7 Aug. 2002 (DAO).
The nearest site to that listed above known to Cody (1996)
is about 75 kilometers to the north.
Potamogeton pectinatus L., Sago Pondweed — YUKON:
shallow backwater, Dezadeash River, Kluane National
Park, 60°45.683'N 137°36.010'W, P. Caswell S05, 16
Aug. 2002 (DAO); locally common in mucky alka-
Copy, KENNEDY, BENNETT, AND CASWELL: PLANTS IN YUKON VI
56]
line pond, Mile 985 Alaska Highway, 60°48'N
136°45'W, Calder & Kukkonen 28277, 14 Aug. 1960
(DAO).
The specimens cited above extend the known range in the
Territory about 120 kilometers west of the vicinity of White-
horse. The Caswell specimen is the first known from Kluane
National Park.
Potamogeton praelongus Wulf., White-stemmed
Pondweed — YUKON: Enoch Lake, Old Crow Flats,
68°05'00"N_ 140°09'50"W, B. Bennett 95-413, 10
Aug. 1995 (B. Bennett Herbarium, photo DAO);
plant fragments washed ashore, Trout Lake, 68°50'N
138°45'W, J. M. Line 2000-140, 28 July 2000 (DAO);
Nordenskiold River wetland pond, M. Dennington,
Nord #23, 19 July 1984 (B. Bennett Herbarium, photo
DAO).
Douglas et al. (1981) considered this species rare in the
Yukon Territory based on specimens from only two locations.
Cody (1996) knew it from five locations. Cody et al. (2000)
added three locations. The first specimen cited above is a
northwestward extension of about 40 kilometers from the
vicinity of Old Crow. The second specimen from about 115
kilometers NNE of Old Crow is the northernmost yet found
in the Territory. The third specimen is an extension of the
known range in the south of about 125 kilometers northwest
of a site just north of Whitehorse.
Potamogeton subsibiricus Hagstr. - YUKON: growing
in about 3 feet of water, lake west of Dempster Rd.
near mile 65, R. T: Porsild 317, 25 July 1966 (AKA,
photo DAO) (determined by A. Batten).
Cody (1996) knew this rare species in the Territory from
a single collection from adjacent to the North Canol Road
about 450 kilometers to the southeast of the locality cited
above.
Potamogeton zosteriformis Fern., Flatstemmed Pond-
weed — YUKON: in water by outlet of pond, Pumphouse
Pond, 3 km S of Alaska Highway, 60°43'31.3"N
135°09'58.3"W, W. J. Cody 38290, 3 Aug. 2002
(DAO).
Cody (1996) knew this rare species in the Territory from
only two localities, one southeast of Haines Junction and one
just north of 64°N. Cody et al. (1998, 2000 and 2001) added
two sites in the south and one north of 68°N.
SCHEUCHZERIACEAE
Triglochin palustre L., Marsh Arrow-grass — YUKON:
silty river bank with Carex utriculata, C. aquatilis
and Juncus alpinoarticulatus, Selwyn, Yukon River,
62°48'06"N 138°15'29"W, B. Bennett 02-294, 9 Aug.
2002 (DAO).
The specimen cited above is between sites adjacent to
the Alaska Highway, Klondike Highway and Dawson City.
POACEAE (GRAMINEAE)
Agropyron pectiniforme R. & S., Crested Wheat
Grass — YUKON: lake shore, Earn Lake, 62°.9'08.3"N
134°23'07.6"W, G. Brunner 557-01, 5 Aug. 2001
(DAO); steep stony slope on east side of highway,
Haines Highway, 60°6'3.2"N 136°54'51"W, Cody &
Cody 37911, 21 July 2002 (DAO).
562
The first specimen of this introduced species cited above
is from a site between the northernmost mapped by Cody
(1996) in the vicinity of Mayo and a site adjacent to Faro.
The second specimen cited above is an extension of the
known range in the Territory of about 85 kilometers south-
east of a site in the vicinity of Haines Junction.
Agropyron sibiricum (Willd.) P. Beauv. — YUKON: top of
bank overlooking road into gravel pit south of Alaska
Highway, 60°49'58"N 135°45'49"W, Cody & Cody
38210, 1 Aug. 2002 (DAO).
Cody (1996) knew this introduced species in the Territory
only from two locations, Whitehorse and Carmacks. A third
site was reported from the vicinity of Ross River (Cody et al.
2003). The specimen cited above is from a site about 40 kilo-
meters west of Whitehorse.
Agrostis filiculmis M. E. Jones — YUKON: open area —
abandoned placer mine, Mechanic Creek, 62°20.1'N
137°21.5'W, S. Withers SWOI-062, 6 July 2001 (DAO).
The specimen cited above is only the second known in the
Territory (Cody 1996) and is from a site about 200 kilometers
southeast of the first site in the vicinity of Dawson City.
Agrostis gigantea Roth., Creeping Bent Grass —
YUKON: Spruce Hill Park, border of playground at
head of Engelman Drive, Whitehorse, 60°36'40.3"N
134°55'08.8"W, W. J. Cody 37743, 14 July 2002
(DAO).
Cody (1996) knew this introduced species in the Territory
from only two localities, Dawson City and Carmacks. An
additional collection from a mine site east of Dawson City
was reported by Cody et al. (2003). The specimen cited above
is from only the fourth known locality in the Territory.
Avena sativa L., Oats — YUKON: scattered in grass area
around Beringia Museum, Whitehorse, 60°42'36"N
135°4'45"W, Cody & Cody 38105, 30 July 2002
(DAO).
Cody (1996) knew this introduced species from only wide-
ly separated sites in the Territory, vicinity of Mayo, middle
of North Canol Road and east of Watson Lake.
Bromus ciliatus L. — YUKON: in moist moss on moun-
tain slope above treeline on east side of Dempster
Highway about 9 kilometers north of Tombstone Park
Campsite, 64°34'49"N 138°15'30"W, Cody & Cody
38047, 26 July 2002 (DAO).
The specimen cited above is at the northern limit of this
species in the Territory (Cody 1996). The nearest sites previ-
ously mapped were about 120 kilometers to the west adjacent
to the Yukon River and about 150 kilometers to the southeast
in the vicinity of Stewart Crossing. This species was con-
sidered rare in the Territory by Douglas et al. (1981).
Bromus inermis Leyss., Smooth Brome — YUKON:
sand beach, Kusawa Lake Campground, 60°5'10"N
136°8'42"W, Cody & Cody 38144, 31 July 2002
(DAO); gravel ditch between road and steep gravel
slope, Haines Highway, 60°6'3.3"N 136°54'51"W,
Cody & Cody 37912, 21 July 2002 (DAO).
The specimens cited above of this introduced species
which are from sites about 100 kilometers southeast of Haines
Junction and southwest of Whitehorse, are the most south-
western yet found in the Territory.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Deschampsia brevifolia R. Br. — YUKON: flats 7 miles
east of Tagish Bridge, 60°19'5"N 134°10'17"W, Cody
& Cody 37940, 23 July 2002 (DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 90 kilometers
southeast of a site west of Whitehorse.
Elymus alaskanus (Scribn. & Merr.) A. Léve ssp.
alaskanus — YUKON: in sandy soil of river bank, Nis-
utlin River Delta National Wildlife Area, 60°11'N
132°35'W, B. Bennett 98-167, 26 July 1998 (DAO).
The specimen cited above is an extension of the known
range in the Territory of about 180 kilometers south of a site
adjacent to the northern South Canol Road.
Elymus glaucus Buckl., Western Rye Grass — YUKON:
roadstop in disturbed gravelly soil, Atlin Road just
north of BC border, 60°00'09"N 133°47'42.1"W,
Cody & Cody 37547, 28 July 2001 (DAO)
Douglas et al. (1981) considered this species rare in the
Territory. The specimen cited above 1s an extension of about
115 kilometers southeast of a site adjacent to Whitehorse
reported by Cody et al. (2002).
Elymus macrourus (Turcez.) Tzvelev — YUKON: grow-
ing in loose sand on riverbar, Wind River, camp #6,
65°40.46'N 135°11.76'W, B. Bennett 00-853, 7 July
2000 (B. Bennett Herbarium, photo DAO); exposed
sandy lakeshore, north end of Atlin Lake, 60°01.5'N
133°50.4'W, S. Withers SWO1-045, 30 June 2001
(DAO).
The first specimen of this Amphi-Beringian species cited
above is the first known from between latitudes 64°N and
66°N east of the Dempster Highway. The second specimen
is an extension of the known range in the Territory of about
200 kilometers southwest of a site east of Haines Junction.
Elymus spicatus (Pursh) Gould — YUKON: common at
base of large talus slope, Yukon River, Brittania Creek,
62°52'28"N 138°42'56"W, B. Bennett 02-641, 10 Aug.
2002 (DAO).
Cody (1996) knew this species in the southwest of the Ter-
ritory and disjunct to the extreme northwest. The specimen
cited above is an extension of the known range in the
Territory of about 85 kilometers west of longitude 137°W.
Elymus trachycaulus (Link) Gould ex Shinners ssp.
andinus (Scribn. & Smith) A. & D. Léve — YUKON:
gravel roadside, Top of the World Highway Km 16,
64°6'6"N 139°38'41"W, Cody & Cody 38035, 38037,
26 July 2002 (DAO); gravel roadside, Top of the World
Highway Km 102, 64°05'33"N 140°55'22"W, Cody
& Cody 38003, 26 July 2002 (DAO).
The specimens cited above extend the known range in the
Territory to the west about 140 kilometers from a site east of
the Dempster Highway.
Festuca brachyphylla Schultes & Schultes f., Short-
leaf Fescue — YUKON: Site KPL #106, 62°17'38.7"N
137°48'25"W, G. Brunner 578-01, July 2001 (DAO).
The specimen cited above is from a site between sites
mapped by Cody (1996) west of Carmacks and adjacent to
southern Dempster Highway.
2004
Festuca richardsonii Hooker — YUKON: beside test plot,
| km N of Montague Roadhouse, Km 132 Klondike
Highway, 61°48'35"N_ 136°7'52"W, Cody & Cody
38082, 28 July 2002 (DAO).
This species is frequent in the southern part of the Terri-
tory west of longitude 137°W and north of latitude 64°N
but has not previously been found adjacent to the Klondike
Highway.
Festuca saximontana Rydb., Rocky Mountain Fescue
— YUKON: gravel beside road, Alaska Highway 8 km
west of White River, 62°3'15.6"N 140°38'20.5"W,
Cody & Cody 37886, 37887, 20 July 2002 (DAO).
The specimens cited above are an extension of the known
range in the Territory of about 100 kilometers northwest of
a site just northwest of Kluane Lake.
Glyceria striata (Lam.) Hitche. var. stricta (Scribn.)
Fern., Fowl Marina Grass — YUKON: moist muddy
organic soil, along road from Dalton Post to Wade
Lakes, 60°07.765'N 137°04.105'W, P. Caswell 650, 4
Aug. 2002 (DAO).
This plant was considered rare in the Territory by Douglas
et al. (1981). Cody (1996) knew it only in the southeast as
far west as just west of Watson Lake. The specimen cited
above from between the Haines Highway and Kluane Na-
tional Park is from a site about 450 kilometers to the west.
It is however known from British Columbia.
Hordeum brachyantherum Nevski — YUKON: disturbed
area in townsite, Big Salmon Village at confluence of
Yukon River, 61°53'N 134°55'W, B. Bennett 02-292,
7 Aug. 2002 (DAO).
Cody (1996) considered this species to be introduced at
Dawson City but native and rare at Carcross. Sites in the
vicinity of Whitehorse (Cody et al. 2001) were considered
to be introduced. The specimen cited above was probably
also introduced.
Koeleria macrantha (Ledeb.) Schultes, June Grass —
YUKON: south aspect-xeric-sage/graminoid-forbs of
low compact growth, Site YPC103 near confluence of
Pelly and Yukon rivers, 62°48'16"N 137°19'35.9"W,
G. Brunner 536-01, 3 Aug. 2001 (DAO) (determined
by S. Darbyshire); gravel pit just north of the Alaska
Highway, Silver City Road, 61°01'22"N 138°19'52"W,
B. Bennett 01-005, 29 Apr. 2001 (DAO); lower slope
south-facing, dry, Five Fingers Coal Mine, Yukon River,
62°12'21"N 136°20'10"W, B. Bennett 02-295, 8 Aug.
2002 (DAO).
Douglas et al. (1981) considered this species rare in the Ter-
ritory. The first specimen cited above was collected just south-
west of the Pelly River Ranch at 62°50'20"N 137°11'40"W
by M. Johansen in 1989 (DAO) (Cody 1996); the second
specimen is an extension of about 60 kilometers northwest
of a site adjacent to Haines Junction; the third specimen is
from a site about 40 kilometers southeast of a site near Minto
(Cody 1996).
Poa annua L., Annual Blue Grass — YUKON: vicinity of
campground, Rancheria, at mile 710 Alaska Highway
(60°0S'N 130°36'W), S. L. Welsh & G. Moore 7539,
29 June 1968 (AKA, photo DAO) (determined by R.
J. Soreng).
Copy, KENNEDY, BENNETT, AND CASWELL: PLANTS IN YUKON VI
563
Cody (1996) knew this introduced species from only five
sites in the Territory. The specimen cited above is about 100
kilometers west of a site adjacent to the southern Canol Road.
Poa interior Rydb. (P. nemoralis sensu Cody 1996) —
YUKON: in subalpine meadow, Onion Lake, ca. 46 mi
S of Haines Junction, G. W. & G. G. Douglas 7089,
12 Aug. 1973 (AKA, photo DAO) (determined by R.
J. Soreng); common on steep, open, west-facing prairie
slopes, Conglomerate Mountain on Dawson-White-
horse road, 61°38'N 135°53'W, Calder & Gillett
25770, 22 June 1960 (DAO); common on south-facing,
prairie slope with scattered aspen, Mile 30 on road to
Dawson from Stewart Crossing, 63°33'N 137°25'W,
Calder & Gillett 25037, 4 June 1960 (DAO); grown on
open southern slope, Pelly Ranch (ca. 62°49'N
136°34'W), J. Y. Tsukamoto s.n., 23 July 1960 (DAO);
silt bluff, south-facing, on Porcupine River, 1.5 km
upstream from junction between Rat Indian Creek
and Porcupine River, 67°34'N 138°21'W L. Cwyner
977, 22 July 1976 (DAO) (determined by M. Bark-
worth); dry open exposed gravel ridge overlooking delta,
west side of river on ridge campsite, Lower Blow
River Delta, 69°53'N 137°10'W, H. L. Dickson & D.
L. Allen 5324, 26 July 1982 (DAO); open meadow-
abandoned beaver pond, Deadman Creek, 60°20.2'N
133°03.5'W, S. Withers SWO1-126, 16 July 2001 (DAO)
(determined by S. Darbyshire). ;
Yukon specimens previously mapped as Poa nemoralis
by Cody (1996) have been revised to P. interior. In addition,
the specimens cited above which were inadvertently missed
have now been mapped. (See new map Figure 1).
Poa interior
FiGurE 1. New distribution map for Poa interior in the Yukon
Territory.
564
Poa leptocoma Trin. — YUKON: steep gravelly slope
adjacent to Alaska Highway 3 km east of Snag Junc-
tion, 62°12'42.3"N 140°41'33.1"W, Cody & Cody
37863, 20 July 2002 (DAO).
The specimen cited above is an extension of the known
range in the Territory of about 175 kilometers northwest of
a site in Kluane National Park.
Poa secunda Presl, Sandberg Bluegrass — YUKON:
commonly found growing on the base of the bluff and
occasionally on midslope, Minto Bluff, 62°36'18"N
136°51'06"W, B. Bennett 02-013, 9 June 2002 (DAO).
The specimen cited above is an extension of about 175 kilo-
meters northwest of a site north of Whitehorse (Cody 1996).
To the north the only other site in the Territory is in the vicin-
ity of Dawson City.
Puccinellia interior Th. Sor. — YUKON: gravel roadside,
Top of the World Highway Km 102, 64°05'33"N
140°55'22"W, Cody & Cody 38002, 26 July 2002
(DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 75 kilometers
west from the vicinity of Dawson City.
Setaria viridis (L.) Beauv., Green Bristlegrass (Fig-
ure 2) — YUKON: in crack at edge of Extra Foods park-
ing lot, downtown Whitehorse, B. Bennett 95-437, 14
Oct. 1988 (B. Bennett Herbarium, photo DAO).
The specimen cited above is a new introduction to the
Flora of the Yukon Territory (Cody 1996). This species which
is introduced from Eurasia is known across Canada from
Newfoundland to British Columbia and has been found at
Fort Simpson in the Northwest Territories. The genus Setaria
can be separated from the genus Panicum as follows:
A. Spikelet surrounded by 1|-many distinct or
more or less connate bristles, these
forming aninvolucre eaters ce ee ee Setaria
B. Spikelet not subtended by bristles
Stipa comata Trin. & Rupr., Needle-and-thread —
YUKON: 45° silty sand south-facing slope with Arte-
mesia frigida and Calamagrostis purpurascens, Dutch
Bluff, Yukon River, 61°55'N 135°03.99'W, B. Bennett
02-289, 7 Aug. 2002 (DAO).
Cody (1996) knew this species in the Territory from only
four sites south of 63°N. Cody et al. (2003) added an addi-
tional site just east of Haines Junction. The specimen cited
above is from a site about 60 kilometers southeast of Car-
macks.
Stipa nelsonii Scribn. ssp. dorei Barkworth & Maze
— YUKON: treeless rocky slope overlooking lake,
Snafu Lake Camp Site, 60°08'10"N 133°48'23.6"W,
Cody & Cody 37567, 28 July 2001 (DAO); open area
adjacent to Populus tremuloides woodland overlook-
ing lake, 7 km east of Tagish Bridge, 60°19'5"N
134°10'17"W, Cody & Cody 37938, 23 July 2002
(DAO).
Cody (1996) knew this species from only six sites in the
Territory north to about latitude 61°N. Cody et al. (2001)
added an additional site in the vicinity of the Carcross Dunes.
The specimens cited above are from east and southeast of
the Carcross Dunes site.
THE CANADIAN FIELD-NATURALIST
Vol. 118
FIGURE 2. Setaria viridis, Green Bristlegrass (drawn by Lee
Mennell).
Stipa richardsonii Link (Achnatherum richardsonii
(Link) Barkw.), Spreading Needlegrass — YUKON: on
steep slope found on lower and mid-slope with Arabis,
Arctostaphylos uva-ursi, Festuca saximontana and Poa,
hill across Tagish Road from Crag Lake, 60°15'30"N
134°28'53"W, B. Bennett 01-008, 19 May 2001 (DAO);
summit of hill behind Carcross Cutoff, south-facing,
pine forest Cowley Creek, 60°35.66'N 134°52.96'W,
B. Bennett 99-300, 6 Aug. 1999 (DAO).
Douglas et al. (1981) knew this rare species in the Territory
from only one locality from adjacent to the Alaska Highway
just east of the Atlin Road junction (Calder & Gillett 26477,
DAO). Cody (1996) mapped three additional sites in the vicin-
ity of Whitehorse. The first specimen cited above is the sou-
thernmost yet found in the Territory.
Vahlodea atropurpurea (Wahlenb.) Fries, Mountain
Hairgrass — YUKON: Site YPN 120, 63°06'39.8"N
133°20'15"W, G. Brunner 568-01, 6 Aug. 2001 (DAO).
Cody (1996) knew this taxon from only six localities:
adjacent to the North Canol Road, adjacent to the South
Macmillan River and near Bennett Lake. Additional sites
have since been found east of the Canol Road (Cody et al.
1998 and 2000). The specimen cited above is from a site
about 50 kilometers northeast of the Macmillan River site.
CYPERACEAE
Carex albo-nigra Mack., Two-toned Sedge — YUKON:
Volcano Mountain, 62°55'N 137°23'W, G. Brunner
521-01, 3 Aug. 2001 (DAO); moist scree with organic
component on north-facing slope, Vulcan Mountain,
Kluane National Park, 60°54.712'N 138°29.484'W, P.
2004
Caswell 527, 15 July 2002 (DAO); moist organic
soil on southwest facing slope on old semi-abandoned
road north of Donjek River bridge, 61°42.209'N
139°48.376'W, P. Caswell 196, 25 June 2002 (DAO).
Cody (1996) knew this rare species in the Territory from
seven localities south of latitude 63°N, three of which were
in Kluane National Park. The first specimen cited above is
the northernmost yet found in the Territory. Cody et al. (2000)
added another site south of Ross River and Cody et al.
(2001) another site in the extreme southeast.
Carex athrostachya Olney — YUKON: moist soil by
lake, Five Mile Lake Campground, 5 km N of Mayo,
63°39'11.1"N 135°53'14.2"W, Cody & Cody 37641,
1 Aug. 2001 (DAO).
Douglas et al. (1981) considered this species rare in the
Territory on the basis of a specimen collected by R. T. Porsild
on the shores of a small bog pond in the vicinity of Mayo,
63°37'N 135°55'W, on 12 May 1967 (Porsild 1975). The
specimen cited above: from nearby is only the second yet
found in the Territory.
Carex atrosquama Mack. — YUKON: steep gravelly
slope adjacent to the Alaska Highway 3 km east of
Snag Junction, 62°12'42.3"N 140°41'33.1"W, Cody
& Cody 37861, 20 July 2002 (DAO); cleared gravel
by highway, Top of the World Highway Km 92,
64°6'6"N 140°46'47"W, Cody & Cody 38024, 26 July
2002 (DAO).
The first specimen cited above is an extension of the known
range in the Territory about 190 kilometers northwest from the
south end of Kluane Lake (Cody 1996) and the second spec-
imen is an extension of the known range of about 100 kilo-
meters west of the Dempster Highway.
Carex capillaris L. ssp. chlorostachys (Steven) Love
et al. — YUKON: Klondike River near mouth of Little
Klondike, 64°02'00"N 137°41'30"W, G. Brunner
440, 3 July 2001 (DAO).
The specimen cited above is the first known to Cody (1996)
between latitudes 64°N and 66°N east of the Dempster High-
way. It is an extension of about 60 kilometers northeast of a
site southwest of the south end of the Dempster Highway.
Carex crawfordii Fern. — YUKON: sandy lake shore,
Kusawa Lake, 60°34'59.2"N 136°08'26.5"W, W. J.
Cody 37718, 13 July 2002 (DAO); meadow adjacent
to RCMP foundation, Fort Selkirk, 62°46'34.4"N
137°23'35.9"W, Cody & Kennedy 37749A, 16 July
2002 (DAO).
This species was considered rare in the Territory by Doug-
las et al. (1981). The specimen from south of Whitehorse
cited above is an extension of the known range in the Terri-
tory of about 250 kilometers south of a site mapped by Cody
(1996) from adjacent to the Pelly River. The second specimen
is from about 85 kilometers west of a site adjacent to the
Pelly River.
Carex eleusinoides Turcz. — YUKON: moist organic
soil with pumice component, down old road west of
Alaska Highway north of Donjek River bridge,
61°42.209'N 139°48.376'W, P. Caswell 205, 2 June
2002 (DAO); gravelly silt near water line, Klondike
River, 64°O1'N 137°51'W, G. Brunner 546, 8 July
Copy, KENNEDY, BENNETT, AND CASWELL: PLANTS IN YUKON VI
565
2001 (DAO); approximately 2 miles downstream
from O’Brian Creek on Klondike River, 64°01'46"N
38°01'00"W, G. Brunner 547, 15 July 2001 (DAO).
This species was considered rare in the Territory by Doug-
las et al. (1981). The first specimen cited above is an extension
of the range known to Cody (1996) of about 50 kilometers
northwest of the north end of Kluane Lake. The second and
third specimens are the first known between latitudes 64°N
and 66°N east of the Dempster Highway and are an extension
of about 45 kilometers northeast of a site south of the south
end of the Dempster Highway.
Carex foenea Willd. — YUKON: Halfway between Order-
ly House and Robert Luke Cabin, 62°46'34.4"N
137°23'35.9"W, Cody & Kennedy 37773, 17 July
2002 (DAO).
Douglas et al. (1981) considered this species rare in the
Territory. Cody (1996) knew it only from three sites, two of
which were in the vicinity of Pelly Crossing. The specimen
cited above came from the same area. Cody et al. (1998) re-
ported an additional site in the vicinity of Beaver Ridge/
Larsen Creek.
Carex limosa L. — YUKON: Sphagnum bog, 64°02'N
137°41'W, G. Brunner 441, 3 July 2001 (DAO).
The specimen cited above is only the second known
between latitudes 64°N and 66°N east of the Dempster High-
way (Cody 1996).
Carex loliacea L. — Yukon: damp silty ground, forest
Picea mariana, Poa glauca, Alnus incana, Salix sp.,
north side of Klondike River near Parker Creek,
64°OI'N 137°51'W, G. Brunner 592, 9 July 2001
(DAO); spring alongside road, gravelly, Big Gold
Creek/60 Mile River Valley, 64°01'N 140°42'W, G.
Brunner 116, 23 July 1991 (DAO).
Cody (1996) considered this species uncommon in the
Territory although mapped north to the Porcupine River.
The specimens cited above are about equally distant east
and west of Dawson City.
Carex obtusata Lilj., Blunt Sedge — YUKON: British
Mountains, 69°26'N 140°07'W, A. Martell 625, 12 July
1979 (DAO); steep south-facing bluffs along Klondike
River, | mile north of 64°02'00"N 137°41'30"W, G.
Brunner 432, 2 June 2001 (DAO).
The first specimen cited above is the northernmost yet
found in the Territory (Cody 1996). It is an extension of the
known range of about 80 kilometers northwest from sites
adjacent to the Babbage River. The second specimen cited
above is an extension of the known range in the Territory of
about 75 kilometers southeast of a site at Sheep Mountain
adjacent to the Dempster Highway (Kojima and Brooke
1985).
Carex pachystachya Cham. — YUKON: open meadow,
abandoned beaver pond, Deadman Creek, S. Withers
SWO1-117, 16 July 2002 (B. Bennett Herbarium, photo
DAO) (determined by A. A. Reznicek).
This species was not included in The Rare Vascular
Plants of the Yukon (Douglas et al. 1981) because it was
widespread in Canada. Cody (1996) knew it from only two
localities in the extreme southern Yukon. The specimen
cited above is from a site about 25 kilometers south south-
east of Whitehorse.
566
Carex pellita Muhl. ex Willd. — YUKON: silty river
bank with Carex utriculata, C. aquatilis, and Juncus
alpinoarticulatus, Selwyn, Yukon River, 62°48'06"N
138°15'29"W, B. Bennett 02-293, 9 Aug. 2002 (DAO);
silty mud at edge of river at high water line with Juncus
alpinoarticulatus, Brittania Creek, Yukon River,
62°52'28"N 138°42'52"W, B. Bennett 02-671, 10
Aug. 2002 (DAO); silty mud at edge of river at high
water line with Juncus alpinoarticulatus, Kirkman
Creek, Yukon’ River, (62°59'21;N«.139°23'07" W)) B.
Bennett 02-675, 10 Aug. 2002 (DAO); river bank in
area frequently scoured by river ice, confluence of 12
Mile River, Yukon River, 64°15'11"N 139°43'18"W,
B. Bennett 02-806, 23 Aug. 2002 (DAO); deeply
rooted, edge of river in silty sand bank, Yukon River,
64°33'28"N 140°38'24"W, B. Bennett 02-807, 24
Aug. 2002 (DAO).
Cody et al. (2000) reported this plant as a rare species in
the Territory based on a specimen from a site below Rink
Rapids adjacent to the Yukon River. An additional site was
reported from Ear Lake, Whitehorse (Cody et al. 2002). The
five sites reported above extend the known range in the Terri-
tory about 275 kilometers northwest of the Rink Rapids.
Bruce Bennett has found that Carex pellita is a common
species on the Yukon River between Pink Rapids and White
River, less common but can be found downstream and even-
tually being replaced by C. saxatilis.
Carex petasata Dewey — YUKON: east slope adjacent
to Alaska Highway ca. 3 km W of Enger Creek,
62°19'12.05"N 140°49'19.9"W, Cody & Cody 37511,
25 July 2001 (DAO); open, abandoned mine road
surface, Viceroy Mine — Big Rock Zone, 64°02'N
138°17.9"W, S. Withers SWO1-057, 3 July 2002 (DAO).
The first specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 215 kilometers
west of a site west of Carmacks and 245 kilometers northwest
of a site adjacent to Haines Junction. The second specimen
cited above is at the northern limit in the Territory about 50
kilometers east of a site in the vicinity of Dawson City.
Carex praegracilis Boott — YUKON: meadow adjacent
to RCMP foundation, Fort Selkirk, 62°46'34.4"N
137°23'35.9"W, Cody & Kennedy 37770B, 17 July
2002 (DAO); sandy lake shore, Kusawa Lake,
60°34'59.2"N 135°08'26.5"W, W. J. Cody 37717, 13
July 2002 (DAO).
Douglas et al. (1981) knew this rare species in the Terri-
tory from only three localities: Mackintosh, Whitehorse and
Carcross. Cody (1996) knew it from 11 sites in the Territory,
most of which were south of latitude 61°15'N. The second
specimen cited above is a slight extension of range south of
Whitehorse.
Carex rossii R. Br., Ross’ Sedge — YUKON: decom-
posed bedrock, South Fork bluffs, Klondike River,
64°O1'N 138°9'W, G. Brunner 446-01, 14 July 2001
(DAO); steep south-facing bluffs along Klondike River
1 mile north of 64°02'N 137°41'30"W, G. Brunner
433, 2 June 2001 (DAO).
The specimens cited above are only the third and fourth
collections known from north of latitude 64°N (Cody 1996)
THE CANADIAN FIELD-NATURALIST
Vol. 118
which are from about 80 kilometers east of a site adjacent to
Dawson. To the south, the nearest known site is adjacent to
the northern South Canol Road about 300 kilometers to the
southeast.
Carex stylosa C. A. Mey. — Cody et al. (2000) reported
this species which is rare in the Yukon Territory from
the Arctic Coast.
The specimen on which it was based (Hoefs & Smitts
93-37) was misidentified and the range extension should be
deleted. There was also an error in the citation where the
latitude should have been 69°23'N not 60°29'N
Carex supina Wahl. ssp. spaniocarpa (Steud.) Hultén
— YUKON: Steep south-facing bluffs along Klondike
River | mile north of 64°02'N 137°41'30"W, G. Brun-
ner 434, 2 June 2001 (DAO).
The specimen cited above is the first known in the Territory
north of 64°N east of the Dempster Highway. The nearest
known site is about 75 kilometers to the northwest cited by
Kojima & Brooke (1985).
Carex sychnocephala Carey — YUKON: damp, fine
gravel with organic component, at base of highway
embankment, Alaska Highway just north of Copper
Joe Creek, 61°19.814'N 138°56.805'W, P. Caswell
570, 21 July 2002 (DAO).
Douglas et al. (1981) considered this species rare in the
Territory. The specimen cited above is an extension of the
range known to Cody (1996) of about 175 kilometers north-
west by west of a site west of Whitehorse.
Carex viridula Michx. — YUKON: on moist shoreline
of Nares Lake south of Carcross, 60°9'20"N
134°40'1L0"W, W. J. Cody 38318, 1 Aug. 2001 (DAO).
This species was considered rare in the Territory by Doug-
las et al. (1981). The specimen cited above is an extension
of the known range to Cody (1996) of about 80 kilometers
south of Whitehorse.
Eleocharis uniglumis (Link) Schult. — YUKON: open
wet area in old road, adjacent to the Alaska Highway,
61°42.209'N 139°48.376'W, P. Caswell 204, 25 June
2002 (DAO); in wet moss by lake shore, Fish Lake,
60°46'3.3"N 135°03'13"W, W. J. Cody 38246, 2 Aug.
2002 (DAO).
The species was considered rare in the Territory by Douglas
et al. (1981). The first specimen cited above is an extension
of the known range to Cody (1996) of about 150 kilometers
northwest of a site northwest of Haines Junction and the
second specimen is from a site just south of Whitehorse.
Eriophorum brachyantherum Trautv., Short-anthered
Cotton-grass — YUKON: Vuntut National Park, vicinity
of Snowdrift Camp, 68°21.4'N 139°13.1'W, P. Cas-
well PPC-2000-Y-070, 21 June 2000 (DAO).
The specimen cited above is the northernmost yet found
in the Territory (Cody 1996). It is an extension of about 100
kilometers north from sites adjacent to the Porcupine River.
Kobresia simpliciuscula (Wahlenb.) Mack., Simple
Kobresia — YUKON: along road track through Picea
glauca forest, Minto RV Campground, 62°35'N
136°51'W, Cody & Cody 37678, 6 Aug. 2001 (DAO).
2004
The nearest site in the Territory (Cody 1996) to the speci-
men cited above is about 130 kilometers to the southeast
adjacent to the Klondike Highway.
Scirpus rollandii Fern. — YUKON: moist organic soil,
side road west of Alaska Highway, north of Donjek
River bridge, 61°42.209'N 139°48.376'W, P. Caswell
202, 25 June 2002 (DAO).
Cody (1996) knew this species in the southwest of the
Territory where he considered it rare. The specimen cited
above is an extension of the known range of about 100 kilo-
meters northwest of southern Kluane Lake.
JUNCACEAE
Juncus bufonius L. s.1., Toad Rush — YUKON: mud
bar, Dezadeash River below Haines Junction, Kluane
National Park, 60°45.545'N 137°34.470'W, P. Cas-
well 791, 16 Aug. 2002 (DAO).
The specimen cited above is new to Kluane National Park
and is a range extension of about 290 kilometers to the south
of a site mapped by Cody (1996) and a site east of Johnson’s
Crossing reported by Cody et al. (2001).
Juncus filiformis L. — YUKON: in muck by small lake
adjacent to the Alaska Highway, 60°51'01"N
135°46'0.5"W, Cody & Cody 38185, 1 Aug. 2002
(DAO).
The specimen cited above which is from a site about 75
kilometers west of Whitehorse is the westernmost yet found
adjacent to the Alaska Highway.
Luzula arcuata (Wahlenb.) Sw. ssp. unalaschkensis
(Buch) Hultén — gravel beside road and steep slope, Al-
aska Highway Km 1918, 62°16'26.1"N 140°45'6.7"W,
Cody & Cody 37851, 20 July 2002 (DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 215 kilometers
northwest of a site northwest of Haines Junction.
LILIACEAE
Allium schoenoprasum L. ssp. sibiricum (L.) Celak,
Wild Onion — YUKON: Herschel Island, 69°35'N
139°05'W, C. E. Kennedy s.n., 1 July 1985 (Environ-
ment Yukon Herbarium, photo DAO).
The nearest site known to Cody (1996) was adjacent to
the Firth River at 69°13'N 139°35'W, about 30 kilometers
southwest of the Herschel Island site.
Maianthemum canadense Desf. ssp. interius (Fern.)
A. & D. Love, Wild Lily-of-the- Valley — YUKON: com-
mon in understory in the riparian white spruce poplar
zone, Contact Creek, 60°00'00"N 127°43'44"W, B.
Bennett 01-025, 25 June 2001 (DAO).
Cody (1994, 1996) suggested that this taxon should be
looked for in the Territory and Cody et al. (1998, 2000) re-
ported it from the extreme southeast. The specimen cited
above is an extension of the known range of about 80 kilo-
meters southwest from a site adjacent to the Beaver River
hotspring.
Tofieldia coccinea Richards., Northern False Asphodel
— YUKON: south aspect-xeric-graminoid/forb/lichen
meadow, Volcano Mountain, 62°55'N 137°23'W, G.
Brunner 521a-01, 3 Aug. 2001 (Environment Yukon,
photo DAO).
Copy, KENNEDY, BENNETT, AND CASWELL: PLANTS IN YUKON YI
567
The specimen cited above is from the first known site
between latitudes 62°N and 64°N. The nearest site to the north
is about 175 kilometers to a site adjacent to the Dempster
Highway and to the southwest about 190 kilometers adjacent
to the Alaska Highway.
IRIDACEAE
Tris setosa Pall. ssp. interior (Anders.) Hultén, Wild
Iris — YUKON: at high water level, confluence of 12 Mile
River and Yukon River, 64°15'11"N 139°43'18"W, B.
Bennett 02-743, 23 Aug. 2002 (DAO).
Cody (1996) knew this rare species in the Territory from
only three locations, two from near the western end of the
Alaska Highway and one from adjacent to the Takhini River
west of Whitehorse. The specimen cited above is an extension
of the known range of about 225 kilometers to the north of the
sites near the Alaska border. Only four plants were observed.
ORCHIDACEAE
Spiranthes romanzoffiana Cham. & Schlecht., Hooded
Ladies’-tresses — YUKON: tussocks near bog, east of
Haines Highway, 60°08.570'N 136°58.469'W, P. Cas-
well 453, 13 July 2002 (DAO).
The specimen cited above is an extension of the known
range in the Territory of about 120 kilometers southwest of
Whitehorse.
SALICACEAE
Salix alaxensis (Anderss.) Cov. ssp. longistylis (Rydb.)
Hultén — YUKON: beside recreation centre in middle
of town, Beaver Creek, 62°22'56"N 140°52'41"W, B.
Bennett 01-102, 12 June 2001 (DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 140 kilometers
northwest of a site near the north end of Kluane Lake.
Salix glauca L. var. acutifolia (Hook.) C. Schneider —
YUKON: Mt. Merrill, 60°06'N 124°45'W, G. Brunner,
1994 (DAO).
The specimen cited above is about 90 kilometers east of
the easternmost site of Salix glauca sl. mapped by Cody
(1996).
Salix pseudomyrsinites (Anderss.) Ball ex Hultén (S.
novae-angliae Anderss.) — YUKON: along Bennett
Lake just above high water mark, Carcross Dunes,
60°10'30"N 134°43'26"W, B. Bennett & G. Argus 99-
548, 29 Aug. 1999 (DAO) (determined by G. Argus).
The nearest site of this species known to Cody (1996) is in
the vicinity of Whitehorse, about 60 kilometers to the north-
west.
Salix rotundifolia Trauty. ssp. dodgeana (Rydb.) Argus
— YUKON: Dryas alaskensis tundra, Mount Casca
border Monument 97, 65°21'25"N 141°00'00"W, B.
Bennett & M. B. Cook 02-519, 27 Jane 2002 (DAO)
(determined by G. Argus).
The specimen cited above from adjacent to the Alaska
border is from a site about 70 kilometers northwest of the
nearest site known to Cody (1996).
URTICACEAE
Urtica dioica L. ssp. gracilis (Ait.) Selander, Sting-
ing Nettle — YUKON: dwelling mound, Forty Mile
Historic Site at the confluence of Forty Mile and
568
Yukon rivers, 64°25'N 140°30'W, C. E. Kennedy 44,
July 2000 (DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 50 kilometers
northwest of the vicinity of Dawson City.
POLYGONACEAE
Polygonum lapathifolium L., Willow Weed, Pale Smart-
wood — YUKON: wetland Carex fen, uncommon silty
mud beside beaver pond, 60°07'00"N 124°15'2"W, B.
Bennett 98-609, 16 June 1998 (DAO).
This species was considered rare in the Territory by Doug-
las et al. (1981). The specimen cited above is an extension
of the known range in the Territory of about 700 kilometers
southeast of sites in the vicinity of Carmacks.
Rheum rhabarbarum L. (R. rhaponticum L.) Rhubarb
— YUKON: adjacent to garage near machine shop, Fort
Selkirk, 62°46'34.4"N 137°23'35.9"W, Cody & Ken-
nedy 37799, 17 July 2002 (DAO).
Cody et al. (2001) and (2002) reported Rhubarb growing
wild at Silver City and Destruction Bay. The specimen cited
above is the third known cited where it was growing wild.
Rumex crispus L., Curled Dock — YUKON: moist shore
of small lake between Ross River and Campbell
Highway, 61°58'7"N 132°38'34"W, Cody & Cody
37961, 24 July 2002 (DAO).
The specimen cited above is the sixth site in the Territory
for this introduced species. Cody (1996) knew it from the
vicinity of Dawson City and it has since been reported from
just west of Whitehorse, Haines Junction and adjacent to the
Alaska Highway near the Alaska border (Cody et al. 2002).
CHENOPODIACEAE
Atriplex alaskensis S. Watson, (A. patula sensu Cody
(1996), A. patula var. alaskensis (S. Wats.) Welsh),
Alaskan Orache (Figure 3) — YUKON: alkaline flat,
Takhini Salt Flats, 60°51.2'N 135°43.23'W, Bennett &
Parker 98-431, 2 Sept. 1998 (B. Bennett Herbarium,
photo DAO) (determined by P. W. Ball); alkaline flats,
between the salt flat and the highway in the area of the
fence, Takhini Salt Flats, 60°51'23"N 135°42'55"W,
B. Bennett 01-168, 23 Aug. 2001 (B. Bennett Herb-
arium, photo DAO); occasional in wet alkaline margin
of a brackish slough, Mile 484.5 Alaska Highway west
of Whitehorse, R. L. Taylor 4094, 14 July 1959 (DAO);
common around clay margins of dried up alkaline
pond, east of Haines Junction at Mile 985 Alaska
Highway, 60°48'N 136°45'W, Calder & Kukkonen
25252, 14 Aug. 1960 (DAO); common around clayey
margin of alkaline lake, between Minto and Pelly
Crossing on Dawson-Whitehorse road, approximately
62°46'N 136°36'W, Calder & Kukkonen 28095, 10
Aug. 1960 (DAO).
Cody (1996) considered the Calder & Cody specimens as
introductions from Europe (A. patula). Atriplex alaskensis
should now be added to the Yukon Flora and the list of rare
plants of the Territory (Douglas et al. 1981). The Taylor spe-
cimen cited above was the basis for the drawing published
in the Yukon Flora as A. patula.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Atriplex subspicata (Nutt.) Rydberg — YUKON: grassy
area in open alkaline salt ponds, Mayo Road, Dilla-
bough’s Grazing Lease, 60°55'54"N 135°10'14"W, B.
Bennett 02-649, 19 Aug. 2002 (DAO).
Cody (1996) knew this species from a single locality adja-
cent to a saline pond just west of Whitehorse. The specimen
cited above from just north of Whitehorse is only the second
known from the Territory.
Chenopodium capitatum (L.) Asch., Strawberry-blite
— YUKON: disturbed gravelly soil, roadstop, Atlin Road
just north of BC border, 60°00'09"N 133°47'42.1"W,
Cody & Cody 37546, 28 July 2001 (DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 60 kilometers
to the southwest from a site in the vicinity of Johnson’s
Crossing.
Corispermum ochotense Ignatov var. alaskanum
Mosyakin (C. hyssopifolium sensu Cody 1996) —
YUKON: river bar in loose aluvial sand between Salix
exigua and river with Tanacetum bipinnatum, Poten-
tilla anserina and Aster falcatus, Yukon River at con-
fluence of Nester Creek, 64°38'22"N 140°52'52"W,
Bennett & Mulder 02-665, 25 Aug. 2002 (DAO); river
bar in loose alluvial sand between Salix exigua and
river with Tanacetum bipinnatum, Potentilla anserina
and Aster falcatus, Yukon River, 64°22'19"N
140°26'49"W, Bennett & Mulder 02-740, 24 Aug.
2002 (DAO).
The specimens cited above are the first yet found in the
Territory.
PORTULACACEAE
Claytonia megarrhiza (A. Gray) Parry, Alpine Spring-
beauty (Figure 3) — YUKON: alpine tundra, three plants
seen at base of a long scree slope near a very small
stream, northwest side of Wade Mountain, Kluane
National Park, 61°18'N 139°33'W, P. Caswell 236,
28 June 2002 (DAO).
This species, which is new to the Flora of the Yukon Terri-
tory (Cody 1996), should be added to the list of rare plants
of the Territory (Douglas et al. 1981). Porsild and Cody
(1980) knew it from three sites in the Mackenzie Mountains
in the Continental Northwest Territories and McJannet et al.
(1995) knew it from four sites in that area in the Rare
Vascular Plants in the Northwest Territories. To the south
Douglas et al. (2002) mapped three sites in the extreme
southeast of British Columbia where it was considered rare.
Montia fontana L., Blinks — YUKON: aquatic, growing
in the shallows (10-30 cm) in a backwater slough,
Lewes Marsh, 60°34'N 134°35'W, B. Bennett OO-
1091, 25 June 2000 (DAO) (determined by C. Parker
and W. J. Cody).
Cody (1996) knew this rare plant in the Territory only from
a single locality on the Arctic Coast where it was collected
by Erling Porsild in 1934 (CAN, photo DAO). In addition a
second specimen was collected by Cody on Herschel Island
in 1999 (Cody et al. 2001). This is a circumpolar, low-arctic
species, which was considered rare in the Territory by
Douglas et al. (1981). To the east of the location cited above
it is known from the southern Mackenzie Mountains in the
2004
FiGure 3. Claytonia megarrhiza, Alpine Springbeauty (drawn
by Lynne Bartosch).
former District of Mackenzie, and to the west in essentially
coastal regions of Alaska and British Columbia.
CARYOPHYLLACEAE
Cerastium arvense L., Field Chickweed — YUKON: wet
roadside ditch, Top of the World Highway Km 100,
64°05'53"N 140°54'43"W, Cody & Cody 38011, 26
July 2002 (DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 100 kilometers
west of the vicinity of Dawson City.
Minuartia dawsonensis (Britt.) House — YUKON: steep
slope by Alaska Highway, 8 km west of White River,
62°3'15.6"N 140°38'20.5"W, Cody & Cody 37880,
20 July 2002.
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 125 kilometers
northwest of a site adjacent to Kluane Lake.
Minuartia elegans (Cham. & Schlecht.) Schischk. —
YUKON: Dryas alaskensis heath, 30° southwest-facing
large talus dolomite boulders, summit of mountain
on Canadian side of Mount Casca, 65°21'37"N
140°59'34"W, B. Bennett & M. B. Cook 02-543, 27
June 2002 (B. Bennett Herbarium, photo DAO).
The specimen cited above from adjacent to the Alaska bor-
der is an extension of the known range of about 75 kilometers
northwest of the nearest site in the Ogilvie Mountains.
Minuartia macrocarpa (Pursh) Ostenf. — YUKON: al-
pine tundra, spotty occurrence in raised rocky mounds,
mountain between Kusawa and JoJo Lake, 60°35'47"N
136°15'19"W, B. Bennett 97-681, 19 Sept. 1997 (DAO).
The specimen cited above is an extension of the known
range in the southwest of the Territory of about 80 kilo-
meters southeast of a site northwest of Haines Junction.
Copy, KENNEDY, BENNETT, AND CASWELL: PLANTS IN YUKON VI
569
Minuartia yukonensis Hultén — YUKON: coarse gravel
and small rocks of a stream’s outwash, Upper Joe
Creek, Kluane National Park, 61°12.861'N 139°03.863'W,
P. Caswell 585, 24 July 2002 (DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 225 kilometers
west of a site north of Whitehorse.
Silene involucrata (Cham. & Schlecht.) Bocquet ssp.
tenella (Tolm.) Bocquet — YUKON: meadow between
Stone House and river near Fort Selkirk sign, Fort
Selkirk, 62°46'34.4"N 137°23'35.9"W, Cody & Ken-
nedy 37805, 17 July 2002 (DAO).
The specimen cited above is from a site between sites in
the vicinity of Mayo and south of latitude 62°.
Silene williamsii Britton — YUKON: talus lower slope
of southwest-facing bluff, Yukon River, Minto Bluff,
62°37'06"N 136°57'41"W, B. Bennett 02-678, 9 Aug.
2002 (B. Bennett Herbarium, photo DAO); common
on base of slope across from Brittania Creek growing
with Artemisia frigida and Calamagrostis purpuras-
cens, Yukon River, 62°52'28"N 138°42'56"W, Bennett
02-443, 10 Aug. 2002 (B. Bennett Herbarium, photo
DAO).
This species was considered rare in the Territory by
Douglas et al. (1981) on the basis of 3 collections from south
and southwest of Dawson City.
Silene vulgaris (Moench) Garcke, Bladder Campion
— YUKON: gravelly soil in old field with grass and
sweet clover, west of Mayo airport, 63°37'01.4"N
135°58'20.9"W, Cody & Cody 37665, 4 Aug. 2001
(DAO).
The specimen cited above of this introduced species in
the Territory (Cody 1996) was previously known only from
an area just east of Dawson.
Stellaria umbellata Turcz. — YUKON: wet scree cushion
in zinc moss, Wade Mountain, Kluane National Park,
61°18.450'N 139°30.921'W, P. Caswell 354, 7 July
2002 (DAO).
Douglas et al. (1981) considered this species as rare in the
Territory. Cody (1996) knew it from only three widely sepa-
rated sites. The specimen cited above is from a site about 60
kilometers northwest of a previously known site in Kluane
National Park.
NYMPHAEACEAE
Nuphar polysepalum Engelm., Yellow Pond-lily —
YUKON: shallow water along shore of lake, Tatchun
Lake Campground, 62°17'52.8"N 136°08'11.4"W,
Cody & Cody 37626, 30 July 2001 (DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 120 kilometers
to the north, south of Mayo.
RANUNCULACEAE
Pulsatilla ludoviciana (Nutt.) Heller, Prairie-crocus —
YUKON: steep grassy slope on ridge northeast of Wood-
burn Creek, Tintina Trench, Ddhaw Ghro, 63°08'N
136°05'W, C. E. Kennedy 4, 27 July 2001 (DAO).
570
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 100 kilometers
east northeast of a site north of the junction of the Pelly and
Yukon rivers.
Ranunculus aquatilis L. var. subrigidus (W. B. Drew)
Breitung — YUKON: near South Fork intake, Klondike
River on edge of beaver dam in old ditch, 64°0'30"N
138°12'00"W, G. Brunner 549, 22 July 2002 (DAO).
The nearest site known to Cody (1996) of this uncommon
variety was about 60 kilometers to the north adjacent to the
Dempster Highway.
Ranunculus occidentalis Nutt. var. brevistylis Greene,
Western Buttercup — YUKON: alpine tundra, valley
above treeline, Macmillan Pass, 63°15'N 130°02'W,
J. Basinger s.n., June 1982 (DAO).
Douglas et al. (1981) considered this species rare in the
Territory. The specimen cited above is the northernmost yet
found in the Territory and is an extension of the known
range of about 250 kilometers northeast of a site adjacent to
the northern South Canol Road.
PAPAVERACEAE
Papaver croceum Ledeb. — YUKON: by garbage along
trail in Picea glauca, Pinus, Populus tremuloides wood-
land, Whitehorse, near Hidden Lake, 60°35'00.5"N
135°51'00.2"W, Cody & Cody 37678A, 9 Aug. 2001
(DAO); in gravel beside car parking spot, 11 Chalet
Crescent, Whitehorse, 60°55'54.7"N 135°10'26.5"W,
W. J. Cody 37711, 12 July 2002 (DAO) (determined
by H. Solstad).
This species is a garden escape which has not previously
been recorded from the Whitehorse area. In addition Heidi
Solstad revised three collections previously determined as
Papaver nudicaule (Dawson, Calder & Billard 3121 (DAO),
Halfway Lakes area 15 miles north of Mayo, Calder & Gil-
lett 4176 (DAO) and Tower Hill, Tagish, R. Rosie 798 (DAO))
to P. croceum. P. nudicaule ssp. nudicaule should be replaced
by P. croceum in the flora (Cody 1996, 2000).
BRASSICACEAE (CRUCIFERAE)
Alyssum obovatum (C. A. Meyer) Turez. (A. ameri-
canum Greene) — YUKON: 45° talus southwest-facing
slope, Yukon River, | km east of Alaska/Yukon border,
64°41'05"N 140°57'30"W, Bennett & Mulder 02-666,
25 Aug. 2002 (B. Bennett Herbarium, photo DAO)
(determined by G. A. Mulligan).
Douglas et al. (1981) considered this species too wide-
spread to include it in The Rare Vascular Plants of the Yukon.
Cody (1996) knew it from only eleven sites north of latitude
62°N. The specimen cited above is a slight extension of the
known range in the Territory about 50 kilometers to the
northwest of another site adjacent to the Yukon River.
Arabis caucasica Willd., Wall Rock-Cress (Figure 4)
— YUKON: garden escape, Alsek Road, Hayes Property,
10 km NW of Haines Junction, 64°47'N 137°41'W,
B. Bennett 01-041, 12 June 2001 (DAO) (determined
by G. A. Mulligan). Submitted to B. Bennett by
Carolyn Hayes.
This garden escape has not previously been observed in
the Yukon Territory.
THE CANADIAN FIELD-NATURALIST
Vol. 118
re a
Ze
AL
Figure 4. Arabis caucasica (drawn by Lee Mennell).
Arabis caucasica can be separated from A. codyi as
follows:
A. Garden escape; cauline and caudex leaves
with similar dentate to subdentate margins,
flowering stems spreading to ascending;
petals!/6:Simim) longi ee ee ae A. caucasica
B. Native species; cauline and caudex leaves not
similarly dentate to subdentate; flowering stems erect;
petals more than 10 mm long............. A. codyi
Arabis holboellii Hornem. var. retrofracta (Graham)
Rydb. — YUKON: gravel beside road and steep slope,
Alaska Highway Km 1918, 62°16'26.1"N 140°45'6.7"W,
Cody & Cody 37855, 20 July 2002 (DAO).
The nearest site adjacent to the Alaska Highway known
to Cody (1996) is about 150 kilometers to the southeast in the
vicinity of Kluane Lake. There is, however, a site adjacent
to a river about 60 kilometers to the east.
Arabis holboellii Hornem. var. secunda (Howell) Jep-
son — YUKON: adjacent to narrow road through woods
leading down to Nares Lake southeast of Carcross,
60°9'20"N_ 134°40'10"W, Cody & Cody 37934, 23
July 2002 (DAO) (determined G. A. Mulligan).
Cody (1996) knew this taxon from only four localities in
the Territory, west of longitude 135°. Cody (2001) added new
sites in the vicinity of Whitehorse and Wolf Lake to the east.
The specimen cited above is the southernmost yet found in
the Territory.
,
{
'
2004
Armoracia rusticana (Lam.) Gaert., Mess. & Scherb. —
YUKON: Hultén (1941-50) reported this species “A specimen
of this plant was collected at Stewart R. July 1898 by Anders-
son (S). It must have been cultivated or have escaped from
cultivation". Hultén (1968) mapped the worldwide distribution
of this species with a single dot in the Territory and Welsh
(1974) sub Rorippa armorocia (L.) A. S. Hitche. stated “Cul-
tivated for the root; in southern Alaska and Yukon, persisting:
introduced from Europe". Fortunately this species was over-
looked by Cody when preparing the Flora of the Yukon
Territory (1996); since the Anderson specimen was recently
borrowed from the Swedish Museum of Natural History,
Stockholm and was revised by Gerald A. Mulligan to
Rorippa barbareifolia (DC.) Kitagawa, an amphi-Berigian,
nonarctic species which extends across Alaska to central
Yukon Territory, the Porcupine River valley, the central Rich-
ardson Mountains and the Fort McPherson area south of the
Mackenzie Delta.
Brassica rapa L., Bird rape — YUKON: roadside gravel,
Alaska Highway, near Kluane Wilderness Camp Km
1791, B. Bennett 01-095, 24 July 2001 (DAO).
The specimen cited above of this introduced species is an
extension of the known range in the Territory of about 175
kilometers northwest of a site adjacent to the Haines High-
way. It may have resulted from roadside seeding.
Camelina sativa (L.) Cranz, Falseflax (Figure 5) —
YUKON: disturbed site, Whitehorse Shipyards,
60°43'34"N 135°03'12"W, B. Bennett 01-150, 28 Aug.
RNA
tS a Men
AP,
SS Yee
“has ls
yy
AY
.\
Za
FiGure 5. Camelina sativa, Falseflax (drawn by Lee Mennell).
Copy, KENNEDY, BENNETT, AND CASWELL: PLANTS IN YUKON VI
S74
2001 (B. Bennett Herbarium, photo DAO) (determined
by G. A. Mulligan).
The specimen cited above is new to the Flora of the Yukon
Territory (Cody 1996). It is a Eurasian introduction which is
known in Canada from New Brunswick to British Columbia
and north into southern District of Mackenzie.
The genus Camelina can be separated from the genus
Alyssum as follows:
A. — Styles usually 2-3 mm long; silicles oval-elliptic to
egg-shaped, usually at least 5 mm long; seeds numer-
ous; petals often shallowly bilobed; annual Camelina
B. Styles not over 1 mm long; silicles oval
in outline, less than 5 mm long; petals
notbilobed:perennialy ys ee eae ere Alyssum
Capsella bursa-pastoris (L.) Medic., Shepherd’s-purse
— YUKON: level gravel area, Campbell Highway Km
380, 62°02'34.2"N 132°52'02.2"W, Cody & Cody
37591, 30 July 2001 (DAO); growing beside Artemi-
sia tilesii by narrow road through woodland, Pelly
Farm Road, 62°51'22.2"N 137°00'34"W, Cody &
Kennedy 37821B, 17 July 2002 (DAO); gravel, Pick-
handle Lake, 63°02'22.2"N 138°23'15.8"W, Cody &
Cody 37834, 20 July 2002 (DAO).
The first specimen cited above of this introduced species
is from a site between two sites adjacent to the Campbell
Highway (Cody 1996) in the vicinity of Carmacks. One of
sites is 175 kilometers to the west and the other is about 185
kilometers to the southeast. The second and third specimens
are from sites between Keno and Carmacks (Cody 1996).
Cardamine bellidifolia L., Alpine Bittercress — YUKON:
Herschel Island, 69°35'N 139°O5S'W, C. E. Kennedy
s.n., 20 July 1985 (DAO).
The nearest sites known to Cody (1996) were from the
north coast about 30 kilometers to the west and near the
Firth River about 30 kilometers to the southwest.
Descurainia incisa (Engelm. ex A. Gray) Britton var.
incisa, Tansy Mustard — YUKON: gravel roadside, rare,
Dempster Highway Km 98, 64°42'N 138°24'46"W,
Cody & Cody 38056, 27 July 2002 (DAO) (deter-
mined by G. A. Mulligan).
Cody et al. (2001) reported this species as new to the
Territory and Cody et al. (2002) added additional sites adja-
cent to the Alaska Highway north of latitude 62°N. The
specimen cited above is from the first known site adjacent
to the Dempster Highway.
Draba aurea M. Vahl, Golden Draba — YUKON: Site
KP 110, 62°15\09-6°N) 137°41:03) W. (Gs Brunner
591-01, 8 Aug 2001 (Environment Yukon Herbariam,
photo DAO) (determined by G. A. Mulligan).
The specimen cited above is the northernmost yet found
in the Territory (Cody 1996). It is an extension of the known
range of about 50 kilometers from a site south of latitude
62°N.
Draba corymbosa R. Br. — YUKON: Herschel Island,
69°35'N 139°05'W, C. E. Kennedy s.n., 10 Aug. 1985
(Environment Yukon Herbarium, photo DAO) (deter-
mined by G. A. Mulligan).
S72
The nearest site known to Cody (1996) was from near the
Firth River about 30 kilometers to the southwest.
Draba crassifolia Graham — YUKON: sandy moist soil in
eroded area, ridge south of Donjek Glacier, 61°08.277'N
139°31.170'W, P. Caswell 403, 8 July 2002 (DAO)
(determined by G. A. Mulligan).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) northwest of sites in
Kluane National Park.
Draba glabella Pursh — YUKON: steep south-facing
bluffs along Klondike River, 1 mile north of
64°02'00"N_ 137°41'30"W, G. Brunner 435, 2 June
2001 (DAO) (determined by G. A. Mulligan).
The specimen cited above is from a site about 70 kilo-
meters east of a site in the vicinity of Dawson City (Cody
1996).
Draba nemorosa L., Wood Whitlow-grass — YUKON:
disturbed farm area, Black Sheep airline base, Mayo,
63°35.26'N 135°51.83'W, B. Bennett 00-1193, 2 July
2000 (DAO) (determined by G. A. Mulligan).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 110 kilometers
northeast of a site west of longitude 137°W and north of the
Pelly River.
Draba ogilviensis Hultén — YUKON: summit of small
peak south of Donjek Glacier, Kluane National Park,
61°08.318'N 139°31.132'W, P. Caswell 392, 8 July
2002 (DAO) (determined by G. A. Mulligan).
Douglas et al. (1981) considered this species rare in the
Territory. The specimen cited above is the westernmost yet
known in Kluane National Park.
Draba palanderiana Kjellm. — YUKON: dry alpine
Dryas heath with Dryas alaskensis, Silene acaulis,
Synthyris borealis, Podistera macounii and lichens,
summit of mountain, calcareous dolomite talus,
65°21.37'N 140°59.34'W, B. Bennett 02-523, 27 June
2002 (DAO).
The specimen cited above from adjacent to the Alaska
border is an extension of the known range in the Territory of
about 60 kilometers to the north of a site mapped by Cody
(1996).
Draba porsildii G. A. Mulligan — YUKON: wet scree,
Wade Mountain, Kluane National Park, 61°18'N
139°33'W, P. Caswell 240, 2 June 2002 (DAO) (deter-
mined by G. A. Mulligan).
Douglas et al. (1981) considered this species rare in the
Territory on the basis of three specimens from Kluane Nation-
al Park and one from the South Canol Road southwest of Ross
River. Cody (2003) cited a specimen from west of the three
sites in Kluane National Park. The specimen cited above is
from an additional site in the Park about 70 kilometers north
of the last site.
Draba stenoloba Ledeb. — YUKON: Donjek Valley,
61°25.689'N 139°53.074'W, R. Maraj s.n., 29 June
2002 (DAO) (determined by G. A. Mulligan).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 90 kilometers
northwest of a site in Kluane National Park.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Lepidium densiflorum Schrad. var. densiflorum, Com-
mon Pepper-grass — YUKON: roadstop in disturbed
gravelly soil, Atlin Road just north of BC border,
60°00'09"N_ 133°47'42.1"W, Cody & Cody 37543,
37551, 28 July 2001 (DAO) (determined by G. A.
Mulligan).
The specimens cited above are an extension of the known
range in the Territory (Cody 1996) of about 125 kilometers
southeast of a site just west of Whitehorse.
Lepidium densiflorum Schrad. var. macrocarpum G.
A. Mulligan — YUKON: adjacent to Catholic Church,
Fort Selkirk, 62°46'34.4"N 137°23'35.9"W, Cody &
Kennedy 37808A, 17 July 2002 (DAO) (determined by
G. A. Mulligan).
Cody et al. (2001) reported this variety, which is probably
introduced, new to the Territory from the vicinities of Daw-
son, Ross River and Pelly Crossing. The specimen cited
above is an extension of the known range in the Territory of
about 50 kilometers to the west of Pelly Crossing.
Parrya arctica R. Br. — Two specimens, one from Pauline
Cove, Herschel Island (Cody 36030) and the other from the
Bonnet Plume River (Loewen 99-25-93) were recently revised
to P. nudicaulis by G. A. Mulligan. These two species can
be separated as follows:
A. Stamens linear, 1.5 to
IEPfoyistVool) KON reteieicn acc bane jaa P. nudicaulis
B. Stamens oblong, less than
1h Oimmvlon es kane een OT ate ee P. arctica
In addition, Cody (1994) reported P. arctica from Herschel
Island on the basis of a specimen collected by P. F. Cooper
(433), 9 May 1979 (CAN) as new to the Territory and sug-
gested that it should be added to the list of rare plants (Doug-
las et al. 1981). This specimen has now been revised to Thlas-
piarcticum Porsild by G. A. Mulligan and should be deleted
from the flora of Herschel Island and the Yukon Territory.
Rorippa barbareifolia (DC.) Kitagawa — YUKON: Pelly
Crossing, 62°51'09"N 136°56'05.2"W, Cody & Ken-
nedy 37831, 17 July 2002 (DAO) (determined by G.
A. Mulligan).
This species was considered rare in the Territory by Doug-
las et al. (1981). The specimen cited above is the southern-
most yet found adjacent to the Alaska Highway.
Sinapis arvensis L., Charlock — YUKON: in a well-tend-
ed flower bed, Haines Junction, P. Caswell 311, 5 July
2002 (DAO) (determined by G. A. Mulligan).
The specimen cited above which was the only plant ob-
served in Haines Junction of this introduced species was from
only the third site known to Cody (1996) in the Territory.
Subularia aquatica L. ssp. americana Mulligan &
Calder, Awlwort — YUKON: shallows of large pond east
of Alaska Highway north of Sulphur Lake, 61°00.435'N
138°12.729'W, P. Caswell 772, 9 Aug. 2002 (DAO)
(determined by G. A. Mulligan).
This species was considered rare in the Territory by Doug-
las et al. (1981). The specimen cited above is an extension
of the known range of about 175 kilometers east of a site in
the vicinity of Whitehorse (Cody 1996).
2004
Thlaspi arvense L., Penny Cress — in black muck just
inside gate, flats 7 miles east of Tagish Bridge,
60°19'S"N 134°10'17"W, Cody & Cody 37958, 23
July 2002 (DAO) (determined by G. A. Mulligan).
The specimen cited above is an extension of the known
range of this introduced species of about 80 kilometers south-
east of the vicinity of Whitehorse.
SAXIFRAGACEAE
Ribes oxyacanthoides L. ssp. oxyacanthoides — YUKON:
meadow adjacent to RCMP foundation, Fort Selkirk,
62°46'34.4"N 137°23'35.9"W, Cody & Kennedy 37757,
16 July 2002 (DAO).
Although quite frequent in the Territory south of latitude
62°N, Cody (1996) knew this shrub from only two sites to
the north.
Saxifraga caespitosa L.— YUKON: 40° slope talus dolo-
mite boulders, Mount Casca border Monument 97,
65°21'25"N 141°00'00"W, B. Bennett & M. Cook 02-
SISA, 27 June 2002 (DAO).
Cody (1996) mapped this species in the Territory from
three distinct areas (between latitudes 60° and 62°, between
latitudes 64° and 66°, and north of latutude 68°. The specimen
cited above from adjacent to the Yukon-Alaska border is about
70 kilometers from the sites east and southeast.
Saxifraga eschscholtzii Sternb. — YUKON: dry alpine
heath at summit of mountain on Canadian side of
Mount Casca, 65°21'37"N 140°59'34"W, B. Bennett
& M. Cook 02-512, 27 June 2002 (DAO).
Cody (1996) knew this species only from the British
Mountains in the extreme northwest of the Territory. The
specimen cited above is an extension of the known range in
the Territory of about 460 kilometers to the south.
Saxifraga foliolosa R. Br. — YUKON: damp sand of
small sandy depression in sedge tundra, ridge south
of Donjek Glacier, Kluane National Park, 61°07.383'N
139°31.308'W, P. Caswell 416, 8 July 2002 (DAO).
Douglas et al. (1981) considered this species which was
known to Cody (1996) from north of latitude 67°N and a
single site on the west side of Haines Highway southeast of
Haines Junction as rare in the Territory. Cody et al. (2000)
reported another site in the south from about 80 kilometers
northeast of the site adjacent to the Haines Highway. The
specimen cited above is an extension of the range in the south
of about 135 kilometers northwest of the site near the Haines
Highway.
Saxifraga nelsoniana D. Don ssp. pacifica (Hultén) —
YUKON: wet organic soil with some fine scree at edge
of stream, Tabletop Mountain, Kluane National Park,
61°15.231'N 139°11.115'W, P. Caswell 285, 29 June
2002 (DAO).
Douglas et al. (1981) considered this subspecies rare in
the Territory. The specimen cited above is an extension of the
known range in the Park of about 25 kilometers west of a site
west of Kluane Lake.
Saxifraga rufopilosa (Hultén) Porsild — YUKON: moist
places in 30° southwest facing large talus dolomite
boulders, summit of mountain on Canadian side of
Mount Casca, 65°21'37"N 140°59'34"W, B. Bennett
& M. B. Cook 02-528, 27 June 2002 (DAO).
Copy, KENNEDY, BENNETT, AND CASWELL: PLANTS IN YUKON VI
SME:
The specimen cited above is from a site about 35 kilometers
northwest of the northernmost site south of latitude 66°N
known to Cody (1996).
Saxifraga tricuspidata Rottb., Prickly Saxifrage —
YUKON: steep grassy slope on ridge northeast of Wood-
burn Creek, Tintina Trench, Ddhaw, 63°08'N 136°05'W,
C. E. Kennedy 7, 27 July 2001 (DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 100 kilometers
east northeast of a site at about longitude 137°W, north of the
Pelly River.
ROSACEAE
Amelanchier alnifolia (Nutt.) Nutt., Saskatoon —
YUKON: southwest-facing slope across from Brittania
Creek, Yukon River, 62°52'28"N 138°42'56"W, B.
Bennett 02-653, 10 Aug. 2002 (DAO).
Cody (1996) knew only three sites of this species north of
the site reported above: Dawson City, Mayo, and adjacent
to the Stewart River.
Chamaerhodos erecta (L.) Bge. ssp. nuttallii (Picker-
ing ex Rydb.) Hultén — YUKON: common at base of
southwest-facing slope, across from Brittania Creek,
Yukon River, 62°52'28"N 138°42'56"W, B. Bennett
02-640, 10 Aug. 2002 (DAO).
Cody (1996) knew this species in the Territory north to
near latitude 64°. The specimen cited above is an extension
of the known range in the Territory of about 80 kilometers
west of a site adjacent to the Pelly River.
Dryas hookeriana Juz. — YUKON: Ogilvie Mountains,
Tombstone Range, Yakamaw Creek, watershed east of
Angelcomb Peak, 64°36'N 138°14'W, Cody 36808,
36845, 20-22 July 1999 (DAO); Dryas alaskensis
tundra, Mount Casca border Monument, 65°21'25"N
141°00'00"W, B. Bennett & M. B. Cook 02-518, 27
June 2002 (B. Bennett Herbarium, photo DAO).
The specimens cited above are the first yet known to Cody
(1996) from west of the Dempster Highway between latitudes
64°N and 66°N.
Geum aleppicum Jacq. ssp. strictum (Ait.) Clausen,
Yellow Avens — YUKON: Top of the World Golf Course,
64°3'38"N 139°26'13"W, Cody & Cody 37998, 25
July 2002 (DAO).
Douglas et al. (1981) considered this taxon rare in the Ter-
ritory. The specimen cited above is an extension of the known
range in the Territory of about 200 kilometers west of a site
west of Keno City (Cody et al. 2001) and north of sites adja-
cent to the Alaska Highway near the Alaska border.
Geum rossii (R. Br.) Scr. — YUKON: moist places at sum-
mit of the Canadian side of Mount Casca, 65°21'37"N
140°59'34"W, B. Bennett 02-524, 27 June 2002 (B.
Bennett Herbarium, photo DAO).
The specimen cited above is from a site about 100 kilo-
meters northwest of the nearest location in the Ogilvie Moun-
tains where it has been collected frequently.
Potentilla arguta Pursh ssp. convallaria (Rydb.) Keck,
Tall Cinquefoil — YUKON: dry rocky area, South Fork
intake, Klondike River, 64°0'30"N 138°12'00"W, G.
Brunner 551, 22 July 2002 (DAO).
574
The specimen cited above is only the second collected
from north of latitude 64°N in the Territory (Cody 1996). It is
from a site about 60 kilometers east of the vicinity of Dawson.
Rosa woodsii Lindl., Western Rose — YUKON: Artemi-
sia frigida slope, east side of lake, Whitehorse, Hid-
den Lakes, 60°41'30"N 135°02'45"W, B. Bennett O1-
118, 11 July 2001 (B. Bennett Herbarium, photo
DAO); grassy alkaline slope north of highway on slope,
Alaska Highway Km 1588, | km east of Cracker Creek,
60°48'20"N 136°48'00"W, B. Bennett 02-735, 11 Sept.
2002 (DAO); common at base of slope, Yukon River,
Brittania Creek, 62°52'28"N 138°42'56"W, B. Bennett
02-639, 10 Aug. 2002 (B. Bennett Herbarium, photo
DAO).
This is a rare species in the Territory (Douglas et al. 1981).
The first specimen cited above is only the fourth known in
the Territory (Cody 1996). The second is an extension of the
known range in the Territory (Cody 1996) of about 50 kilo-
meters west of a site adjacent to the Alaska Highway. The
third specimen is an extension of about 125 kilometers north-
west of a site reported by Cody et al. (2003) from the vic-
inity of Carmacks.
FABACEAE (LEGUMINOSAE)
Lupinus nootkatensis Donn — YUKON: clearing bet-
ween road and poplar forest, west side of Haines High-
way, north of cut-off to Dalton Post, 60°09.405'N
136°58.572'W, P. Caswell 440, 13 July 2002 (DAO).
The specimen cited above is only the third known from
southeastern Kluane National Park and the Yukon Territory.
Oxytropis arctica R. Br., Arctic Oxytrope — YUKON: at
base of talus slope, Lower Kathleen Lake, along south
shore ca. 25 km SE of Haines Junction, 60°33'N
137°16'W, G. W. & G. G. Douglas 8391, 25 June
1975 (Kluane National Park, photo DAO); in alpine
fell field, Dezadeash River Valley ca. 16 km WSW of
Haines Junction, G.W. & G.G. Douglas 8405, 30 June
1975 (Kluane National Park Herbarium, photo DAO).
Cody (1996) suggested that this species should be looked
for in the mountains of northern Yukon Territory because it
is known in the Canadian Arctic and northern Alaska. Douglas
et al. (1999) included the Territory in the distribution of O.
arctica presumably on the basis of the specimens cited above
and also reported the only collection known in British Colum-
bia from Mile 416 Alaska Highway which is about 700 kilo-
meters east southeast of the Yukon sites. It should be added
to the list of rare species in the Territory.
Oxytropis campestris (L.) DC. ssp. varians (Rydb.)
Cody, Field Locoweed — YUKON: steep grassy slope
on ridge northeast of Woodburn Creek, Tintina Trench,
Ddhaw Ghro, 63°08'N 136°05'W, C. E. Kennedy 6,
27 July 2001 (DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 110 kilometers
northeast of a site adjacent to the Yukon River.
Trifolium pratense L., Red Clover — YUKON: road-
side, junction of Campbell Highway and Frenchman
Lake Road, 62°4'30"N 135°30'55"W, Cody & Cody
37985, 24 July 2002 (DAO).
THE CANADIAN FIELD-NATURALIST
Vol. 118
The nearest site of this introduced species in the Territory
(Cody 1996) is from the vicinity of Whitehorse, about 150
kilometers to the south.
Vicia americana Muhl., American Vetch — YUKON: bor-
der of grassland and Populus, Macoobs Park, Mayo,
63°35'42.5"N 135°56'57.1"W, Cody & Cody 37668,
5 Aug. 2001 (DAO); west end of parking lot by visitor
kiosk, Rancheria, 60°05'16"N 130°36'10"W, B. Ben-
nett 01-059, 26 July 2001 (DAO).
Douglas et al. (1981) considered this species rare in the
Territory on the basis of a single collection from the Larsen
Creek hotsprings in the extreme southeast (Scotter & Cody
1979). Additional collections were added from this area by
Cody et al. (1998) and from the vicinity of Watson Lake (Cody
et al. 2000). The first specimen cited above is an extension
of the known range in the Territory of about 550 kilometers
to the northwest of Watson Lake. The second collection is an
extension of the known distribution of about 120 kilometers
west of Watson Lake but was probably introduced at that site.
CALLITRICHACEAE
Callitriche anceps Fern. — YUKON: on mud substrate at
edge of water, old beaver pond east of Haines Highway
about 10 kilometers south of Kathleen Lake cutoff,
60°30.838'N 137°04.970'W, P. Caswell 787, 11 Aug.
2002 (DAO).
This species was considered rare in the Territory (Douglas
et al. 1981). The specimen cited above is from a site about
30 kilometers northwest of a site in Kluane National Park.
VIOLACEAE
Viola renifolia Gray var. brainerdii (Greene) Fern.,
Kidney-leaved Violet - YUKON: humus covered with
old poplar leaves, poplar and white spruce wood flat,
Wade Lakes Road, between Kluane National Park and
Haines Highway, 60°07.119'N 137°05.369'W, P. Cas-
well 020, 6 June 2002 (DAO).
Cody (1996) knew this species as far north as the vicinity
of Dawson City. The specimen cited above is an extension
of the known range in the Territory of about 150 kilometers
southwest of the vicinity of Whitehorse.
HALORAGACEAE
Myriophyllum verticillatum L. — YUKON: in water be-
side dock, Nunatuk Camp, 62°9'49"N 135°48'4"W,
Cody & Cody 37989, 24 July 2002 (DAO).
Douglas et al. (1981) considered this species rare in the
Territory. The specimen cited above is from a site about half
way between the Pelly River and the north end of Lake Le-
barge.
APIACEAE
Cicuta maculata L. var. angustifolia Hook., Spotted
Water-hemlock — YUKON: lush herbaceous meadow on
riverbank, Kirkman Creek, Yukon River, 62°59'21"N
139°23'07"W, B. Bennett 02-284, 10 Aug. 2002
(DAO).
Douglas et al. (1981) considered this taxon rare in the
Territory. The specimen cited above is an extension of the
known range of about 175 kilometers to the northwest of
Carcross (Cody 1996).
Podistera macounii (Coult. & Rose) Mathias & Const.
— YUKON: Dryas alaskensis tundra, Mount Casca bor-
2004
der Monument 97, 65°21'25"N 141°00'00"W, Bennett
& Cook 02-520, 27 June 2002 (DAO).
This species was considered rare in the Territory by Doug-
las et al. (1981). Cody (1996) knew it only from the Richard-
_ son Mountains area in the northeast. Cody et al. (1998) ex-
tended the known range in the Territory south into the Daw-
son range at latitude 62°26'N. The specimen cited above is
an extension of the known range in the Territory of about
275 kilometers to the west from the southernmost site in the
Richardson Mountains.
PYROLACEAE
Pyrola minor L. — YUKON: adjacent to the Catholic
Church, Fort Selkirk, 62°46'34.4"N_ 137°23'35.9"W,
Cody & Kennedy 37815, 17 July 2002 (DAO).
Although quite frequent in the Territory east and north of
the Klondike Highway, Cody (1996) also knew this species
_ from the vicinity of southern Kluane Lake, to the west.
_ ERICACEAE
Cassiope tetragona (L.) D. Don ssp. saximontana
(Small) Porsild — YUKON: dry alpine Dryas heath,
summit of Mount Casca, 65°21'37"N 140°59'34"W,
Bennett & Cook 02-522, 27 June 2002 (DAO).
The specimen cited above is the northernmost yet found in
_ the Territory. The nearest site to the above north of Chapman
Lake in the Ogilvie Mountains is about 125 kilometers to the
southeast (Cody et al. 2001).
| Harrimanella stellariana (Pallas) Coville — YUKON:
Morley River watershed, Englishman Range, 8 km SW
of Morris Lake, northwest facing slope growing in
bedrock controlled draw, 60°23'40"N 131°47'50"W,
J. Meikle 02-126, 20 June 2002 (DAO).
The specimen cited above is a rarity in the Territory (Doug-
las et al. 1981). It is a slight range extension north of the
eastern site mapped by Cody (1996).
Phyllodoce glanduliflora (Hook). Cov., Yellow Moun-
tain-heather — YUKON: subalpine slope by creek, Tank
Creek, 60°05'30"N 134°41.9'W, S. Withers SWO1-114,
15 July 2001 (DAO).
Cody (1996) knew this species in the Territory only from
sites east of longitude 130°W and west of longitude 137°W.
The specimen cited above is about 125 kilometers east of a
site in Kluane National Park.
Vaccinium membranaceum Dougl., Tall Blueberry —
YUKON: moist subalpine meadow, Kotaneelee Range,
60°14'31L"N 124°7'19"W, B. Bennett 95-149, 20 June
1998 (B. Bennett Herbarium, photo DAO); subalpine
forest, Beavercrow Ridge, 60°12.865'N 124°35.79'W,
B. Bennett 98-310, (B. Bennett Herbarium, photo
DAO).
Cody (1996) suggested that this species should be looked
for in the southeastern part of the Territory. Cody et al. (1998)
reported four collections from Mount Merrill and Gusty
Lakes. The two specimens cited above are from the extreme
southeast.
PRIMULACEAE
Douglasia alaskana (Cov. & Standl.) Kelso — YUKON:
eroded alpine slope, Table Mountain, Kluane National
Copy, KENNEDY, BENNETT, AND CASWELL: PLANTS IN YUKON VI
575
Park, 61°15'.231'N 139°11.115'W, P. Caswell 282,
29 June 2002 (DAO).
Douglas et al. (1981) considered this species rare in the
Territory where it was only known in Kluane National Park.
The specimen cited above extends the known range in the
Park about 75 kilometers to the northwest.
Douglasia arctica Hook. — YUKON: Cody et al. (2000)
reported this species from a mountain between Kusawa
and JoJo Lake, which was a considerable southward
range extension.
The specimen upon which it was reported was unfortu-
nately misidentified and the range extension should be deleted.
Primula eximia Greene (P. tschuktschorum Kjellm.
ssp. cairnesiana A. E. Porsild) — YUKON: Dempster
Highway about Km 96, at about altitude 4000 ft., S.
Frisch, spring 2001 (DAO).
Douglas et al. (1981) considered this species rare in the
Territory on the basis of collections from the northern Rich-
ardson Mountains and a site adjacent to the Alaska border at
about 63°50'N latitude. The specimen cited above is from a
site about 150 kilometers northeast of the Alaska border site
where there was “a whole field of them".
Trientalis europaea L. s.1., Starflower — YUKON: damp
mossy Picea glauca, Alnus incana, Dawson area,
64°02'00"N 137°41'30"W, G. Brunner 439, 30 June
2001 (DAO).
The specimen cited above from about 70 kilometers east of
Dawson City, is only the second collection in the Territory
from north of latitude 64°N (Cody 1996).
GENTIANACEAE
Gentianella tenella (Rottb.) Boerner — YUKON: alpine
barrens on long ridge, Atlas Mountain, Kluane Nation-
al Park, 61°14.772'N 139°19.254'W, D. Normandeau
s.n., P- Caswell 328A, 6 July 2002 (DAO); patch of al-
pine tundra, mountain opposite Donjek Glacier, Kluane
National Park, 61°11.859'N 139°23.372'W, P. Cas-
well 619, 26 July 2002 (DAO).
This species was considered rare in the Territory by Doug-
las et al. (1981). Cody (1996) knew it from only three sites,
two about 40 kilometers west of the specimens cited above
and one just north of latitude 62°N.
POLEMONIACEAE
Phlox hoodii Richards., Moss Phlox — YUKON: dry
rocky slope, open habitat, Donjek River watershed near
Kluane Glacier, M. Hoefs 02-693, 4 July 2002 (DAO).
The specimen cited above from west of the Alaska High-
way is the fifth and southernmost in that area. This species
was not included in the Rare Vascular Plants of the Yukon
(Douglas et al. 1981) because of its widespread distribution.
Polemonium acutiflorum Willd. forma lacteum Lepage
— YUKON: rare in lush subalpine meadow at 4800 ft..
mountain 4 miles west of Upper Hyland Lake, 62°03'N
128°59'W, Calder & Kukkonen 27889, 3 Aug. 1960
(DAO) (determined by B. Boivin 1970).
Lepage (1950) described this white-flowered form on the
basis of a specimen collected at Anchorage, Alaska. Cody
(1996) unfortunately did not mention this white form
occurring in the Yukon Flora.
576
Polemonium boreale Adams forma albiflorum Cody,
— YUKON: fox den, sandy/grass area, Herschel Island,
site 203, 69°30'N 139°15'W, C. E. Kennedy 262, 16
July 1985 (DAO) (PARATYPE); [NORTHWEST TERRI-
TORIES: MACKENZIE: on a sandy portion of a gravel bar,
Horton River, N.W.T., 69°42'N 126°56'W, G. W.
Scotter 101016b, 6 July 1995 (DAO) (HOLOTYPE)
(Cody et al. 2003).
Cody (1996) stated that the corolla of this species was
blue to violet or rarely white. The white form had not been
described at that time.
HYDROPHYLLACEAE
Phacelia mollis Macb., Macbryde’s Phacelia — YUKON:
scattered in dry, open rubble on south-facing slopes
near base of bluff, Moosehide Hills, Bluff on N side
of Yukon R., 25 km downstream from Dawson,
64°15'41"N 139°36'13"W, C. Roland 93-27, 24 May
1993 (AKA, photo DAO).
The specimen cited above is an extension of about 50 kilo-
meters to the southwest from the nearest site in the Ogilvie
Mountains known to Cody (1996).
BORAGINACEAE
Eritrichium aretioides (Cham. & Schlecht.) DC. —
YUKON: dry alpine Dryas heath, Canada/US Boundary
Monument 97, 65°21'25"N 141°00'00"W, B. Bennett
02-019, 27 June 2002 (DAO).
The specimen cited above is an extension of the known
range in the Territory of about 40 kilometers northwest of the
nearest site known to Cody (1996) between latitudes 64°
and 66°N.
Eritrichium chamissonis DC. — YUKON: vicinity of
Snowdrift Camp, Vuntut National Park, 68°21.4'N
139°13.1'W, P. Caswell PPC-Y-076, 19 June 2000 (B.
Bennett Herbarium, photo DAO).
Cody (1996) knew this rare species in the Territory from
only two localities in the British Mountains. The specimen
cited above is from a site about 50 kilometers south of a site
on Mt. Sedgwick.
Mertensia paniculata (Britt.) G. Don var. alaskana
(Britt.) Williams — YUKON: adjacent to Joe Robert’s
Cabin, Fort Selkirk, 62°46'34.4"N 137°23'35.9"W,
Cody & Kennedy 37796, 17 July 2002 (DAO).
Cody (1996) knew this variety only from south of latitude
61°30'N and north of latitude 67°30'N.
Myosotis scorpioides L., Forget-me-not — YUKON:
flower bed at Kluane Park Inn, Haines Junction,
60°44'N 137°31'W, P. Caswell PPC-2000-Y-426, 28
Aug. 2000 (B. Bennett Herbarium, photo DAO).
This introduced species was previously known in the Ter-
ritory only from the vicinity of Whitehorse (Cody 1996).
LAMIACEAE (LABIATAE)
Galeopsis tetrahit L. ssp. bifida (Boenn.) Fries, Hemp-
nettle — YUKON: Forty Mile Historic Site at the conflu-
ence of the Forty Mile and Yukon rivers, 64°25'N
140°32'W, C. E. Kennedy 2, 6 July 2000 (DAO); under
large Picea glauca in squirrel midden, Judas Creek,
60°23.4'N 134°07.4'W, S. Withers SWO1-178, 30 Aug.
2001 (B. Bennett Herbarium, photo DAO).
THE CANADIAN FIELD-NATURALIST
Vol. 118
This introduced species was previously known in the Ter-
ritory from only three localities: North Canol Road (Cody
1994, 1996), Km 9 Dempster Highway (Cody et al. 1998)
and Whitehorse (Cody et al. 2001). The first specimen cited
above is the northernmost yet found in the Territory.
SCROPHULARIACEAE
Euphrasia subarctica Raup — YUKON: stony soil and
moss in cleared area below rest stop, Klondike High-
way Km 628, 63°50'18.1"N 137°59'20.5"W, Cody &
Cody 37660, 4 Aug. 2001 (DAO).
The specimen cited above is the northernmost yet found in
the Territory (Cody 1996). It is from a site about 110 kilo-
meters northwest/west of Mayo.
Mimulus guttatus DC., Yellow Monkeyflower —
YUKON: small seep near the road, Km 4.5 Atlin Road,
60°17'30"N 133°50'3"W, S. Withers SWO1-131, 24
July 2001 (DAO).
Douglas et al. (1981) considered this species rare in the
Territory. The specimen cited above is from a site about 80
kilometers southeast of Whitehorse.
Pedicularis oederi Vahl., Oeder’s Lousewort — YUKON:
Herschel Island, 69°35'N 139°05'W, C. E. Kennedy
s.n., 30 July 1985 (Yukon Renewable Government
Herbarium, photo DAO).
This species, which is frequent in the British Mountains
to the south is now known to the north on Herschel Island.
Rhinanathus minor L. ssp. borealis (Sterneck) A. Love
— Yukon: gravel parking area at foot of trail to Rock
Glacier, Haines Highway, 60°27'18"N 137°03'37.6"W,
Cody & Cody 37894, 21 July 2002 (DAO).
This taxon is known in the Territory only as far north as
about latitude 61°30'N. The specimen cited above is the first
record from the Haines Highway.
OROBANCHACEAE
Orobanche fasciculata Nutt. — YUKON: 45° silty sand
south-facing slope with Artemisia frigida and Cala-
magrostis purpurascens, Dutch Bluff, Yukon River,
61°55.72'N 135°03.99'W, B. Bennett 02-290, 7 Aug.
2002 (DAO).
This species was considered rare in the Territory by Doug-
las et al. (1981). Cody et al. (2003) reported a new site in
Kluane National Park adjacent to the Alaska Highway and
southern Kluane Lake. The specimen cited above is from a
site about 50 kilometers southeast of Carmacks.
LENTIBULARIACEAE
Pinguicula villosa L. — YUKON: in Sphagnum tus-
sock, bog east of Haines Highway, 60°08.421'N
136°58.499'W, P. Caswell 446, 13 July 2002 (DAO).
The specimen cited above is new to southwestern Yukon.
It is an extension of the known range in the Territory of about
300 kilometers southwest from a site adjacent to the northern
South Canol Road.
Utricularia minor L., Lesser Bladderwort — YUKON:
shallow water of lake between Ross River and Camp-
bell Highway, 61°58'16"N 132°38'06"W, Cody &
Cody 37967, 24 July 2002 (DAO).
This is a rare species in the Territory that Cody (1996) knew
from only four sites between latitudes 60°N and 64°30'N.
2004
Cody et al. (1998, 2000 and 2003) reported new collections
from the southeast in the vicinity of La Biche River and in
the far north between Trout Lake and the Babbage River.
The specimen cited above is from about 150 kilometers
north of a site near the south end of the South Canol Road.
PLANTAGINACEAE
Plantago canescens Adams — YUKON: base of cliffs,
talus, south-facing slope, Mount Carmacks, 64°20'08"N
140°12'25"W, B. Bennett 02-820, 24 Aug. 2002
(DAO).
The specimen cited above is an extension of the known
range in the Territory of about 200 kilometers northwest of
a site adjacent to the Klondike Highway (Cody 1996).
_ Plantago maritima L., Seaside Plaintain — YUKON: dry
sandy gravel slope north of gravel pit south of Alaska
Highway, 60°49'58"N 135°45'49"W, Cody & Cody
— 38204, 1 Aug. 2002 (DAO).
This species was considered rare in the Yukon Territory by
Douglas et al. (1981). Cody (1996) knew it from only two
localities adjacent to Kluane Lake in the extreme southwest.
_ The specimen cited above is from a site about 100 kilometers
to the east.
_ CAPRIFOLIACEAE
_ Sambucus racemosa L. ssp. pubens (Michx.) House,
_ Red Elderberry — YUKON: roadside and lakeshore,
Wade Lakes, 60°05.0'N 137°19.6'W, R. Maraj s.n.,
14 Sept. 2002 (DAO).
Douglas et al. (1981) (as var. arborescens) knew this taxon
from a single locality in southern Kluane National Park. The
specimen cited above extends the known range about 80 kilo-
_ meters to the east between the park and Haines Highway.
VALERIANACEAE
Valeriana sitchensis Bong., Sitka Valerian — YUKON:
Site YPN 120, 63°06'39.8"N 133°20'15"W, G. Brun-
ner 569-01, 6 Aug. 2001 (Environment Yukon, photo
DAO).
The specimen cited above is from a site between the North
Canol Road and Mayo.
ASTERACEAE (COMPOSITAE)
Aster alpinus L. ssp. vierhapperi Onno, Alpine Aster
— YUKON: steep grassy slope on ridge, northeast of
Woodburn Creek, Tintina Trench, Ddhaw Ghro,
_ 63°08'N 136°05'W, C. E. Kennedy 2, 27 July 2001
_ (DAO).
The specimen cited above is an extension of the known
range in the Territory (Cody 1996) of about 100 kilometers
northeast of a site near the junction of the Pelly and Yukon
rivers.
Aster falcatus Lindl., Western Heath Aster — YUKON:
lush herbaceous meadow riverbank, Kirkman Creek,
Yukon River, 62°59'21"N 139°23'07"W, B. Bennett
02-673, 10 Aug. 2002 (B. Bennett Herbarium, photo
DAO).
Douglas et al. (1981) considered this species rare in the
Territory. The specimen cited above is from a site about 150
kilometers west of a site adjacent to the Klondike Highway.
Erigeron caespitosus Nutt. — YUKON: silty sand south-
facing slope, Dutch Bluff, Yukon River, 61°55.72'N
Copy, KENNEDY, BENNETT, AND CASWELL: PLANTS IN YUKON VI
yd
135°03.99'W, B. Bennett 02-300, 7 Aug. 2002 (DAO);
top of slope of open bank, 1 mile upstream of Big
Salmon, on Yukon River, 61°51.41'N 134°55.01'W,
B. Bennett 02-302, 7 Aug. 2002 (DAO); base of cliffs,
talus, south-facing slope, Yukon River, Mount Car-
macks, 64°20'08"N 140°12'25"W, B. Bennett & R.
Mulder 02-816, 24 Aug. 2002 (DAO).
The first specimen cited above is from a site about 75 kilo-
meters southeast of a site adjacent to Carmacks and the sec-
ond specimen is from a site about 120 kilometers southeast
of Carmacks. The third specimen is from a site between two
sites near the Alaska border, one to the south about 120 kilo-
meters and the other to the north about 100 kilometers (Cody
1996).
Erigeron hyperboreus Greene — YUKON: middle of
dirt road leading to Copper Joe Creek Road, Kluane
National Park, 61°18.688'N 138°56.319'W, P. Caswell
170, 24 June 2002 (DAO).
This species was considered as rare in the Territory by
Douglas et al. (1981). The specimen cited above is an exten-
sion of about 425 kilometers south of a site northwest of
Dawson City.
Senecio eremophilus Richards., Dryland Ragwort (Fig-
ure 6) — YUKON: Pine Creek Campground, 4 miles
east of Haines Junction, Mile 1012 Alaska Highway,
V. L. Harms 6299, 17 August 1968 (DAO).
The specimen cited above is the first known record in the
Yukon Territory where it was probably introduced. To the
FiGurE 6. Senecio eremophilus, Dryland Ragwort (drawn
by J. Looman).
578
west in Alaska, Hultén (1968) knew it only from the
vicinity of Tok where he considered it also to be introduced.
To the east Porsild and Cody (1980) knew it from the Slave
River area north of Fort Smith where it was found in damp
woodland meadows and adjacent to roadsides and considered
native. To the south it is found in eastern British Columbia
east to Manitoba and south into the United States. It can be
separated from S. sheldonensis as follows:
A. Stem leaves deeply incised, not
TeducedipwardSey ss yale. coset S. eremophylus
B. Stem leaves with merely repand-denticulate
margins, reduced upwards ......... S. sheldonensis
Solidago canadensis L. var. salebrosa (Piper) Jones —
YUKON: beside test plot, 1 km N of Montague Road-
house, Km 132 Klondike Highway, 61°49'35"N
136°7'52"W, Cody & Cody 38073, 28 July 2002
(DAO).
Douglas et al. (1981) considered this species rare in the
Territory. The specimen cited above is from about 90 kilo-
meters southwest of a site mapped by Cody (1996).
Sonchus arvensis L. ssp. uliginosus (Bieb.) Nyman,
Perennial Sow-thistle — YUKON: roadside gravel, Alaska
Highway 3 km west of Kusawa Lake turnoff below
microwave tower, 60°46'00"N 136°05'36"W, _ B.
Bennett 02-749, 11 Sept. 2002 (DAO).
The specimen of this introduced species cited above is from
a site between Whitehorse and Haines Junction.
Tanacetum vulgare L., Common Tansey — YUKON: in
distributed ground along Campbell Highway, Tuchitua
River, 60°56'N 129°13'00"W, R. Rosie 1959, 16 Aug.
1997 (DAO); single patch west of the boat launch,
Yukon River Bridge, 60°34'20"N 134°40'W, B. Ben-
nett 01-063, 19 Aug. 2001 (DAO).
The specimens cited above are only the second and third
records of this introduced species in the Territory. Cody et al.
(1998) reported the first collection from just north of Kath-
leen Lake Lodge on the Haines Highway.
Acknowledgments
We thank Donald Britton and Daniel Brunton for
their identification of /soetes; Stephen J. Darbyshire for
his identification of several Poaceae; Gerald Mulligan
for his identification of Brassicaceae specimens; Heidi
Solstad for her identification of Papaver croceum; Greg
Brunner, Manfred Hoefs, Jennifer Line, R. Maraj,
Rhonda Rosie and Stu Withers for their contributions;
Margaret Cody and Douglas Cody for assisting the
senior author in the summers of 2001 and 2002 in
southern Yukon; artist Lee Mennell for his art work;
Paul Catling for reviewing an earlier version of this
manuscript, and especially Leslie Cody for the many
hours inputting this information on her computer.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Literature Cited
Cody, W. J. 1994. The Flora of the Yukon Territory: Addi-
tions, Range Extensions and Comments. Canadian Field-
Naturalist 108: 428-479.
Cody, W. J. 1996. Flora of the Yukon Territory. National
Research Council (NRC) Press, Ottawa, Ontario, Canada.
643 pages.
Cody, W. J. 2000. Flora of the Yukon Territory — Second
Edition. National Research Council (NRC) Press, Ottawa,
Ontario, Canada. 669 pages.
Cody, W. J., C. E. Kennedy, and B. Bennett. 1998. New
Records of Vascular Plants in the Yukon Territory. Cana-
dian Field-Naturalist 112: 289-328.
Cody, W. J., C. E. Kennedy, and B. Bennett. 2000. New
Records of Vascular Plants in the Yukon Territory I. Cana-
dian Field-Naturalist 114: 417-443.
Cody, W. J., C. E. Kennedy, and B. Bennett. 2001. New
Records of Vascular Plants in the Yukon Territory HI.
Canadian Field-Naturalist 115: 301-322.
Cody, W. J., C. E. Kennedy, B. Bennett, and V. Loewen.
2002. New records of Vascular Plants in the Yukon Terri-
tory IV. Canadian Field-Naturalist 116: 446-474.
Cody, W. J., C. E. Kennedy, B. Bennett, and J. Staniforth.
2003. New records of Vascular Plants in the Yukon Ter-
ritory V. Canadian Field-Naturalist 117: 278-301.
Cody, W. J., K. L. Reading, and J. L. Line. 2003. Additions
and range extensions to the vascular plant flora of the Con-
tinental Northwest Territories and Nunavut, Canada II.
Canadian Field-Naturalist 117(3): 448-465.
Douglas, G. W., G. W. Argus, H. L. Dickson, and D. F.
Brunton. 1981. The rare vascular plants of the Yukon.
Syllogeus 28: 1-96.
Hulten, E. 1941-1950. Flora of Alaska and Yukon, 1-10.
Lunds Universitets Arsskrift, N. F. Aud. 2. Volumes 37-
46. 1902 pages.
Hulten, E. 1968. Flora of Alaska and neighboring territories.
Stanford University Press. Stanford, California. 1008 pages.
Kojima, S., and R. C. Brooks. 1985. An annotated vascular
flora of areas adjacent to the Dempster Highway, central
Yukon Territory. I. Pteridophyta, Gymnospermae and
Monocotyledonae. British Columbia Provincial Museum,
Contributions of Natural Science 31: 1-16.
Lepage, E. 1950. Variations mineures de quelques plantes
du nord-est du Canada et de l’ Alaska. Le Naturaliste cana-
dien 77 : 228-231.
McJannet, C. L., G. W. Argus, and W. J. Cody. 1995. Rare
vascular plants in the Northwest Territories. Syllogeus
73: 1-104.
Porsild, A. E. 1975. Materials for a flora of central Yukon
Territory. National Museum of Natural Sciences. Publica-
tions in Botany 4, Ottawa, Ontario. 77 pages.
Porsild, A. E., and W. J. Cody. 1980. Vascular plants of Con-
tinental Northwest Territories, Canada. National Museum
of Natural Sciences, Ottawa, Ontario. 667 pages.
Scotter, G. W., and W. J. Cody. 1979. Interesting vascular
plants from southeastern Yukon Territory. Canadian Field-
Naturalist 93: 163-170.
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Parts of Canada. Brigham Young University Press, Provo,
Utah, U.S.A. 724 pages.
Received 11 December 2003
Accepted 3 February 2004
Hybridization Between a Green Turtle, Chelonia mydas, and
Loggerhead Turtle, Caretta caretta, and the First Record of a
Green Turtle in Atlantic Canada
MICHAEL C. JAMES!, KATHLEEN MARTIN2, and PETER H. DuTTON?
' Department of Biology, Dalhousie University, 1355 Oxford St., Halifax, Nova Scotia B3H 4J1 Canada (Corresponding
author)
> Nova Scotia Leatherback Turtle Working Group, 2070 Oxford St., Halifax, Nova Scotia B3L 2T2 Canada
3 Southwest Fisheries Science Center, National Marine Fisheries Service, 8604 La Jolla Shores Dr., La Jolla, California
92037 USA
James, Michael C., Kathleen Martin, and Peter H. Dutton. 2004. Hybridization between a Green Turtle, Chelonia mydas,
and Loggerhead Turtle, Caretta caretta, and the first record of a Green Turtle in Atlantic Canada. Canadian Field-
Naturalist 118 (4): 579-582.
The Green Turtle (Chelonia mydas) principally occupies tropical and subtropical waters, although juveniles are known to
occur seasonally in temperate coastal waters. Collaboration with commercial fishers in eastern Canada yielded the most
northerly records of this species in the northwest Atlantic. Here we report on the first confirmed record of a Green Turtle in
eastern Canada and on the occurrence of a rare Green Turtle—Loggerhead Turtle (Caretta caretta) hybrid. Hybridization
between the Carettini and Chelonini is extraordinary given that these groups have been genetically distinct for 50 million
years Or more.
Key Words: Green turtle, Chelonia mydas, hybrid, Loggerhead Turtle, Caretta caretta, Atlantic Canada.
The Green Turtle (Chelonia mydas) has a broad
range in the Atlantic, which includes waters off the
continental United States. Presence in temperate waters
of the northeastern United States is seasonal, with tur-
tles retreating to more southerly latitudes when water
temperatures decline (Epperly et al. 1995). During
summer and fall, this species regularly occurs as far
north as New York (Morreale et al. 1992); however,
records of Green Turtles at higher latitudes of the
United States are rare. While both Leatherback Tur-
tles (Dermochelys coriacea) and Loggerhead Turtles
(Caretta caretta) are commonly encountered in waters
off Atlantic Canada (e.g., Bleakney 1965), with leath-
erbacks occupying both nearshore and offshore waters
(James et al. 2005) and loggerheads mainly offshore
waters, there were no previous confirmed reports of
the Green Turtle in this region. Here we report on
photo-documented records of a Green Turtle and a
Green Turtle-Loggerhead Turtle hybrid in nearshore
waters off Nova Scotia, Canada. These exist as the
most northerly confirmed records of Chelonia mydas
in the northwest Atlantic.
Notification about both turtles initially came through
calls to a toll-free phone line established for fishing
community members in Atlantic Canada to report sea
turtle sightings (Martin and James 2005). A small,
live cheloniid turtle was reported on 8 August 1999.
The turtle was found in Chedabucto Bay, Nova Scotia
(at 45°20'37"N, 61°15'36"W, Figure 1) and was pho-
tographed and released shortly before the call was
46 - (ag
Chedabucto Bay
450 Nova Scotia 2 4
St Margarets
Ite Bay
447 ;
| eo |
a = A
FiGurE 1. Capture locations of juvenile Green Turtle (solid
circle) and juvenile Green Turtle x Loggerhead Tur-
tle hybrid (solid triangle).
placed. The turtle was not measured; however, curved
carapace length (CCL) was estimated to be between
30 and 40 cm and its mass approximately 4-5 kg.
Species identification was confirmed as C. mydas (juve-
nile) upon receipt of several excellent photographs
that depicted carapacial scute configuration and scale
patterning on the head (Figure 2).
The second turtle, also live, was reported on 2 Octo-
ber 2001. It was found in St. Margarets Bay, Nova Sco-
tia (at 44°34'56"N, 64°03'06"W, Figure 1). The animal
579
580
THE CANADIAN FIELD-NATURALIST
Vol. 118
FiGure 2. Juvenile Green Turtle (Chelonia mydas) found in Chedabucto Bay, Nova Scotia, on 8 August 1999.
was considered unusual by the inshore commercial
fishers who encountered it because they had never seen
a cheloniid turtle before. Therefore, they collected it
and brought it to shore for examination.
One of us (MCJ) responded to the report and exam-
ined the turtle (CCL 34 cm; mass 4.07 kg), tentatively
identifying it as a juvenile C. mydas. The plastron of
the turtle was cream coloured, the cutting edge of the
lower tomium was mildly serrated, and it had a pair
of large prefrontal scutes on its head (Figure 3), all
features characteristic of a Green Turtle. However,
while the number and arrangement of carapacial scutes
was consistent with those of a Green Turtle, there
were two claws on the anterior margin of each front
flipper, the costal and vertebral scutes overlapped con-
siderably, and the marginal scutes were strongly ser-
rated (Figure 3), which suggested that the turtle was
possibly a hybrid.
At the time of examination, the turtle’s movements
were sluggish and it was judged to be mildly hypother-
mic. Small juvenile cheloniid turtles foraging in coastal
areas of the temperate north Atlantic in the fall are
particularly vulnerable to developing hypothermia, as
water temperatures can rapidly drop below 20°C (Dav-
enport 1997). This animal was recovered from an area
where the sea surface temperature was 16.2°C. Given
the turtle’s compromised physical condition and the
declining water temperatures along the coast of Nova
Scotia, the turtle was moved to the animal care facili-
ties at Dalhousie University in Halifax, where it was
warmed and rehydrated for approximately 60 hours
in a freshwater bath at 24°C. It was then transported
south by air on the evening of 4 October 2001 for
release in Bermudian waters.
Subsequent genetic analysis at the U.S. National
Marine Fisheries Laboratory in La Jolla, California,
confirmed that this turtle was a hybrid. This was deter-
mined by sequencing a 391 bp fragment of the control
region of mitochondrial DNA (mtDNA) extracted
from a blood sample (Dutton 1996). The results revealed
that this turtle had Loggerhead Turtle mtDNA, while
phenotypically it was principally a Green Turtle. Since
mtDNA is maternally inherited, we conclude that this
animal was the progeny of a female Loggerhead Turtle
and a male Green Turtle.
Discussion
The extent to which natural hybridization in sea tur-
tles occurs has not been determined. However, as genet-
ic techniques like the ones employed here are increas-
ingly applied, hybridization may prove to be more
common than previously thought. Molecular genetics
have confirmed hybridization between the Loggerhead
Turtle and Kemp’s Ridley Turtle (Lepidochelys kempii)
(Karl et al. 1995; Barber et al. 2003), Loggerhead
Turtle and Hawksbill Turtle (Eretmochelys imbricata)
(Karl et al. 1995; Witzell and Schmid 2003), and Green
Turtle and Hawksbill Turtle (Wood et al. 1983; Karl
2004
et al. 1995). In addition to the results presented here,
there is only one previous report of hybridization
between a Loggerhead Turtle and a Green Turtle (Karl
et al. 1995). Hybridization between the Carettini and
Chelonini is extraordinary given that these tribes have
been genetically separated for 50 million years or more
(Bowen et al. 1993; Dutton et al. 1996). It has been
suggested that these may be the oldest vertebrate line-
ages known to hybridize in nature (Karl et al. 1995).
The reproductive status of marine turtle hybrids is
not known; however, the identification of potential
second-generation hybrids (Karl et al. 1995) suggests
that at least some hybrids may be fertile. Reproductive
viability in hybrids could have important biological
consequences for the conservation of marine turtles
(Karl 1996).
Both turtles reported here were of the size class typ-
ical of neritic foraging populations of Green Turtles
(i.e., straight carapace length >25 cm) (Musick and
Limpus 1997). Therefore, these animals likely arrived
in eastern Canadian waters from coastal foraging habi-
tat off the northeastern United States, rather than from
pelagic areas.
Our current understanding of juvenile Green Turtle
distribution in the northwest Atlantic suggests that these
turtles occupy areas where sea surface temperature is
normally higher than that of coastal Atlantic Canada.
In the case of the hybrid turtle, the Loggerhead Turtle
component of its genotype may have been responsible
for directing the animal to higher latitudes for for-
aging, as Loggerhead Turtles are commonly encoun-
tered in Atlantic Canadian offshore waters. However,
the animal’s presence in nearshore waters off Nova
Scotia remains puzzling. Loggerhead Turtles are rarely
encountered in coastal areas of Atlantic Canada be-
cause sea surface temperatures are normally at or
below the lower thermal tolerance limits of this species.
There was no formal attempt in eastern Canada to
specifically promote the reporting of marine turtle
sightings until 1998, when a broad public education
program and toll-free reporting line were established
JAMES, MARTIN, and DUTTON: GREEN TURTLE IN ATLANTIC CANADA
The large
pair of prefrontal scutes on the head (left) are characteristic of Chelonia mydas. However, overlapping costal and
vertebral scutes and strongly serrated marginal scutes (right) are not characteristic of Chelonia mydas.
for this purpose (Martin and James 2005). Continued
collaboration with commercial fishers will be key to
determining if the records reported here represent
accidental occurrences of the Green Turtle in this
region, or if small numbers of this species regularly
forage along the Scotian Shelf in summer and early
fall when inshore water temperatures are highest.
Acknowledgments
We thank K. Horne, A. Harnish and P. Young for
reporting the turtles described here to the Nova Sco-
tia Leatherback Turtle Working Group. Thanks are
also extended to C. Harvey-Clark for treating the
hybrid turtle at Dalhousie University’s Animal Care
facilities and to J. Conway (Maritime Aquatic Species
at Risk Office), K. Eckert (Wider Caribbean Sea Turtle
network) and J. Gray (Bermuda Aquarium Museum
and Zoo) for facilitating the transport to and subse-
quent release of this turtle in Bermudian waters. We
thank S. Mockford (Dalhousie University), R. Le Roux
and E. La Casella (National Marine Fisheries Service)
for assistance with genetic analysis and R. Myers
(Dalhousie University) for helpful comments on earli-
er drafts of the manuscript. We acknowledge support
from World Wildlife Fund Canada, George Cedric
Metcalf Charitable Foundation, Canadian Wildlife
Federation, U.S. National Marine Fisheries Service,
the Habitat Stewardship Program for Species at Risk,
and the Natural Sciences and Engineering Research
Council of Canada (scholarship to M.C.J.). This work
was conducted under Department of Fisheries and
Oceans License #2001-425.
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Louis, Jr. 2003. Natural hybridization between a Kemp’s
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(Caretta caretta) confirmed by molecular analysis. Che-
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assessment and conservation relevance. Proceedings of
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Martin, K., and M. C. James. 2005. Conserving sea turtles
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Standora. 1992. Annual occurrence and winter mortality
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Musick. CRC Press, Boca Raton, Florida.
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Received 26 January 2004
Accepted 6 December 2004
A Snow-tracking Protocol Used to Delineate Local Lynx, Lynx
canadensis, Distributions
JOHN R. SQUIRES, KEVIN S. MCKELVEY, and LEONARD F. RUGGIERO
U.S. Forest Service, Rocky Mountain Research Station, Forestry Science Laboratory, P.O. Box 8089, Missoula, Montana 59807
USA. jsquires @fs.fed.us
Squires, John R., Kevin S. McKelvey, and Leonard F. Ruggiero. 2004. A snow-tracking protocol used to delineate local lynx, Lynx
canadensis, distributions. Canadian Field-Naturalist 118(4): 583-589.
Determining Canada Lynx (Lynx canadensis) distribution is an important management need, especially at the southern extent
of the species range where it is listed as threatened under the U. S. Endangered Species Act. We describe a systematic snow-
track based sampling framework that provides reliable distribution data for Canada Lynx. We used computer simulations to
evaluate protocol efficacy. Based on these simulations, the probability of detecting lynx tracks during a single visit (8 km
transect) to a survey unit ranged from approximately 0.23 for surveys conducted only one day after snowfall, to 0.78 for surveys
conducted 7 days after a snowfall. If the survey effort was increased to three visits, then detection probabilities increased
substantially from 0.58 for one day after snowfall to about 0.95 for surveys conducted 7 days after a snowfall. We tested the
protocol in the Garnet Range, Montana, where most lynx were radio-collared. We documented a total of 189 lynx tracks during
two winters (2001-2003). Lynx distribution based on snow-track surveys was coincident with the area defined through radio
telemetry. Additionally, we conducted snow-track surveys in areas of western Wyoming where lynx were believed present but
scarce. We detected a total of six lynx tracks during three winters (1999-2002). In Wyoming , where lynx presence was inferred
from a few tracks, we verified species identification by securing genetic samples (hairs from daybeds) along track-lines.
Key Words: distribution, forest carnivore, Canada Lynx, Lynx canadensis, snow-track, Montana, Wyoming, surveys.
Listing Canada Lynx (Lynx canadensis) as “Threat-
ened” in the U. S. under the Endangered Species Act
compels land managers to consult with the U.S. Fish
and Wildlife Service regarding potential impacts of
management actions (Federal Register, Volume 63,
Number 130). One of the most fundamental informa-
tion needs is to delineate the current distribution of
lynx in the contiguous United States. Definitive range
determination for rare and elusive carnivores, like the
lynx, is difficult and may require several well-tested
survey methods. The National Lynx Survey uses hair-
collection pads (McDaniel et al. 2000) as a means of
detection over large areas including much of the north-
ern and western portions of the United States (K. S.
McKelvey). DNA analysis of collected hair provides
positive species identification (Mills et al. 2000), and
is the only tested detection method during non-snow
periods for lynx. However, unless multiple samples are
obtained from a site, the method cannot distinguish
local populations from single dispersing individuals,
an important issue for land managers.
Snow-tracking provides a survey method for detect-
ing lynx during the winter (Halfpenny et al. 1995;
Zielinski and Kucera 1995). Unlike hair-pad surveys,
snow track surveys do not require a behavioral re-
sponse, like rubbing, for detection. Lynx also have many
attributes that make them particularly good candidates
for snow-track surveys: lynx from southern populations
have large spatial-use areas (approximately 150 km? for
males and 70 km? for females; Aubry et al. 2000); have
high daily travel rates (Ward and Krebs 1985; Mowat
et al. 2000); and a distinctive snow-track that facilitates
identification (Halfpenny and Biesiot 1986; Forrest
1988). Snow-tracking also provides anecdotal infor-
mation, such as identification of family groups, useful
for distinguishing local populations from dispersing
individuals.
Snow tracking has been used extensively to survey
lynx and other forest carnivores (Thompson et al. 1989;
Stephenson and Karczmarczyk 1989; Beier and Cun-
ningham 1996; Becker et al. 1999), but, like other detec-
tion techniques, snow-track surveys have inherent
strengths and weaknesses. Snow track surveys can be
conducted across extensive landscapes at reasonable
costs, and the method is sensitive to changes in carni-
vore occupancy. However, potential problems with
snow-track surveys include track misidentification and
difficulties in achieving representative surveys (Half-
penny et al. 1995; Zielinski and Kucera 1995). For ex-
ample, Aubry and Lewis (2003) found that unscreened
records of Fishers (Martes pennanti) that presumably
included many “false positives” yielded a different,
and much more extensive, distribution when compared
to verified records. Misidentifications can also have
serious management impacts if the detected species
is listed as Threatened or Endangered under the U. S.
Endangered Species Act.
Here, we describe and evaluate a track-based survey
method for lynx and its potential limitations. Our goal
was to develop a reliable and representative winter sur-
vey method to complement existing summer surveys.
Specifically, we needed to improve on existing snow-
583
track survey methodologies to ensure they are repre-
sentative in terms of their spatial extent and habitat
coverage, and to address problems of track misidenti-
fication by incorporating genetic sampling (i.e., scats
and hairs frozen in tracks and daybeds). To evaluate
reliability we tested these methods both through com-
puter simulation and through direct comparisons with
radio-telemetry data in an area where most lynx were
radio-collared.
Study Areas
We conducted lynx surveys in the Garnet Mountain
Range of western Montana, and in the Wyoming/Salt
River Mountains approximately 80 km southwest of
Jackson, Wyoming. Approximately 80% of the Garnet
Range is forested within the Douglas-fir (Pseudotsuga
menziesii) and Subalpine Fir (Abies lasiocarpa) series
of the Montana Forest Habitat type (Pfister et al. 1977;
Burcham et al. 1999). Dominant tree species include
Subalpine Fir, Engelmann Spruce (Picea engelmannii),
Lodgepole Pine (Pinus contorta), and Douglas-fir. Ele-
vations range from 1160 to 2090 m. The primary use of
forested public and private lands is timber management,
and much of the area was extensively logged within the
past 25 years. The Garnet Range is adjacent to private
lands that consist mainly of irrigated hay fields and
Big Sage Brush (Artemisia tridentata) — wheat grass
(Agropyron spp.) cover types.
The Wyoming and Salt River ranges, located in west-
central Wyoming, support mixed conifer forests that
include Subalpine Fir, Engelmann Spruce, Lodgepole
Pine, Whitebark Pine (Pinus albicaulis), Douglas-fir,
and Quaking Aspen (Populus tremuloides). Mesic sites
are dominated by Subalpine fir and Engelmann Spruce
forests in seasonally moist or wet areas, or where sub-
irrigation maintains a high water table. Spruce-fir forests
are typically co-dominant with Lodgepole Pine. Dry
sites are dominated by Lodgepole Pine forests, often
intermixed with Douglas-fir and Quaking Aspen. Pre-
THE CANADIAN FIELD-NATURALIST
Vol. 118
cipitation is mostly in the form of snow; elevations
range from 1981 — 3353 m.
Methods
Modeling Track Detections
We estimated the probability of detection relative
to search effort using computer simulation to model
track detections based on the tortuosity of actual lynx
tracks. As part of our research, we __ back-
tracked 15 radio-collared lynx and mapped their tracks
using a Trimble GEO Explorer II with data points
taken at 2 s intervals. We randomly selected one 3-km
track from each lynx and calculated the average track
tortuosity by dividing total length by the linear dis-
tance traveled (Turchin 1998). This result was used
when generating simulated tracks to ensure realistic
track tortuosity.
Computer simulations required that we estimate daily
travel distances of lynx. Daily movements as meas-
ured by radio telemetry are shorter than the animal’s
actual movement because of unrecorded tortuosity.
In general, reported daily movements of lynx ranged
from 1-9 km as measured using various methods,
with most estimates from 1-4 km (Table 1). For mod-
eling, we assumed that daily movements varied ran-
domly from 1.0-4.0 km (z= 2.5 km). We chose a con-
servative estimate of daily movements to better ensure
that our model results addressed locating lynx at low
densities where tracks were uncommon. A uniformly-
distributed random number was drawn from this range
for each trial. A simulated day’s movement was com-
pleted when the linear distance traveled between the
day’s start and the current location exceeded the drawn
random number. The program continued in this man-
ner counting the number of days elapsed until the
survey transect intersected a simulated track, and the
number of elapsed days was written to an output file.
Simulated tracks began at random locations within
hypothetical, circular home ranges of 100 km? with
TABLE |. Reported daily distances for lynx movement; only winter movements were included where both summer and win-
ter movements were reported.
Study Distance (km)
Parker et al. 1983 8.8, male
7.6, female
6.5, juvenile
Ward and Krebs 1985
2.7 (95% CI = 1.8-3.7), hares common
Method
Cumulative distance based on 2 hour relocations
Daily telemetry locations
2.4 (95% CI = 2.0-2.9), hares uncommon
Brittell et al. 1989 1.0, (range = 0.02-7.4), males
0.7, (range = 0.02-4.0), females
3.8 (sd = 0.6), male
3.0 (sd = 0.4) female
Apps 2000
Mowat et al. 2000
Squires and Laurion 2000
5-9 reported average of multiple studies
2.8 (range = 2.5-3.3), 4 Montana males
Daily telemetry locations
Daily telemetry locations
Snow tracking
Daily telemetry locations
3.2 (range = 2.5-3.9), 3 Montana females
2.7 (range = 0.7-9.5), Wyoming male
2.2 (range = 0.3-5.2), Wyoming female
2004
an initial random direction. The length of simulated
tracks was evaluated using travel distances that would
be expected if we assumed that 1, 3, or 7 days had
elapsed since the most recent snowfall.
The survey route was modeled as a straight, 8-km
transect, randomly located within the 100 km? home
range. The entire transect was incorporated into the
home range, an assumption based on the study design
in which the simulated survey track would be repli-
cated within each cell of a contiguous grid. Hence, at
least 8 linear km of survey track would be found in
any arbitrary 100 km? circular area within the survey.
Snow-track Protocol
We used GIS to establish an 8 x 8 km grid across
each survey area to define sample units. The size of
this sample unit was slightly smaller than a typical
female home range (Aubry et al. 2000) and was em-
ployed to reduce the chance of missing individuals,
but was still efficient for searching large landscapes
(Zielinski et al. 1995). Female lynx typically have small-
er home ranges than males (Koehler 1990; Poole 1994;
Slough and Mowat 1996). Establishing a grid of sur-
vey units covering the study areas ensured that our
search effort was spatially well distributed across avail-
able habitats (Zielinski et al. 1995). After establishing
the sample grids, we assigned a high or low priority to
sampling units based on dominant habitat-type. Sam-
ple units in moist, Subalpine Fir forests were a high
priority because these stands are more heavily used by
lynx than drier forest types (McKelvey et al. 2000).
Our protocol specified that “high” priority
units be surveyed at least twice per winter (Halfpenny
et al. 1995). Open-forest types, such as dry Lodgepole
Pine, Quaking Aspen, and Ponderosa Pine (Pinus pon-
derosa), were “low” priority and were only searched
once per winter. Open habitat types (large park lands,
sage brush, tundra, agriculture) and high elevation sites
(tundra, rock, and ice) are rarely used by lynx (Koehler
1990; Aubry et al. 2000; McKelvey et al. 2000) and
were not surveyed.
Observers primarily searched for animal tracks by
traveling 15-20 km/hr on roads and trails using snow-
mobiles. We saw no evidence that lynx were reluctant
to cross snowed-in logging roads and trails (Squires;
unpublished data; see also O’Donoghue et al. 1998).
Survey units that could not be surveyed by snowmobile
were searched on snowshoes to the extent possible.
The protocol specified that we search 10 km in each
8 x 8 km sample unit choosing routes that preferen-
tially traversed forested habitats with high horizontal
cover. This search effort per sample unit was sufficient
to traverse key areas within the unit, but still allowed
us to efficiently search multiple sample units per day.
High horizontal cover is an important component of
Snowshoe Hare (Lepus americanus) habitat, the domi-
nant prey species of lynx (Hodges 2000). Sample units
that contained only dry, open forests were surveyed
using routes that best bisected the search area.
SQUIRES, MCKELVEY, and RUGGIERO: SNOW-TRACKING PROTOCOL
585
Our goal was a representative survey of sample units
that were spatially well distributed across available
habitats, while preferentially searching the best habitats
in each unit to maximize the chance of detecting lynx.
We recorded the locations of all lynx tracks and the
tracks of other carnivores using a Trimble GEO Ex-
plorer Il GPS. Multiple crossings known to be the same
animal and <100 m apart were recorded as a single
detection. We measured (stride, straddle, length, width,
depth; Halfpenny et al. 1995) and photographed all rare
carnivore tracks to provide documentation. Track mis-
identification is a potential problem of snow-based
surveys (Zielinski and Kucera 1995; Halfpenny et al.
1995), especially in areas where the species of interest
is rare. We collected genetic samples (e.g., hairs, scats)
from snow-tracks on the Wyoming study area to pro-
vide unequivocal documentation. To collect genetic
samples, we followed presumed lynx tracks in search
of scats or day beds. We carefully removed loose snow
from daybeds until we reached the frozen bed layer.
We then thoroughly searched the snow surface and used
tweezers to secure hairs frozen in the snow. Hairs were
stored in desiccant until the Rocky Mountain Research
Station’s Wildlife Genetics Laboratory, Missoula, Mon-
tana, extracted and analyzed DNA samples.
Snow-track surveys require trained personnel to be
effective (Zielinski and Kucera 1995). We trained ob-
servers at our long-term lynx study area near Seeley
Lake, Montana. Observers back-tracked radio-collared
lynx to practice identifying tracks under diverse envi-
ronmental conditions (e.g., forest type, snow conditions,
topography). Following this training, we assumed that
all observers could recognize lynx tracks.
Survey Verification
In the Garnet Range, we used radio-telemetry data to
determine if the distribution of lynx within the study
area was coincident with survey results. Lynx were
trapped using specially designed box traps baited with
carrion, beaver castor, and pie plates and wings for
visual lures (Kolbe et al. 2003). Trapping was conduct-
ed throughout the winters of 2001-02 and 2002-03.
Lynx were chemically immobilized using a syringe
pole to administer a mixture of ketamine (10 mg/kg
Ketaset®; concentration 100 mg/mL) and xylazine
(1 mg/kg; concentration 100 mg/mL); this dose pro-
duced predictable immobilization periods (30-40 min-
utes) and stable vital signs. We fitted adult lynx with
VHF radio transmitters (170 g), weighed, measured,
and extracted blood from each for future DNA analy-
sis. Kittens were fitted with a padded, 100 g collar that
allowed for growth. We monitored lynx movements
using aerial telemetry (90% of locations) approximately
twice per month augmented with ground-based tel-
emetry.
We combined all relocation points and calculated a
95% kernel home range to delineate the distribution of
the local lynx population based on telemetry (Worton
1989; Seaman et al. 1999). We then overlaid a 95%
586
fixed kernel home range on the distribution of lynx,
as delineated by snow tracking, to determine if the
two methods yielded coincident distributions.
Results
Simulations of track detections
Computer simulations of track detections indicated
different asymptotic relationships between the proba-
bility of detection and survey effort (number of visits
per winter), based on the time between snowfalls suf-
ficient to obliterate tracks (Figure 1). The probability
of detecting lynx tracks during a single visit (8 km
transect) to a survey unit ranged from approximately
0.23 for surveys conducted only one day after snow-
fall, to 0.78 for surveys conducted 7 days after a snow-
fall. If the survey effort was increased to three visits,
then detection probabilities increased substantially from
0.58 for one day after snowfall to about 0.95 for surveys
conducted 7 days after a snowfall. Even a modest sur-
vey effort of two visits would detect tracks approxi-
mately 80% of the time, provided more than 3 days
had passed since the last snowfall.
Field test — Garnet Range, Montana
During winters 2001-2002 and 2002-2003, we sur-
veyed for lynx on 242 km and 438 km of roads and
trails, respectively. We documented 37 track detections
of lynx in 4 of 12 survey units during winter 2001-
2002, and 37 detections in 4 of 16 survey units during
winter 2002-2003. In addition, we observed 115 lynx
tracks during winter 2001-2002 and 53 in 2002-2003
in survey units, but not during the formal survey. These
detections were made during trapping and related trav-
el. We encountered a higher number of track-cross-
ings during trapping because we only trapped in
areas of high lynx use. The average elevation where we
located lynx tracks was 1839 m (SD 97, range 1443 —
2012 m).
We trapped five lynx during winter 2001-2002, and
two additional individuals during winter 2002-2003.
We believed this sample of radio-collared individuals
was a local census of lynx in the Garnet Range based
on trapping results, recaptures, and field observations,
but we could not formally test this perception.
Field test — Wyoming and Salt River Ranges, Wyoming
We conducted track-surveys for lynx in Wyoming
during the winters of 1999-2000, 2000-2001, 2001-
2002. During winter 1999-2000, we surveyed 1055 km
in 32 sample units, and we detected one lynx track in
the Salt River Range and a second track in the north-
eastern portion of the Wyoming Range. In addition,
tracks from a family group were observed in the north-
eastern portion of the Wyoming Range by Wyoming
Game and Fish Department biologists (B. Oakleaf,
personal communication 2000). During winter 2000-
2001, we surveyed 1103 km in 37 sample units, and
4 lynx tracks were detected in the northeastern portion
of the Wyoming Range, and one set in the southwestern
THE CANADIAN FIELD-NATURALIST
Vol. 118
©
fo)
Probability of detecting lynx
oO
(op)
Number of visits
FIGURE |. Computer-modeled relationship between the proba-
bility of detecting lynx and the number of visits to an 8 km
survey transect pixel relative to the number of days since
last snow.
Salt River Range. We surveyed 1080 km in 34 sample
units during winter 2001-2002 and detected no lynx.
Two tracks located during the 1999-2000 survey
looked like lynx, but were poorly defined with each
impression being a pedestal above the snow surface
as a result of wind scouring. We followed two tracks
for approximately 200 m until we located daybeds and
collected five hairs. Two of the hairs contained suffi-
cient DNA to amplify and the species identification
was verified as lynx.
Survey Verification
The distribution of lynx in the Garnet Range, as de-
fined by a 95% fixed kernel home range of all marked
animals (n= 96 locations from 7 individuals, = 14 loca-
tions per individual, Figure 2B) combined, subsumed
97% of all tracks detected during snow-track surveys.
The general distribution of lynx in the Garnet Range
as defined by radio telemetry and snow-track surveys
was coincident (Figure 2A).
We documented too few lynx detections in the Wy-
oming and Salt River ranges to delineate a distribution
based on snow-track surveys. However, biologists with
the Wyoming Game and Fish Department trapped two
lynx in the northeastern portion of the Wyoming Range
during the winter of 1996-1997 (B. Oakleaf personal
communication 2000). The winter home ranges of these
two individuals were restricted to the northeastern por-
tion of the Wyoming Range in the same approximate
area as 5 of the 7 track detections from our survey.
Discussion
Snow-tracking has been used to document the pres-
ence/absence of carnivores (Zielinski and Kucera 1995),
and continues to be an important technique, especially
when the organisms of interest are rare and difficult
to observe. One primary appeal of using track-based
surveys for presence/absence sampling is the method’s
2004 SQUIRES, MCKELVEY, and RUGGIERO: SNOW-TRACKING PROTOCOL 587
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f y © Lynx Telemetry Locations s Drummond
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| 95% Fixed Kernal Home Range (Telemetry - See Above)
Sa a
FicurE 2. The local distribution of lynx in the Garnet Range delineated from: (A) radio telemetry of all individuals com-
bined (95% fixed kernal, n = 96 locations from 7 individuals, x = 13 locations per individual) compared to, (B) the local
distribution based on sample units with track detections.
588
sensitivity to changes in use patterns, especially for
species like lynx that are highly mobile and have large
home ranges (Ward and Krebs 1985; Poole 1994; Slough
and Mowat 1996; Aubry et al. 2000). Changes in lynx
occupancy can be quickly detected across extensive
areas using snow-track surveys. For example, general
occurrence data from 1842-1998 suggested that lynx
had a long-term history of occupancy in the Salt River
and Wyoming Ranges (see McKelvey et al. 2000: Fig-
ure 8.17), and the perception that lynx were currently
distributed throughout the Wyoming and Salt River
Ranges was shared by local managers. Snow-track sur-
veys conducted in a representative manner throughout
the Wyoming and Salt River Mountain ranges provided
evidence that lynx were present in 1999, and this result
was confirmed using genetic analyses in 2000. How-
ever, the low overall detection rate coupled with the lack
of tracks in 2001 indicated that lynx were rare and
only located in a small area in the northern part of the
Wyoming range.
In areas with many track detections, snow-track sur-
veys can yield more than simple presence/absence data.
Results from the Garnet Range demonstrated that snow-
track surveys conducted in a representative manner can
also be used to delineate the local distribution of lynx.
The high overlap in distributions determined through
telemetry and survey data suggested that snow-track
surveys can at least coarsely define the local distribu-
tion of lynx (Figure 2). We acknowledge that survey data
are more limited than telemetry data given that only
winter movements are documented and the resulting
distribution is coarse-scale relative to the sample unit.
However, even a coarse-scale understanding of local
distributions is useful to habitat managers. Thus, based
on our data in the Garnet Range, we believe that snow-
track surveys that are spatially well distributed across
all available habitats can be used to estimate the local
distribution of lynx during the winter.
If lynx are abundant in an area, a 5% misidentification
rate would have little impact on management decisions.
However, in areas where lynx are very rare, a track
misidentification can have serious management rami-
fications. One way to address the chronic problem of
track misidentification is to view the track as a “‘col-
lection device” for obtaining genetic samples rather
than a primary method of species identification. Genet-
ic verification provides definitive species documentation,
regardless of the observer’s ability to identify rare car-
nivores based on track characteristics. We therefore rec-
ommend that genetic identification be included when-
ever proper identification of an individual set of tracks
is critical.
Snow-track surveys are labor intensive, and we have
only used this method at a mid or “meso” spatial scale,
where we searched all sample units. Such an intensive
approach would be impractical across large landscapes,
for example a large portion of a state. Although we
have not conducted a snow-track based survey at a
THE CANADIAN FIELD-NATURALIST
Vol. 118
“state” scale, adaptive cluster sampling may provide
a promising method of achieving a representative sam-
ple across very large landscapes (Thompson 1992).
Adaptive cluster sampling is effective for delineating
clumped distributions, which we believe is the case for
lynx at the southern extent of the species’ range (Aubry
et al. 2000).
Snow-track surveys are often conducted when track
characteristics are most distinctive, usually within a
day or two following fresh snowfall. This constraint
limits the utility of snow tracking because the proba-
bility of detecting lynx and other rare carnivores is a
function of the time since last snow. The more time
that lynx have to travel and establish long tracks, the
more likely it is that their tracks will be detected on a
survey route. For example, our simulations suggest
almost a 100% probability of detecting lynx in two
entries 7 days after a snowfall compared to a 43%
probability of detection if the area was searched 1 day
from snowfall (Figure 1). In the areas we surveyed, snow
accumulations over 5 cm were recorded on 22 and 24
(17-18%) of the days for the Garnet and Wyoming
ranges, respectively, and the snow-free periods
between storms varied from 4-6 days (U.S.D.A., Nat-
ural Resources Conservation Service, SNOTEL data).
The ability to correctly identify “old” tracks by incor-
porating genetic samples allows biologists to survey
for rare carnivores when the probability of detection
is high, even under poor tracking conditions.
The winter surveys that we used to detect lynx in
Wyoming and Montana had the following key ele-
ments: (1) sample units were representative in terms
of spatial coverage, but still focused on high-quality
habitats that maximize lynx detections; (2) search
effort per survey grid was defined and consistent across
the survey area; (3) search intensity was consistent
with simulated results indicating a high probability
of detection, (4) technicians were well trained in track
identification and data recording; (5) track identifica-
tions were rigorously documented and spatially ref-
erenced; and (6) lynx tracks were searched for genetic
samples to confirm identification. We believe that sur-
veys having these characteristics can be used to rigor-
ously define the range of local lynx populations, and
could be extended to the regional scale using adap-
tive cluster sampling.
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Received 4 February 2004
Accepted 17 August 2004
Hummock Vegetation at the Arctic Tree-line near Churchill, Manitoba
JORG TEWS
Institute of Geography, University of Erlangen-Niirnberg, Kochstr. 4/4, 91054 Erlangen, Germany
Current address: Geomatics and Landscape Ecology Research Laboratory (GLEL), Department of Biology, Carleton University,
1125 Colonel By Drive, Ottawa, Ontario K1S 5B6 Canada
Tews, Jérg. 2004. Hummock vegetation at the arctic tree-line near Churchill, Manitoba, Canadian Field-Naturalist 118(4):
590-594.
Hummocks, small earth or peat mounds, are widely distributed in the arctic and develop as a consequence of biomass accumulation
and cryoturbation in the active layer. There is general agreement that the type of vegetation covering peat hummocks may
alter the accumulation rate of organic material and thus hummock growth and local carbon sink dynamics. Studies on hummock
plant community compositions from the arctic are very scarce. Here, I present results of a case study from the arctic tree-line
near Churchill, Manitoba (Canada). Vegetation composition, hummock height and soil moisture content were recorded in
40 peat hummocks located along a tree-line gradient from open forest to tundra. Based on a cluster analysis I found three
moss-dominated types of hummock vegetation, according to (1) a Tomenthypnum nitens (golden fuzzy fen moss) type on
low hummocks, (2) a Hylocomium splendens (stair-step moss) type on medium-sized hummocks, and (3) a Pleurozium schreberi
(red-stemmed feathermoss) type on hummocks higher than 60-70 cm. I found hummock height to increase towards the forest
interior with decreasing water content of the upper organic layer on the hummock top. This is indicated by a significant change
in vegetation composition towards drought resistant moss species on higher hummocks. Furthermore, species richness decreased
with increase in hummock height. Based on evidence from historical tree-line invasion the overall results suggest that hammock
height increases due to peat accumulation over the course of time resulting in a typical change in plant community composition.
Key Words: peat hummocks, Tomenthypnum nitens, Golden Fuzzy Fen Moss, Hylocomium splendens, Stair-step Moss, Pleu-
rozium schreberi, Red-stemmed Feathermoss, subarctic, forest-tundra ecotone, Hudson Bay Lowlands, Manitoba.
Hummocks are small, up to 1 m high soil mounds
widely distributed in the northern boreal, sub-arctic
and arctic permafrost regions (e.g., Lundquist 1969;
Mackay 1980). Generally, two types of hummocks can
be classified: earth hummocks and peat hummocks.
Earth hummocks may develop as a result of frost heave
and cryoturbation processes where the organic layer
overlies fine-grained frost-susceptible soils (Quinton
et al. 2000). In contrast, peat hummocks grow as the
result of the accumulation of organic material and
where the surface of the uppermost mineral layer inside
the hummock is positioned below the surrounding
ground level (see Dredge 1992). Both hummock types
may be perennially frozen or, as a result of warmer
summer climate and lower latitude, completely thawed
(Zoltai and Pettapiece 1974; Tarnocai and Zoltai 1978).
As a transitional form they may be partially frozen with
ice lenses remaining in the hummock core during the
summer period.
Even though hummocks are a common landscape
feature and hummocky terrain covers a large proportion
of Arctic Canada (Tarnocai and Zoltai 1978), scientific
studies focusing on the vegetation structure of peat
hummocks are very scarce. This lack of empirical data
and also the potential role of peat hummocks for the
carbon dynamics in the northern hemisphere empha-
size the need to investigate the spatial distribution of
major hummock plant community types. Besides the
prevailing local climate, carbon storage in the arctic
is strongly influenced by vegetation composition and
succession (see Camill et al. 2001). Thus, in order to
appreciate carbon dynamics in the northern hemisphere
acknowledge of potential carbon sinks (such as peat
hummocks) and their major plant community types are
necessary. This enables evaluation of ecological factors
which may alter accumulation or decomposition rates
of organic material and related carbon dynamics. For
example, mosses which often dominate hummock veg-
etation have the potential to play a key role in modifying
decomposition rates and the thermal and hydrological
regime of arctic soils (Beringer et al. 2001). Here, I
present results of a case study on vegetation composi-
tion, succession and physiognomy of 40 peat hum-
mocks located along an arctic tree-line transect from
tundra to open forest in the Hudson Bay Lowlands
near Churchill, Manitoba (Canada).
Methods
Study area
The study site is situated at the open forest tree-line
near Twin Lakes, a flat-topped glacial kame deposit
approximately 25 km southeast of the town of
Churchill (Figure 1). The open forest vegetation is com-
posed of a mix of Tamarack (Larix laricina [Du Roi]
K. Kock) and White Spruce (Picea glauca [Moench]
Voss) with interspersed Black Spruce (Picea mariana
[Mill.] Britt Sterns & Pogg). The present tree line
north of Twin Lakes is extended into a wet sedge fen
590
2004
roy
udson|Bayss
S
=
es
SiS
apa
ov
Twin Lakes
FiGuRE |: Location of the study site in the Hudson Bay
Lowlands near Churchill in northeastern Manitoba
(Canada).
predominated by Carex aquatilis (Water Sedge) and
Carex limosa (Mud Sedge). The current position of the
tree-line has moved up to 150 m towards the open
_ sedge fen within the last 70 years (see Scott et al. 1987).
_ Here, the current tree-line is composed of L. laricina
which established during the latest forest invasion.
_ Whereas young L. laricina tree-line stands are char-
acterized by small hummocks, the open forest interior
towards Twin Lakes is dominated by mature P. glauca
trees on typically hummocky terrain with large hum-
_ mocks and inter-hummock, water-filled troughs. The
nomenclature for plants follows after Porsild and
Cody (1980).
_ Sample design
During July 1999 I established a 250 m transect from
the open sedge fen towards the forest interior. I sam-
pled each hummock (total 40) that occurred within a
5 m wide corridor along the transect line. For each
hummock I measured its height from the top to the
base. Vegetation composition was studied by using a
_ frame placed on top of each hummock. The frame size
0.5 * 0.5 m was small enough to cover the tops of the
smallest hummocks. For larger hummocks I chose
homogeneous parts of the vegetation on the hammock
top. Vascular plant cover within the sampling frame
was then estimated for each plant species separately
_ using the decimal Londo-scale (Londo 1984). Within
each frame soil samples were taken from the upper
organic layer (5 cm — 20 cm depth) during one sam-
pling day and then water content gravimetrically deter-
mined (samples were 24h oven-dried at 95°).
Statistical analysis
To group species datasets Mulva’s minimal variance
clustering technique using van der Maarel’s coefficient
was used (Wildi and Orléci 1996). Simple linear regres-
sion was used to examine the relationship between
hummock height as an independent variable and water
content, species richness, and similarity of species com-
TEWS: HUMMOCK VEGETATION AT THE ARCTIC TREE-LINE
59]
position (species turnover rate) as the dependent vari-
ables. For the species turnover rate between sample i
and j hummocks were ranked by height and / defined
according to:
B=
where / is the number of species that disappeared
between sample i and j and g the number of new species.
l+g
i+]
eqn |,
Results
Hummocks are a dominant micro-topographical fea-
ture at the open forest tree-line. For the transect area I
found a mean density of 320 hummocks ha’!. However,
density was significantly higher in mature P. glauca
stands towards the open forest. The majority of hum-
mocks were predominately covered by either one of
the moss species Tomenthypnum nitens (Golden Fuzzy
Fen Moss), Hylocomium splendens (Stair-step Moss)
or Pleurozium schreber (Red-stemmed Feathermoss)
whereas herbaceous plants where less frequent. This
was confirmed by a resemblance matrix of a cluster
analysis for 40 sample plots (Figure 2). The Tomen-
thypnum nitens-group was mainly composed of Poly-
gonum viviparum (Alpine Bistort), Eguisetum varie-
gatum (Variegated Scouring-rush), Andromeda polifolia
(Dwarf Bog-rosemary), and Carex aquatilis (Water
Sedge), indicating somewhat wet conditions (see Table
1). In contrast, hammocks with Hylocomium splendens
had a more or less Dwarf Shrub dominated cover with
species such as Vaccinium vitis-idaea (Lingonberry),
Ledum groenlandicum (Common Labrador Tea), and
the lichen Cladina rangiferina (Grey Reindeer Lichen).
The third major group was dominated by Pleurozium
schreberi associated with Betula glandulosa (Dwarf
Birch) and the grass Calamagrostis canadensis (Blue
Joint), indicating somewhat dry conditions.
The species groups that were revealed by the clus-
ter analysis showed significant affiliation in terms of
transect position and respective hummock height. The
Tomenthypnum nitens-group was mainly found on low
hummocks (see Table 1) located near the tree-line (Fig-
ure 3a). Here, the organic layer on hummock tops was
mostly saturated (Figure 3b), typical for the hydro-
logical situation near the sedge fen. Hummocks with
Hylocomium splendens had medium-sized heights
and an intermediate transect position, whereas Pleu-
rozium schreberi-hummocks with heights above 60 cm
where predominately found in the open forest interior.
Overall, there was an increase in hummock height
towards the open forest (Figure 3a, R? = 0.57). Increase
in height had a significant negative effect on organic
layer water content (Figure 3b, R*= 0.46). In terms of
patterns of plant species richness, species number de-
creased with increase in hummock height (Figure 3c,
R? = 0.42; see also Table 1). Total number of plant
species found, including mosses and lichens, was 45,
and 8.1 species per sample plot on average. More-
over, intermediate hummock heights were indicated
592
-4.66E-02
4.66E-01
9.79E-01
31
26
22
34
28 oa
27
Tomenthypnum 20
nitens -
Gruppe 21
Pleurozium
schreberi -
Gruppe
Hylocomium
splendens -
Gruppe
a ee | ee eee]
9.79E-01 4.66E-01 -4.66E-02
FiGuRE 2: Cluster analysis of 40 hummock vegetation sam-
ples. Three moss-dominated plant community types are
distinctive according to the occurrence of Tomenthyp-
num nitens, Hylocomium splendens and Pleurozium
schreberi. Numbers for each sample indicate respec-
tive hummock height given in cm.
by a relatively high species turnover rate when plots
were ranked by height (Figure 3d), i.e., species com-
position showed a higher variation than vegetation of
either low or high hummocks.
Discussion
The results of this field study from the arctic tree-
line near Churchill indicate a significant relationship
between hummock height and the position along the
tree-line gradient on one hand, and hummock height
and water content, vegetation type, species richness,
THE CANADIAN FIELD-NATURALIST
Vol. 118
and species turnover on the other hand. Increasing
hummock height towards the forest interior seemed to
reduce moisture availability for mosses on the hum-
mock tops and facilitate the establishment of species-
poorer communities with drought-resistant vascular
plants. Interestingly, Zomenthypnum nitens, Hylocomi-
um splendens and Pleurozium schreberi are ubiqui-
tous moss species with a wide ecological distribution
(Nicholson and Gignac 1995). However in this study
they showed distinct distribution patterns in relation
to hummock height and soil water availability within
a relatively small area.
The plant community composition of peat hammocks
described here are the first inventory of hummock
vegetation in the Hudson Bay Lowlands, the largest
contiguous wetland in North America (Boudreau and
Rouse 1995). Other published studies are concerned
with the Mackenzie delta region where earth hummock
physiology and plant species composition is com-
pletely different. Thus, they are difficult to compare
(see e.g., Zoltai and Pettapiece 1974). It is unclear
whether peat hummocks accumulate organic material
and increase in size regardless of the local environ-
ment or whether this is driven by the micro-topogra-
phy such as the establishment of trees. However, the
local tree-line extension near Twin Lakes suggests that
once young trees establish on formerly open tundra, peat
hummocks may develop where shading and increased
moisture from trapped snow coincide with feather moss
establishment (Scott and Hansell 2002). Moreover,
the occurrence of rotten tree stumps in the subsoil of
the former centre of large, degraded hummocks (J. Tews
personal observation) may support the latter hypothesis
and is additional evidence that these hummock are
formed by organic matter accumulation, not by cryo-
genic processes as is the case with earth hummocks.
Based on this study I hypothesize that hummock
plant community composition at the tree-line near Twin
Lakes is changing in the course of hummock growth.
This is important as accumulation rates of peat (and
thus carbon dynamics) are strongly influenced by local
vegetation succession (Camill et al. 2001). Bello and
D’Souza (2000) found that with increase in hum-
mock height, accumulation rates of organic material
decrease. For an average height of 20 cm they estimated
an accumulation rate of 20 g m? year’, for 60 cm hum-
mock height only 5 g m? year". These results largely
confirm growth rates found for Tomenthypnum nitens
and Hylocomium splendens (see Busby et al. 1978).
In general, decomposition rates increase with decreas-
ing water saturation during the short summer period.
However, due to this rather small array of data, current
available data may not support proper estimates of
community-specific accumulation rates necessarty to
model large-scale spatial and temporal carbon dynam-
ics in the arctic. Thus, based on the knowledge of the
predominant types of hummock plant communities,
more studies on community-specific accumulation
rates are needed.
|
H 2004 TEWS: HUMMOCK VEGETATION AT THE ARCTIC TREE-LINE 593
| Hummock height vs. gradient position Water content
a) @ 120 b) 100,-——_____ ==
Ss ~ R“=0.462, p<0O.
5 80 a areal
oO 3)
Oo 80
2 60 ie SH Lges gs
4 40 E ro oe
i)
& 20 2 60 © e
= 1 {0)
x 50
0 ee Ale 0 20 40 60 80 100 120
Gradient [m] *f a
Tuda ————— > Open forest ummock eight [cm]
Species richness 8 — turnover rate
oii
@) 4s
a R2= 0.4209, p < 0.€ rian R* = 0.2563, p < 0.C
8 oe FS
8 10 206
oa =
= B04
ra |
che ca 0.2
5
Z, 0 0
0 20 40 60 80 100 120 0 20 40 60 80 100 120
Hummock height [cm] Hummock height [cm]
| Ficure 3: Simple regression analysis for: (3a) hummock height vs. gradient position along the tree-line from open tundra to
forest; (3b) water content of upper humus layer on hummock top vs. hummock height; (3c) total number of plant
species vs. hammock height; (3d) species turnover rate vs. hummock height.
Another current environmental issue makes the mat- agreement that global climate change will alter decom-
| ter even more complex: global climate change. On __ position rates and carbon storage (e.g., Gorham 1997;
| average, climate change in the arctic may yield more _ Earle et al. 2003). Dormann and Woodin (2002) point-
| precipitation and warmer summers (see Sonesson ed out that the driver of future change in arctic vege-
| 2002). Based on these assumptions, there is general _ tation is likely to be increased nutrient availability, aris-
Table 1: Typical species composition of hummocks at the arctic tree-line near Churchill, Manitoba. The table shows 27
characteristic hammock samples out of a total of 40 samples (13 samples with less significant community affiliation are not
| shown). Three moss-dominated plant community types are evident according to Tomenthypnum nitens, Hylocomium splendens
) and Pleurozium schreberi.
Dp ies BER Sy 6s ONO AP Aa AS 14y SANG 17; 16H 19 4 (20): 21) 22) 23) 242526 27
‘Hummock height 21 19 26 28 34 31 25 20 25 37 22 22 27 98 47 98 73 77 61 10595 76 11277 84 67 80
# of species OMe Onno SSN Oron iO CON niOnn GR Gus GuSie ae fai nlem OMS) a9 hater Ouro
_Tomenthypnum nitens Sei GUORMOeTOLOnaSrwtOe GiB bid OO Li29
Polygonum viviparum Moana Ae Onn Aw Aan Ql a2
| Equisetum variegatum Ana 2s AL 4 OE TAuL eit 4 °.2 4
| _Scirpus caespitosus ne 3 4 4
Carex aquatilis 1 1
_ Andromeda polifolia 2 1
Platanthera obtusata
_Oxyecocus microcarpus
Rubus acaulis
_ Pedicularis lapponica
Salix reticulata _
Aulacomnium palustre
Hylocomium splendens i
iS
_Vaccinium vitis-idaea CEC, Bey Abi 40 Wig ln eg!
Ledum groenlandicum 4.4 2:
_Ledum decumbens 2 ES TY 1
_Cladina rangiferina. c4iuat i PY year sar
Pleurozium schreberi (4 StS OS
_ Betula glandulosa
Calamagrostis canadensis
io
aA
594
ing for example from temperature-induced increases
in mineralization. In particular, the response of plant
growth to rising CO, levels appears to depend on nutri-
ent availability (Heijmans et al. 2002). In the arctic
vegetation nitrogen is tightly controlled by the moss
layer (e.g., Li and Vitt 1997; Sommerkorn et al. 1999).
Moreover, mosses such as Pleurozium schreberi have
been reported to be able to fix nitrogen in symbiosis
with a cyanobacterium (i.e. Nostoc sp.) (Deluca et al.
2002). Thus, increase in average summer temperatures
due to climate change and the resulting increase in min-
eralization rates may potentially decrease local carbon
storage with severe consequences for the global carbon
cycle. However, scientific research is far from estab-
lishing realistic future scenarios. For example, in the
context of our study, it was recently shown that indi-
vidual bryophyte species displayed contrasting respons-
es to changes in the nutrient supply and that they should
not be grouped as a single functional type (Gordon et
al. 2001). From this it is evident that further detailed
hummock vegetation studies are needed, particularly
in the arctic where the impact of climate change is
likely to be most effective.
Acknowledgments
I thank the Churchill Northern Studies Centre and
the Northern Research Fund (NRF) for logistical and
financial support. Special thanks go to C. Oswald and
P. Brown for their great help during the field work. I
appreciate the constructive comments on this manu-
script by two anonymous reviewers.
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Received 17 February 2004
Accepted 24 December 2004
Effects of Lodgepole Pine Dwarf Mistletoe, Arceuthobium americanum,
on Jack Pine, Pinus banksiana, Growth in Manitoba
_ Brock Epp and JACQUES C. TARDIF'!
| Centre for Forest Interdisciplinary Research (C-FIR) and Department of Biology, University of Winnipeg, 515 Avenue
Portage, Winnipeg, Manitoba R3B 2E9 Canada
‘Corresponding author
| Epp, Brock, and Jacques C. Tardif. 2004. Effects of Lodgepole Pine Dwarf Mistletoe, Arceuthobium americanum, on Jack
Pine, Pinus banksiana, growth in Manitoba. Canadian Field-Naturalist 118(4): 595-601.
| The Lodgepole Pine Dwarf Mistletoe (Arceuthobium americanum Nutt. ex Engelm.) is an important pathogen of Jack Pine
| (Pinus banksiana Lamb.). Dwarf Mistletoe alters tree form, suppresses growth, and reduces volume and overall wood quality
of its host. Stem analysis and a 3-parameter logistic regression model were used to compare the growth of heavily and lightly
to non infected Jack Pine trees. At the time of sampling, no significant reduction in diameter at breast height and basal area
were observed in heavily infected trees. However, a significant reduction in height and volume and an increase in taper were
observed in heavily infected trees. Growth models predicted a 21.1% lower basal area, 23.4% lower height and 42.1% lower
volume by age 60 for the high infection group.
Key Words: Lodgepole Pine Dwarf Mistletoe, Arceuthobium americanum, Jack Pine, Pinus banksiana, stem analysis, logistic
regression, basal area, height, volume, tree growth, productivity, Manitoba.
Le Faux—gui du pin (Arceuthobium americanum Nutt. ex Engelm.) est un important agent pathogeéne du Pin gris (Pinus banksiana
Lamb.). Le faux—gui modifie le défilement des arbres hotes, réduit leur croissance et leur volume marchand ainsi que la qualité
du bois. L’analyse de tige et la régression logistique a trois-paramétres ont été utilisés afin de comparer |’accroissement
entre les Pins Gris sévérement atteints et faiblement atteints. Au moment de |’ échantillonnage, aucune réduction significative
du diamétre a hauteur de poitrine ou de la surface terriére ne fut observée chez le groupe sévérement atteint. Toutefois, les
arbres atteints ont enregistré une baisse significative de la hauteur et du volume ainsi que du coefficient de défilement. Les
modeéles de régression ont prédit une perte de 21,1% en surface terriére, de 23,4% en hauteur et de 42,1% en volume pour
les pins gris fortement atteints par le faux—gui a un age de 60 ans.
Mots clés: Le Faux—gui du pin, Arceuthobium americanum, Pin gris, Pinus banksiana Lamb., analyse de tige, régression
logistique, surface terriére, hauteur, volume, croisssance, productivité, Manitoba.
Jack Pine (Pinus banksiana Lamb.) is an important
commercial tree species because of its pole-like growth
form, and as a pioneer species, it is relatively easy to
regenerate following harvest (Rudolph and Laidly 1990;
Sims et al. 1990). An important pathogen of Jack Pine
is Lodgepole Pine Dwarf Mistletoe (Arceuthobium
americanum Nutt. ex Engelm.). There are five species
of Dwarf Mistletoe known in Canada, of which A.
americanum is the most widely distributed, extend-
ing from British Columbia to southeastern Manitoba
(Hawksworth and Wiens 1996). Individual species of
Dwarf Mistletoe are generally host-specific, able to
infect only a few tree species. In the case of A. amer-
icanum, other susceptible hosts include Lodgepole
Pine (Pinus contorta Doug}. ex Loud.) and Ponderosa
Pine (Pinus ponderosa Dougl. ex P. & C. Laws.).
As of 1996, there were 670 000 ha of forest with
severe A. americanum infections in Alberta, Saskat-
chewan and Manitoba (Brandt et al. 1998). In Mani-
toba, approximately 8.7% of mature Jack Pine stands
in important growing regions were infected by Dwarf
Mistletoe (Baker et al. 1992). This has resulted in a loss
of up to 7.9% of the total pine volume in these regions
(525 224 m? out of 6 648 405 m°) and a loss of up to
70.3% within the infected stands. Aside from the sub-
stantial volume losses, there is also a reduction in wood
quality, making wood less merchantable. Wood of
Lodgepole Pine infected by A. americanum exhibited
greater longitudinal shrinkage and was weaker in
strength when compared to uninfected trees because of
the production of tree-rings having a lower percentage
of latewood, shorter tracheid length, and higher resin
content (Piirto et al. 1974). Generally, Dwarf Mistletoe
deprives its host of water and nutrients, thus reducing
height and diameter growth as well as seed production,
and weakening the tree (Franc and Baker 2000). Dwarf
Mistletoe alters tree form by disrupting apical domi-
nance (Tinnin and Knutson 1980) through formation
of witches’ brooms. Because Dwarf Mistletoe derives
all of its nutrients from host tissue and fixes little or
no carbon dioxide for its own use, witches’ brooms act
as sinks for metabolites produced in other parts of the
host (Hull and Leonard 1964a, 1964b). Douglas-fir and
Western Larch infected by A. douglasii and A. laricis,
respectively, exhibited a significant increase in leaf to
sapwood ratios in heavily infected trees, altering resource
395
596
allocation processes and reducing the overall water-
use efficiencies (Sala et al. 2001).
The long incubation period characterized by the
life cycle of A. americanum (Hawksworth and Wiens
1996) poses a problem in the early detection of initial
infections. In forest management situations, the current
most effective methods of treatment are removal of
heavily infected trees and isolation of infected stands
by planting buffer zones of incompatible host species
(Franc and Baker 2000). Even-aged silvicultural systems
are often effective in controlling Dwarf Mistletoe, as
the entire overstory may be removed.
No one has quantified volume losses on individual
Jack Pine trees due to infection by Dwarf Mistletoe.
One study examined the effect of A. americanum on the
growth of Lodgepole Pine (Baranyay and Safranyik
1970). Within Manitoba, Baker et al. (1992) studied
the impact of Dwarf Mistletoe on Jack Pine trees at the
stand scale, focusing on loss of wood volume in the
forest stands. The objective of this study was to com-
pare the growth of heavily infected Jack Pine trees to
that of non-infected or lightly infected Jack Pine trees
based on differences in diameter at breast height (dbh),
basal area, height, volume, and stem form. We hypoth-
esized that there was a significant reduction in total
cumulative dbh, basal area, height, and volume growth
rate in trees infected with Dwarf Mistletoe.
Methods
The sampling area is located about 97 km north-
east of Winnipeg, Manitoba (Figure |) within Belair
Provincial Forest (50°38'N, 96°29'W, 250 meters
above sea level). The underlying bedrock consists of
Archean granites and gneisses (Manitoba Geological
Survey 2002*). The closest meteorological station is
located at Pine Falls about 21 km from the sampling
area. The climate is continental (Burton et al. 1998).
The mean annual temperature for Pine Falls is 2.1°C,
and the total annual precipitation is 538.5 mm (Envi-
ronment Canada 2002*). In winters, the average min-
imum temperature reaches —23.5°C in January, and in
summers, the average maximum temperature reaches
25.3°C in July.
The sampling site consists of a small, open, fire-
originated Jack Pine stand, and is bound by Provincial
Highway 11 to the south and a recent cutover to the
north. The sample site is located near the south-eastern
limit of the lodgepole pine dwarf mistletoe geograph-
ical distribution in Manitoba (Baker et al. 1992).
Physically, the site is characterized by level, homoge-
neous terrain. The site is also homogeneous with regards
to stand origin, slope variation and understory vege-
tation. Due to the small size of the infected stand, and
the localized nature of the mistletoe infections, the
number of trees for sampling was limited. There are
epicentres of Dwarf Mistletoe infections scattered
throughout the area. Within the sampling site, there is
a relatively even scattering of heavily infected trees
THE CANADIAN FIELD-NATURALIST
Vol. 118
intermixed with lightly and non-infected trees (Fig-
ure 1).
Three transects were established approximately 50 m
apart, oriented in a north-south direction, extending
north from Provincial Hwy. 11. Ten sampling points
were randomly established along the three transects,
and the surrounding area was divided into four quad-
rants. One of the four quadrants was randomly select-
ed in which the two nearest trees to the point were select-
ed; one heavily infected tree and the nearest lightly or
non-infected tree between 40 and 60 years of age.
Trees with noticeable fire scars, fungal infections, or
injuries were avoided to minimize the effects of other
disturbances on tree growth. Trees that exhibited exces-
sive branching or forking on the main stem were also
avoided to simplify stem analysis. Trees were selected
up to 50 m from plot centre, as long as they remained
within the stand boundaries. If no trees matching our
criteria were found within the selected quadrant, sam-
pling was done in the next quadrant in numerical order.
This method helped to eliminate bias by selecting the
closest trees to the sampling points. Once candidate
trees were selected, they were numbered, marked with
a north-orientation line, marked at 0.5 m and 1.3 m, and
locations were recorded with a GPS unit (Figure 1).
Sampling took place in late July — early August 2002.
Prior to felling, the infestation index of the trees
was estimated using the Hawksworth 6-class system
(Hawksworth 1977). Infection was most easily deter-
mined from the ground by the presence of witches’
brooms. Trees with an infestation index of 0 to 3 were
classified as lightly infected, whereas trees with an
index of 4 to 6 were classified as moderately to heavily
infected. In order to take into account the competition
of other trees, the dbh and distance of the nearest tree
in each cardinal direction were measured.
Following felling of the trees, tree height was record-
ed and stems were sectioned at 0 m, 0.5 m, 1.3 m, and
then 1-m intervals until stem diameter was less than
1 cm. Sections at points of the stem where branches
emerged were avoided, and the adjusted height was
recorded. For each cross-section, diameter inside-bark
and outside-bark were measured along two diameters
perpendicular to each other. At the laboratory, age of
each cross-section was measured, and the pointer-year
method of cross-dating was used to validate ages (Yam-
aguchi 1991). Following dating, stem analysis was per-
formed on each tree to determine annual increments.
Ring width measurements were done using the Win-
DENDRO™ y. 2002a program (Régent Instruments
Inc. 2002*), and annual increments were calculated us-
ing XLSTEM™ 1.3a (Régent Instruments Inc. 1999*).
Each cross-section was scanned with a high-resolution
scanner and saved as a digital image. An image reso-
lution of 800 dpi was used, except for cross-sections
exhibiting high levels of suppression, where a resolu-
tion of 1600 dpi was used. For one tree, suppression was
too great for ring detection by the WinDENDRO™
Sast atchewan
@
Winnipeg
100° 96° g2°
Epp AND TARDIF: EFFECS OF LODGEPOLE PINE DWARF MISTLETOE
597]
0 Low-infection
O High-infection
50 Meters
FicurE 1: Location of the study area and distribution of the sampled trees. The lower right panel illustrates the relative posi-
tion of the sampled trees and their infection level in the jack pine stand. Empty circles correspond to heavily infected
trees, and empty squares correspond to lightly or non-infected trees.
program, so measurements were performed manually
at a magnification of 50x using a Velmex measuring
stage to a precision of 0.001 mm. Ring widths were
measured, starting at the pith, along four radial paths
in the north, east, south and west directions.
Data obtained were examined for differences between
the two infection groups with regards to age, competi-
tion index, dbh, basal area, height, volume and stem
form. The competition index was modified from Hegyi’s
distance weighted size ratio index (Avery and Burk-
hart 2002):
i
Sy DIST,
jal
where C/I; is the competition index for the subject
tree, D; is the dbh of the jth of four competitor trees
(N, E, S, and W directions), D, is the dbh of the subject
tree, and DIST, is the distance between the subject
tree and the jth competitor tree. Basal area at dbh was
calculated for each tree by using the formula for the
area of a circle. Tree volume without bark was calcu-
lated by applying Smalian’s formula for volume (Avery
and Burkhart 2002) to each segment. The volume of
each segment was then added to obtain tree volume.
Stem form expressions were determined using the
Girard form class (Avery and Burkhart 2002), with the
quadratic mean diameter taken at the section nearest
5 metres. Because each group had a relatively low
sample size (N=10), the non-parametric Mann-Whitney
U-test was performed on each variable to determine
significant differences between samples from each
infection group (a = 0.05). It should be noted that the
Mann-Whitney U-test and the Wilcoxon two-samples
test yield the same statistic and give the same results
(Sokal and Rohlf 1997). To limit the effect of environ-
mental variability, lightly or non-infected and heavily-
infected trees were also carefully matched in pairs based
on the distance separating them (Figure 1). Nine pairs
were formed with a mean distance of 9.49 m (standard
deviation = 4.83 m) between lightly or non-infected
and heavily-infected trees. A Wilcoxon signed-rank
test (Sokal and Rohlf 1997) was used to test for sig-
nificant differences between infection groups. Paired-
sample tests are more powerful than independent-
sample tests.
The cumulative dbh, basal area, height and volume
average growth curves produced for each tree were
compared between infection groups. First, predicted
growth curves were modelled for each growth variable
and tree using non-linear regression. Best fit to actual
cumulative growth curves for each variable and tree
were obtained using a three-parameter logistic model
of the form:
a
SD
1+ ext
]
where y is the value of the subject growth variable, x
is the year of growth, a is the asymptotic level of
598
growth, b is the growth constant, and xp is the inflection
point. Because each of these three parameters defines
the shape of the growth curves, significant differences
between parameters for the two infection groups were
determined using the Mann-Whitney U-test (a = 0.05).
This was repeated for each growth variable. Second,
the best three-parameter logistic model was determined
for each variable and infection group using the 10 trees
as replicates. The resulting predicted growth curves
were plotted to age 60. Because trees were not all of the
same age and the number of observations decreased with
time, only data covering the first 45 years of growth
were used in all the regression analyses.
Results
The two infection groups showed no significant dif-
ference in age, competition index, dbh, and basal area
(Table 1). There was, however, a significant difference
in height and form class (Table 1). Specifically, trees
in the high infection group were 20.2% shorter and
THE CANADIAN FIELD-NATURALIST
Vol. 118
had more stem taper. Both independent- and paired-
sample tests yielded divergent results regarding total
volume, and when partially controlling for environmen-
tal variability no significant difference in total volume
was observed as indicated by the Wilcoxon signed-rank
test.
The analysis of the coefficients from the logistic
regressions derived from each tree in each infection
group revealed that the high infection group reached a
significantly lower maximum basal area, height, and
volume, as predicted by the asymptotic values of the
regression model (Table 2). Maximum dbh did not dif-
fer significantly between groups. The logistic regres-
sion model, projected to age 60, predicts a 21.1% lower
basal area (Figure 2B), a 23.4% lower height (Figure
3A), and a 42.1% lower volume (Figure 3B) for the
high infection group.
Results showed that there was a significantly higher
growth rate for dbh and basal area in the high infection
group (Table 2). This was also observed for volume but
TABLE |: General characteristics of heavily infected and non-infected or lightly infected trees (n = 10 for each group) at time
of sampling (Max = Maximum value, Min = Minimum value, SEM = Standard Error of the Mean). The first column of
probabilities (P!) is based on the Mann-Whitney U-test (n=10 for each group). The second column of probabilities (P?) is
based on the Wilcoxon signed-rank test (n=9 pairs).
Low infection High infection
Max Min Mean SEM Max Min Mean SEM P! Pp?
Infestation index 2.0 0.0 12 0.29 6.0 4.0 2 0.20 0.000 0.007
Tree age 48.0 42.0 46.3 0.62 82.0 44.0 50.0 3.59 O28 022:
Competition index 3.34 0.77 1.85 0.30 1.89 0.66 1.29 0.15 0257) .O!515:
Diameter at breast height (cm) 19205) W310 od 0.38 L960 SES ON eliS 45 0.83 0.544 0.515
Basal area (m7?) 0:022> O!012. ~0:017;- 0:00 0.024 0.007 0.016 0.00 0.544 0.594
Height (m) 14.10 10.90 12.65 0.39 L330 830 ea lORO 4s 3054: 0.004 0.008
Volume (m?) 0.16 0.09 0.12 0.01 0.17 0.04 0.08 0.01 0.019 0.110
Form class 0.83 0.64 0.73 0.02 0:76" 10335 0.56 0.04 0.004 0.008
TABLE 2. Values of the three parameters of the predicted logistic growth curves used to model diameter at breast height, basal
area, height, and volume for heavily infected and non-infected or lightly infected Jack Pine trees (n = 10 for each group).
The three parameters are the theoretic maximum (a), growth (b), and the inflection point (x9) (Max = Maximum value, Min
= Minimum value, SEM = Standard Error of the Mean). The first column of probabilities (P') is based on the Mann-Whit-
ney U-test (n=10 for each group). The second column of probabilities (P?) is based on the Wilcoxon signed-rank test (n=9
pairs).
Low infection group High infection group
Max Min Mean SEM Max Min Mean SEM P! pz
Diameter at breast
height (cm) a 22: OS na WLANs lif2,9 0.85 QO0:97 18287 2 18.97 PAIL 0.059 0.260
b — 84) '-3230) 1 <2:46%) 10M3 -2.46 -4.29 -3.26 0.19 0.005 0.015
Xo 36:220 23133) 28:46 1.50 Qe oie MOD3ie 524 1.19 0.023 0.028
Basal area (m7) a 0.071 0.019 0.038 0.0061 0.032 0.007 0.016 0.0026 0.002 0.038
b -2.32 -3.51 =O Ams ORS -3.07 -5.27 -3.84 0.20 0.001 0.008
Xo OB Man) S464) 5538/8 Soe 39.18 24.84 31.59 1.72 0.001 0.011
Height (m) a 24.37 14.99 19.59 1.01 20.63 9.28 13.90 1.2] 0.008 0.015
b -1.71 -2.64 -1.98 0.09 -1.44 -2.65 -2.07 0.12 0.326 0.374
Xo AD OI 24938 = 32°66 1.74 49.34 20.56 27.58 DATA 0.034 0.038
Volume (m?) a 2237 2 OM2OF 1Or604s O97, 0.214 0.042 0.097 0.021 0.001 0.015
b -2.98 -4.36 -3.60 0.13 -3.12 -6.07 -4.09 0.25 0.082 0.028
Xo 111.79 40.48 60.48 6.51 48.74 30.68 36.59 1.97 0.001 0.011
2004
P<0.0001
16 y = 16.6392/[1+(x/27.2775) 242"
adj. ° = 0.96
aaa, P<0.0001 eso
5 e
=
a4 +
: . y = 13,8979/{1+(x/23.3196)?°%)
iw adj. r = 0.88
3 P<0.0001
5 6
5 4
(S)
2
0
0.020 y = 0.0274/[1+(x/45.0484)22743)
B) adj. r =
j. F = 0.92
P <0.0001 Wa
~ 0.015 Vy ,
nN | i os
© Pe
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© 0.010 gf
g q
© #
jaa) ¥ y = 0.0170/[1+(x/33.1868) 74767]
0.005 # SAE ey
0 10 20 30 40 50 60
Tree age
FIGURE 2: Average cumulative dbh growth (A) and average
cumulative basal area growth (B) for each of the two infec-
tion groups. Dashed lines represent predicted growth up to
year 60 for the infection groups, based on the 3-parameter
logistic regression models depicted. Vertical bars represent
standard errors of the mean. The black dashed line and
empty circles indicates the low infection group, and the
dark grey dashed line and empty triangles indicates the
high infection group.
only after the Wilcoxon signed-rank test. It should be
noted that in a logistic regression, there is an inverse
relationship between the growth constant and the actual
growth rate. The significantly lower growth constant
observed in the high infection group indicates a faster
rate of growth. No significant difference in the growth
rate for height was observed. However, all four cumu-
lative growth variables of the high infection group
reached their inflection point significantly sooner than
the low infection group (Table 2), suggesting that the
high infection group reached its maximum growth
rate sooner. Dbh (Figure 2A) and basal area (Figure
2B) of the two infection groups were not predicted to
diverge until after 45 years of age, while height growth
curves began to diverge at about 20 years of age (Fig-
ure 3A), and volume growth curves began to diverge
at 35 to 40 years of age (Figure 3B).
Results indicate a higher level of variability in the
basal area and volume of the high-infection group when
compared to the low-infection group, as indicated by
the lower value of the adjusted 1 for each logistic regres-
sion model. This may indicate variation in environmen-
tal conditions at early stages of growth for the trees, or
Epp AND TARDIF: EFFECS OF LODGEPOLE PINE DWARF MISTLETOE
599
16 y = 18.4039/(1+(x/30.4334) 1%")
14 A) a0 f 087 iS ,
12
E en:
‘er Be antl
5 : agp
a 6 fi Fy = 13.2629/(1+(x/25.9869)29"%
oH r=0.92
il Bsc
4 os
24 a
0 es geet
0.16
] B) y = 0.2048/[1+(x/46.9484)? 7]
0.14 | adh O82 s
0.12 i
“E 0.10 x
2 0.08 4
§ ee
S 0.06
0.04 ft
0.02 sf Pi y = 0.101 1/[1+(x/38.4295)?7""4
0.00 soon? PE OOOR |
0 10 20 30 40 me 2
Tree age
FIGURE 3: Average cumulative height growth (A) and average
cumulative volume growth (B) for each of the two infection
groups. Dashed lines represent predicted growth up to year
60 for the infection groups, based on the 3-parameter logis-
tic regression models depicted. Vertical bars represent stan-
dard errors of the mean. The black dashed line and empty
circles indicates the low infection group, and the dark grey
dashed line and empty triangles indicates the high infec-
tion group.
variation in genetic resistance to mistletoe infection.
Examination of the stem profiles also revealed that some
trees in the high-infection group exhibited little or no
evidence of growth reduction despite a high infection
index (not presented). These trees could have been
recently infected by Dwarf Mistletoe.
Discussion
No significant differences in tree age or competition
levels between the two infections groups were observed
indicating that Dwarf Misteltoe was was the key factor
affecting Jack Pine growth. The lack of a significant
difference in dbh between the heavily infected and
lightly infected Jack Pine trees at the time of sampling
likely reflects the young age of the subject trees and
the duration of the infection period. Tinnin et al. (1999)
found that there was a significant reduction in the
diameter growth of Douglas-fir (Pseudotsuga menziesii
(Mirb.) Franco var. menziesii) heavily infected by A.
douglasii (infection index = 5 and 6) when compared
to non-infected trees (infection index = 0) for trees hav-
ing mean ages between 78 and 84 years. In Lodgepole
Pine, diameter growth was not significantly affected
600
at stump height, but significant decreases in diameter
growth were apparent at heights further up the stem
because of greater stem taper (Baranyay and Safranyik
1970). Our study also showed that stem taper was sig-
nificantly more pronounced in the high infection group.
At the time of sampling, basal area in the high infec-
tion group was not significantly different than that of
the low infection group. Comparison of the logistic
regression coefficients provided similar results to dbh,
except that the high infection group was predicted to
reach a significantly lower basal area compared to the
low infection group as trees continue to grow after
age 45. Assuming that basal area increment after the
age of 45 years will continue to follow that predicted by
the logistic regression model, the projected maximum
basal area of the high infection group was approxi-
mately 57.9% lower than that of the low infection
group. Pierce (1960) also found a 68.5% reduction in
basal area for heavily infected Douglas-fir, and a
41.0% reduction in moderately infected Douglas-fir.
Of the significantly affected growth variables, height
increment showed a reduction first, i.e., between the
ages of 20 and 25 years. Pierce (1960) also found that
differences in height were statistically significant be-
tween all infection classes, in contrast to diameter. This
corresponds with the highly significant 20.2% lower
tree height in heavily infected trees in this study. The
greater sensitivity of this variable is likely due to the
initial response of trees to Dwarf Mistletoe infections.
Dwarf Mistletoe infected trees accumulate a high level
of biomass in their brooms, which detracts the allo-
cation of resources from biomass production elsewhere
in the tree (Tinnin and Knutson 1980). In contrast to
the other growth variables, height of the high-infection
group had similar variability to the low-infection group,
as indicated by similar adjusted r values in the logistic
regression curves. This suggests that height growth is
less sensitive to temporal changes in factors such as
stand density and competition (Avery and Burkhart
2002). Height growth diverged between the two infec-
tion groups at a much earlier age than volume, diame-
ter, or basal area, further suggesting that height growth
begins to show significant decreases shortly after the
development of brooms and loss of apical dominance
(Tinnin and Knutson 1980).
At the time of sampling, there was a 33.3% lower
average total volume in the high infection group, which
was mostly due to a significant reduction in tree height.
However, despite early reduction in height growth,
volume growth of the heavily infected trees was not
significantly affected until 30 to 40 years of age. Our
values very closely correspond with those reported by
Baranyay and Safranyik (1970), where a group of
infected Lodgepole Pine trees with an average age of
37 showed a 35.5% reduction in volume. From the
logistic growth model, it was found that the predicted
maximum average volume of the high infection group
was 83.9% lower than the low infection group. This
THE CANADIAN FIELD-NATURALIST
Vol. 118
projected value exceeded the estimated volume reduc-
tion in infected stands made by Baker et al. (1992),
which was between 53.4% and 70.3% depending on
the level of potential crown closure. However, it should
be noted that our findings reflected the volume loss in
individual trees, and not the volume loss as averaged
through an entire stand.
In conclusion, this study confirmed the significance
of the impact of Dwarf Mistletoe on the growth of com-
mercial Jack Pine forests, and the potential economic
loss due to severe infection. Despite early reduction in
height growth, volume growth of the heavily infected
trees was not significantly affected until 30 to 40 years
of age. Further study on the effects of Dwarf Mistletoe
over a wider range of age classes and site indexes would
be beneficial in modelling the impact of the parasite.
Acknowledgements
This project was part of an undergraduate honours
thesis course at the University of Winnipeg, conducted
by the first author. We thank the following people for
their contributions: F. Conciatori, G. Sayer, R. Moodie,
R. Westwood, D. Ko Heinrichs, the University of Win-
nipeg Department of Biology, and the Centre for For-
est Interdisciplinary Research. Special thanks go to K.
Knowles from Manitoba Conservation and R. Staniforth
for their comments on a previous draft of this paper.
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Baker, F. A., M. Slivitsky, and K. Knowles. 1992. Impact of
dwarf mistletoe on jack pine forests in Manitoba. Plant
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Baranyay, J. A., and L. Safranyik. 1970. Effect of dwarf
mistletoe on growth and mortality of lodgepole pine in
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eries and Forestry. Publication Number 1285.
Brandt, J. P., R. D. Brett, K. R. Knowles, and A. Sproule.
1998. Distribution of severe dwarf mistletoe damage in
west-central Canada. Natural Resources Canada, Canadian
Forestry Service, Northern Forestry Centre, Edmonton,
Alberta. Special Report 13.
Burton, V. B., D. R. Zak, S. R. Denton, and S. H. Spurr.
1998. Forest ecology, Fourth edition. John Wiley & Sons
Inc. New York. 774 pages.
Franc, G. D., and FE. A. Baker. 2000. Dwarf mistletoes affect-
ing pines and firs of Wyoming. University of Wyoming and
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Hawksworth, F. G. 1977. The 6-class dwarf mistletoe rating
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Hawksworth, F. G., and D. Wiens. 1996. Dwarf mistletoes:
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Hull, R. J., and O. A. Leonard. 1964a. Physiological aspects
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Hull, R. J., and O. A. Leonard. 1964b. Physiological aspects
of parasitism in mistletoes (Arceuthobium and Phoraden-
dron). Ul. The photosynthetic capacity of mistletoe. Plant
Physiology 39: 1008-1017.
Pierce, W. R. 1960. Dwarf mistletoe and its effect upon the
larch and Douglas-fir of western Montana. Montana State
University. School of Forestry. Missoula, Montana. Bul-
letin Number 10. 37 pages.
Piirto, D. D., D. L. Crews, and H. E. Troxell. 1974. The
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Tinnin, R. O., C. G. Parks, and D. M. Knutson. 1999.
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Received 10 February 2004
Accepted 24 December 2004
Notes
Excavation of an Arctic Fox, Alopex lagopus, den by a Polar Bear,
Ursus maritimus
Evan S. RICHARDSON! and RYAN K. BROOK?
‘Canadian Wildlife Service, 5320-122 St., Edmonton, Alberta T6H 3S5 Canada
Faculty of Environment, University of Manitoba, Winnipeg, Manitoba R3T 2N2 Canada
Richardson, Evan S., and Ryan K. Brook. 2004. Excavation of an Arctic Fox, Alopex lagopus, den by a Polar Bear, Ursus
maritimus. Canadian Field-Naturalist 118(4): 602-603.
We observed a Polar Bear (Ursus maritimus) excavating an Arctic Fox (Alopex lagopus) den on 24 June 1998, 3 km inland from
the Hudson Bay coast (58°40'N, 93°12'W), near Cape
Churchill in Wapusk National Park, Manitoba. To our
knowledge this is the first observed excavation of an Arctic
Fox den by a Polar Bear.
Key Words: Arctic Fox, Alopex lagopus, Polar Bear, Ursus
maritimus, den, behaviour, Hudson Bay, Wapusk
National Park, Manitoba.
The western Hudson Bay Polar Bear (Ursus mar-
itimus) population remains on shore from approximate-
ly mid-July through early November due to complete
annual melting of the sea ice (Stirling et al. 1977).
During this period, bears mainly remain relatively
inactive (Knudsen 1978; Latour 1981; Lunn and Stir-
ling 1985) and subsist primarily on stored fat reserves
(Nelson et al. 1983; Derocher et al. 1990; Ramsay et
al. 1991). However, during the summer months, polar
bears are opportunistic and occasionally feed on a
variety of terrestrial food sources including grasses,
sedges and berries (Knudsen 1978; Lunn and Stirling
1985, Derocher et al. 1993), Thick-billed Murres (Uria
lomvia) (Donaldson et al. 1995), Canada Geese (Bran-
ta canadensis) (Russell 1975) and their eggs (Smith
and Hill 1996), Snow Goose eggs (Anser caerulescens)
(Abraham et al. 1977), Willow Ptarmigan (Lagopus
lagopus) (Miller and Woolridge 1983), seabirds (Stemp-
niewicz 1993), microtine rodents (Russell 1975; Miller
and Woolridge 1983), and Caribou (Rangifer tarandus)
remains (Brook and Richardson 2002).
We observed an adult male Polar Bear excavate an
Arctic Fox den near Nestor | field camp (58°40'N,
93°12'W), near Cape Churchill in Wapusk National
Park, Manitoba on 24 June 1998 at 11:00 CST. The
bear was initially sighted on a large beach ridge inves-
tigating one of the camp buildings and then moved to
an Arctic Fox den located approximately 350 m south-
east of camp. The bear moved around the site, inves-
tigated several of the den entrances and then stopped
at one entrance and began to excavate the den. The
bear stopped digging every 10 —15 seconds to put its
head into the enlarged entrance, continued this behav-
iour for approximately 3 minutes, then stopped dig-
ging and spent approximately 2 minutes investigating
several other den entrances, but did not dig them out.
The bear then moved away from the den and down
the eastern side of the beach ridge, where it could no
longer be observed. The bear was not observed eating
anything, although while its head was in the entrance,
it could not be observed. Several fox pups were occu-
pying the den at the time and we assumed the pups
were in the den during the observation although the
location of the vixen at the time was unknown. We
visited the following day and found a large pit dug by
the bear. The excavation was 55 cm at its deepest and
was approximately 70 cm wide and 80 cm in length.
Arctic Fox pups could still be heard inside the den
confirming that the den had not been abandoned and
there was no evidence any fox pups were killed. The
top of the den was littered with Canada and Snow
Goose remains, consisting mostly of feet (98) and other
waterfowl remains such as bones and feathers. Cached
prey items inside the den were visible from several den
entrances and consisted primarily of goose remains.
Food remains found at fox dens in the region included
both adult and juvenile geese, ducks, Caribou remains
and in one instance, a Muskrat (Ondatra zibethicus)
(Richardson and Brook, personal observations, 1999).
Polar Bears are known to excavate subnivean lairs
in search of young Ringed Seal (Phoca hispida) pups
(Stirling and Archibald 1977). They also excavate earth
and snow dens for reproduction, as well as open pits
for resting (Clark 1996; Clark et al. 1997). Although
adult male bears are known to excavate open pits on
coastal beach ridges (Clark 1996), we suggest that the
bear was most probably trying to gain access to a poten-
tial food source. The bear may have been attracted to
the fox den for several reasons. In areas where prey is
abundant, Arctic Foxes cache large quantities of food
at den sites for later consumption (Sklepkovych and
602
2004
Montevecchi 1996; Garrott et al. 1984). As a result,
other predators may be attracted to den sites by their
smell (Prestrud 1992). At active den sites, character-
| istic barks of arctic fox pups can be heard from with-
_ in the den when it is disturbed (Eberhardt et al. 1983;
Richardson and Brook, personal observations, 1999).
Bears are adept at locating food sources by smell (Lunn
and Stirling 1985) and it seems unlikely that barking
attracted the bear to the site, but the sound may have
stimulated further investigation. Prey remains at den
_ sites may provide a direct energy source for bears, how-
| ever the energetic cost of excavating a den would not
likely be repaid in the capture of a small Arctic Fox pup.
Although, Macpherson (1969) notes that Arctic Fox
dens may be occasionally excavated by Grizzly Bears
| (Ursus arctos) and Wolves (Canis lupus), we are not
aware of any other published reports of Polar Bears
| excavating Arctic Fox dens.
| Acknowledgments
These observations were made while conducting
research supported by Wapusk National Park, the
Manitoba Department of Conservation, the Churchill
_ Northern Studies Centre, the Northern Studies Training
_ Program of the Department of Indian and Northern
Affairs Canada, the Canadian Department of Fisheries
and Oceans, the Western Canada Service Centre of
_ Parks Canada, Wat’chee Lodge, the Canadian Wildlife
Federation, and the Manitoba Chapter of the Wildlife
Society. We would like to thank I. Stirling and N. J.
Lunn for their valuable comments on the manuscript.
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predators of snow goose eggs. Canadian Field-Naturalist
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Derocher, A. E., D. Andriashek, and I. Stirling. 1993. Ter-
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in western Hudson Bay. Arctic 46: 251-254.
Donaldson, G. M., G. Chapdelaine, and J. D. Andrews.
1995S. Predation of thick-billed murres, Uria lomvia, at two
NOTES
603
breeding colonies by polar bears, Ursus maritimus, and
walruses, Odobenus rosmarus. Canadian Field-Naturalist
109: 112-114.
Eberhardt, L. E., R. A. Garrott, and W. C. Hanson. 1983.
Den use by arctic foxes in northern Alaska. Journal of
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Garrott, R. A., L. E. Ebehardt, and W. C. Hanson. 1984.
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Knudsen, B. 1978. Time budgets of polar bears, Ursus mar-
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2297.
Macpherson, A. H. 1969. The dynamics of Canadian arctic
fox populations. Canadian Wildlife Service Report Series
8. 52 pages.
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Nelson, R. A., G. E. Folk Jr., E. W. Pfeiffer, J. J. Craig-
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biochemistry, and hibernation in black, grizzly, and polar
bears. International Conference on Bear Research and
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Prestrud, P. 1992. Denning and home-range characteristics
of breeding arctic foxes in Svalbard. Canadian Journal of
Zoology 70: 1276-1283.
Ramsay, M. A., R. A. Nelson, and I. Stirling. 1991. Season-
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69: 298-302.
Russell, R. H. 1975. The food habits of polar bears of James
Bay and southwest Hudson Bay in summer and autumn.
Arctic 28: 117-129.
Sklepkovych, B. O., and W. A. Montevecchi. 1996. Food
availability and food hoarding behaviour by red and arc-
tic foxes. Arctic 49: 228-234.
Smith, A. E., and M. R. J. Hill. 1996. Polar bear, Ursus mar-
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Stempniewicz, L. 1993. The Polar bear, Ursus maritimus,
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Stirling, I., and W. R. Archibald. 1977. Aspects of predation
of seals by polar bears. Journal of the Fisheries Research
Board of Canada 34: 1126-1129.
Stirling, I., C. Jonkel, P. Smith, R. Robertson, and D.
Cross. 1977. The ecology of the polar bear (Ursus mar-
itimus) along the western coast of Hudson Bay. Canadian
Wildlife Service Occasional Paper 33: 64 pages.
Received 24 June 2003
Accepted 2 November 2004
604
THE CANADIAN FIELD-NATURALIST
Vol. 118
Two Great Black-backed Gulls, Larus marinus, Kill Male Longtailed
Duck, Clangula hyemalis
MARTHA DowsLey! and ANDREW CIRTWILL?
‘Department of Geography, McGill University, 805 Sherbrooke Street West, Montreal, Quebec H3A 2K6 Canada
°515 Roosevelt Drive, Kingston, Ontario K7M 5Y2 Canada
Dowsley, Martha, and Andrew Cirtwill. 2004. Two Great Black-backed Gulls, Larus marinus, Kill Male Longtailed Duck,
Clangula hyemalis. Canadian Field-Naturalist 118(4): 604-605.
At Presqu’ile Point, Presqu’ile Provincial Park, Ontario on 23 March 2003, while interpreting the waterfowl migration for
park visitors, we witnessed two adult Great Black-backed Gulls attack and kill a male Long-tailed Duck.
Key Words: Great Black-backed Gull, Larus marinus, Long-tailed Duck, Clangula hyemalis, predation
Great Black-backed Gulls, Larus marinus, are known
to be scavengers and to take eggs, nestlings, and fledg-
lings of other birds. However, their efficacy as preda-
tors is less well documented. On 23 March 2003 we
witnessed two adult Great Black-backed Gulls attack
and kill a Long-tailed Duck, Clangula hyemalis.
We were using a spotting scope (power 45x) to
observe diving ducks located 200 to 250 m from shore
off Presqu’ile Point, Ontario (44°00'N, 77°41'W) as they
fed and rested at the front edge of ice in Presqu’ile
Bay. The ducks routinely lifted off when a predatory
bird passed overhead. After one such take-off, we ob-
served a pair of adult Great Black-backed Gulls flying
above the ducks. One male Long-tailed Duck failed
to lift off and the gulls flew down and began to harass it.
We did not see the initial separation of the duck from
the flock, so we were unable to observe whether it was
healthy and merely caught under water when the rest of
the flock flew, or whether it was already injured when
attacked.
The attack proceeded in what appeared to be a coor-
dinated effort by the gulls. One Great Black-backed
Gull flew in circles overhead when the duck dived and
swam under water. When the duck surfaced, the gull
alighted on the water and tried to bite him. The sec-
ond gull then took off from the water and flew over-
head, watching the duck as he dived again to avoid
the attack of the first gull. When the duck resurfaced,
the second gull attacked him while the first gull again
took off and watched as the duck tried to make another
escape under water.
The Great Black-backed Gulls continued to take
turns flying and attacking the duck for 20-25 minutes.
At the end of this time, one gull succeeded in grabbing
the wing of the Long-tailed Duck and both gulls then
pecked at the body of the duck. Less than 5 minutes
later the duck was dead, and its limp body could be seen
floating on the water. The adult Great Black-backed
Gulls were then joined by an immature Great Black-
backed Gull and all three gulls began to eat the dead
duck. We could not continue observations as the wind
and currents had pushed the duck’s carcass out into Lake
Ontario, beyond the useful range of our spotting scope.
Great Black-backed Gulls have a varied diet, but their
main food sources are fish and seabirds (both often
consumed as carrion) (Buckley 1990). Their predation
of birds is focused on the eggs, nestlings, newly fledged
young and sick or injured individuals (Beaman 1978;
Mawhinney and Diamond 1999). Healthy adult birds
are rarely killed, with the notable exception of preda-
tion in some seabird colonies, such as those of the
Atlantic Puffin (Fratercula arctica) in Northern Europe
(Beaman 1978), and Newfoundland (Nettleship 1972).
Great Black-backed Gulls are considered to be pred-
ators of waterfowl (Good 1998); however, observations
of Great Black-backed Gulls attacking and killing adult
ducks are quite rare. One notable record reported by
Cleghorn (1942) was of an adult Great Black-backed
Gull killing a female Goldeneye (Bucephala clangula)
and an immature Great Black-backed Gull killing anoth-
er unidentified duck the same day.
Cobb (1957) observed a single adult Great Black-
backed Gull kill an injured Ruddy Duck, Oxyura
Jamaicensis, in Rhode Island. In that case the method
of attack was similar to what we witnessed at Presqu ile.
The gull hovered above the duck as it dived and then
attempted to grab it when it resurfaced (Cobb 1957).
Our report corroborates the evidence that Great Black-
backed Gulls will fly above diving ducks, presumably
to watch them under water, and attack them when they
resurface.
Addy (1945) witnessed a group of Great Black-
backed Gulls attack and kill an adult American Black
Duck, Anas rubripes. The gulls chased and swooped
at groups of American Black Ducks until one adult
gull injured a duck. The gulls then worried the duck by
lifting it from the water by its neck and by grasping
its back. After about half an hour the duck died, and
was consumed, mainly by the gull which had first
attacked it (Addy 1945). This observation does not
appear to have been a coordinated attack on the duck
as in the case we witnessed, because one gull of a
group carried out most of the attack and was the pri-
mary consumer of the carcass.
In our observation, the two Great Black-backed Gulls
showed a level of coordination in their attack that is
On
2004
unrecorded in the literature. The method they used of
taking turns flying overhead and attacking the duck
seems to be an efficient means to harass their prey to
| the point of exhaustion and death.
Literature Cited
Addy, C. E. 1945. Great Black-backed Gull kills adult Black
Duck. Auk 62: 142-143.
Beaman, M. A. S. 1978. The feeding and population ecology
of the Great Black-backed Gull in northern Scotland. Ibis
120: 126-127.
Buckley, N. J. 1990. Diet and feeding ecology of Great
Black-backed Gulls (Larus marinus) at a southern Irish
breeding colony. Journal of Zoology: Proceedings of the
Zoological Society of London 222: 363-373.
GLYNNIS A. Hoop and TIM NEUFELD
NOTES
605
Cleghorn, J. D. 1942. Great Black-backed Gull killing Amer-
ican Goldeneye. Auk 59: 584-585.
Cobb, S. 1957. Great Black-backed Gull (Larus marinus).
Auk 74: 498.
Good, T. 1998. Great Black-backed Gull. The birds of North
America (330). Edited by A. Poole and F. Gill in The
Birds of North America, Inc., Philadelphia Pennsylvania.
Mawhinney, K., and A. W. Diamond. 1999. Using radio-
transmitters to improve estimates of gull predation on Com-
mon Eider ducklings. Condor 101: 824-831.
Nettleship, D. N. 1972. Breeding success of the Common
Puffin (Fratercula arctica) on different habitats at Great
Island, Newfoundland. Ecological Monographs 42: 239-
268.
Received 7 May 2004
Accepted 4 October 2004
| First Record of Mountain Lions, Puma concolor, in Elk Island National
| Park, Alberta
| Elk Island National Park, R.R. #1, Site 4, Fort Saskatchewan, Alberta T8L 2N7 Canada, e-mail: [Hood] glynnis.hood@pc.ge.ca
| Hood, Glynnis A., and Tim Neufeld. 2004. First record of Mountain Lions, Puma concolor, in Elk Island National Park,
Alberta. Canadian Field Naturalist 118(4): 605-607.
Several sightings of Mountain Lions (Puma concolor) and wildlife mortalities consistent with predation by Mountain Lion have
occurred in and adjacent to Elk Island National Park from February 2003 to present. These are the first recorded Mountain
| Lions (locally called Cougar) sightings since the area encompassing the park was protected in 1906.
Key Words: Mountain Lion, Cougar, Puma, Panther, Catamount, Puma concolor, Elk Island National Park, Alberta, range,
first record.
Along with its current range, Mountain Lion (Puma
concolor) historically occupied central and eastern
Canada (Banfield 1974). In present day Aiberta how-
ever, Mountain Lion (locally called Cougar) popula-
tions are mainly concentrated in the Rocky Mountains
and the foothills (Soper 1964; Banfield 1974; Smith
1993; Pattie and Fisher 1999). By 1961, Bird described
many large predators, including the Mountain Lion, as
being extirpated from the aspen parkland of Canada’s
prairie provinces. Soper (1964) referenced individual
_ reports of Mountain Lions north of Edmonton, Alberta
_ at Boiler and Grand Rapids on the Athabasca River
and in the Peace River Region in northwestern Alberta.
_ He also noted occasional sightings in southern Alberta
along the Milk, Bow, and South Saskatchewan River
systems, as well as in the Cypress Hills. Smith (1993)
added additional sightings near the towns of White-
court and Athabasca, Alberta.
Sightings of Mountain Lions are increasing in areas
where they were previously unreported. Occasional
sightings have been documented to the north in Wood
Buffalo National Park (Gau et al. 2001), and to the
south and west of Elk Island National Park (EINP) near
Cooking Lake, Pigeon Lake, and Sherwood Park (Smith
1979). However, until 2003, there had never been a
documented Mountain Lion sighting in EINP (Soper
1940*; Soper 1951; Burns and Cool 1984*; Parks
Canada Warden Service unpublished notes). Elk Island
lies between longitude W112°57'00" and W112°46'45"
and latitude N53°42'57" and N53°30'37" (Figure 1)
and covers an area of 196 km*. The park is located in
the Aspen Parkland Natural Subregion (Achuff 1994)
in the Beaver Hills of east-central Alberta and is home
to several species of large ungulates.
Given the known distances that Mountain Lions
would have to travel to access the park, Burns and
Cool (1984) predicted “occurrences of cougar in Elk
Island National Park [EINP] in future remain a slim
possibility”. The closest source populations to EINP
are in the Rocky Mountains foothills and the Swan Hills
region of north-central Alberta (Pattie and Fisher 1999).
These populations are approximately 200 km away
from EINP, which is well within the 500 km dispersal
distance observed for Mountain Lions (Logan and
Sweanor 1999).
On 8 February 2003 at 11:00 h one of us observed
an adult Mountain Lion approximately 10 km south
of the boundary of EINP at Islet Lake in the southern
reaches of the Cooking Lake — Blackfoot Grazing,
Wildlife and Provincial Recreation Area (Figure 2).
606
,EBERTA
Elk Island
National Park
Edmonton @
, =» Calgary == Mountain lion
N distribution
A in Alberta
6 i 10 = w Es
FIGURE |. Location of Elk Island National Park in east-central
Alberta. The shaded area indicates the distribution of
Mountain Lion in Alberta (based on Pattie and Fisher
1999).
In late March, a conservation officer found tracks of
one large Mountain Lion and a much smaller Moun-
tain Lion together near the northern boundary of the
Provincial Recreation Area — an area that bounds the
southern extent of EINP. On 26 July 2003 at 14:00 h
a group of Young Canada Works students working in
the park reported seeing an adult Mountain Lion just
south of Highway 16 in the southern half of EINP.
An adult Mountain Lion was also seen by park vis-
itors on two different occasions in the northcentral
section of the park on 29 July 2003. The first visitor
reported seeing a Mountain Lion at 07:30 h beside
the main road through the park and a second visitor
saw a Mountain Lion while on a nearby trail at 21:40 h.
In the latter case the visitor reported seeing the Moun-
tain Lion watching a herd of Bison (Bison bison)
approximately 5 km from the trailhead. Equestrians
saw two Mountain Lions together in the north central
part of the Provincial Recreation Area around the same
time.
Further sightings were reported in the fall of 2003
when a park visitor observed an adult Mountain Lion
while hiking on 17 September. Another park visitor
reported seeing a Mountain Lion cross the main park
road on 2 October. In mid-October, a hiker reported
seeing a Mountain Lion at the southern part of the
Provincial Recreation Area between Push Lake and
Islet Lake. On 20 November 2003 a park warden report-
THE CANADIAN FIELD-NATURALIST
Vol. 118
Elk Island N
nal.Park
‘{ »
atio
iN
(i
Sighting
Ungulate Mortality
CookingLake - Blackfoot Grazing, Wildlife
and Provincial Recreation Area
FiGure 2. Mountain Lion sightings and wildlife mortalities
consistent with predation by Mountain Lion in Elk
Island National Park and the Cooking Lake — Black-
foot Grazing, Wildlife and Provincial Recreation Area
since February 2003.
ed seeing a Mountain Lion crossing a secondary road
in the east-central part of EINP.
In 2004, a cyclist observed a Mountain Lion sitting
beside the main road in the northern part of the park
(13 July). The most recent confirmed sighting in the
park was on 24 October 2004 when a park resident
observed a Mountain Lion in the main part of the park
(Figure 2). On two occasions, acreage owners on lands
east and north of the park heard estrous calls of a Moun-
tain Lion (October 2003 and August 2004). The land-
owner who reported the August 2004 calls observed a
small Mountain Lion on his property a few days later.
In addition to sightings, four ungulate mortalities
with wounds consistent with Mountain Lion predation
(Ross et al. 1997) have been documented in the park
since the winter of 2002-2003 (Figure 2). Prey species
were: 2 American Elk (Cervus canadensis), 1 Moose
(Alces alces), and 1 White-tailed Deer (Odocoileus
virginianus). In all cases the carcasses had signs of
wounds and fatal injuries to the neck and, in some
cases, large puncture marks in the hide. Apart from
Coyotes (Canis latrans), EINP lacks any large resident
predators. In addition, the park has very high ungulate
densities (approximately 13 ungulates per km7; Parks
Canada unpublished data) and is home to American
Elk, Moose, Bison (Bison bison), White-tailed Deer,
and Mule Deer (Odocoileus hemionus). The park also
has a large Beaver (Castor canadensis) population and
many resident medium and small mammal species
| including porcupine (Erethizon dorsatum), Muskrat
| (Ondatra zibethicus) and Red Squirrel (Jamiasciurus
| hudsonicus). Hare (Lepus spp.) are at low densities in
the park (Super 1951).
The park provides adequate undeveloped habitat and
food resources to support an adult Mountain Lion
(Spalding and Lesowski 1971; Ross and Jalkotzy 1992;
Ross et al. 1997; Robinson et al. 2002). Currently, park
staff translocate Bison and American Elk away from
the park to reduce the impact of intense herbivory on
vegetation. The presence of large predators, such as
Mountain Lions, may help to reduce the ungulate den-
| sities in the park, and therefore moderate the amount of
| active management of ungulate populations by park
| staff.
The park is completely fenced and the abundance of
prey species might offer enough resources to support a
| future Mountain Lion population. Given that success-
| ful reproduction in Mountain Lions is related to the
| availability of food (Pierce et al. 2000), the likely pres-
'ence of a mated pair within EINP suggests such a
scenario 1s not unrealistic.
Acknowledgments
We thank Conservation Officer Ed Whitelock and
Park Warden Olaf Jensen for providing us with addi-
( tional information on Mountain Lion sightings. We
also thank three anonymous reviewers for their edito-
rial comments.
Documents Cited
| Burns, G. R., and N. L. Cool. 1984. A biophysical inventory
of the non-ungulate mammals of Elk Island National Park.
Report prepared for Parks Canada by the Canadian Wild-
life Service, Edmonton, Alberta, Canada. 195 pages.
Soper, J. D. 1940. Preliminary final report on Elk Island Na-
tional Park, Alberta, Canada. unpublished report. Depart-
ment of Mines and Resources Lands, Parks and Forest
Branch, National Parks Bureau. Edmonton, Alberta, Cana-
da. 46 pages.
Literature Cited
Achuff, P. L. 1994. Natural regions, subregions and natural
history themes of Alberta — a classification for protected
areas management, revised and updated December 1994.
NOTES
607
Alberta Environmental Protection, Edmonton, Alberta,
Canada. 72 pages.
Banfield, A. W. F. 1974. The mammals of Canada. Univer-
sity of Toronto Press, Toronto, Ontario, Canada. 438 pages.
Bird, R. D. 1961. Ecology of the aspen parkland of western
Canada in relation to land use. Canada Department of Agri-
culture, Ottawa, Ontario, Canada. 155 pages.
Gau, R. J., R. Mulders, T. Lamb, and L. Gunn. 2001.
Cougars (Puma concolor) in Northwest Territories and
Wood Buffalo National Park. Arctic 54: 185-187.
Logan, K. A., and L. Sweanor. 1999. Puma. Pages 347-77
in Ecology and management of large mammals in North
America. Edited by S. Demarais and P. R. Krausman
Prentice-Hall, Englewood Cliffs, New Jersey.
Pattie, D., and C. Fisher. 1999. Mammals of Alberta. Lone
Pine Publishing. Edmonton, Alberta, Canada. 240 pages.
Pierce, B. M., V. C. Bleich, and R. T. Bowyer. 2000. Social
organization of Mountain Lions: does a land-tenure sys-
tem regulate population size? Ecology 81: 1533-1543.
Robinson, H. S., R. B. Wielgus, and J. C. Gwilliam. 2002.
Cougar predation and population growth of sympatric mule
deer and white-tailed deer. Canadian Journal of Zoology
80: 556-568.
Ross, P. I., and M. G. Jalkotzy. 1992. Characteristics of a
hunted population of cougars in southwestern Alberta.
Journal of Wildlife Management 56: 417-426.
Ross, P. I., M. G. Jalkotzy, and B. M. Festa. 1997. Cougar
predation on bighorn sheep in southwestern Alberta dur-
ing winter. Canadian Journal of Zoology 75: 771-775.
Smith, H. C. 1979. Mammals of the Edmonton area. Provin-
cial Museum of Alberta Natural History Occasional Paper
Number 2. Queens Printer, Edmonton, Alberta, Canada.
34 pages.
Smith, H. C. 1993. Alberta mammals, an atlas and guide. The
Provincial Museum of Alberta. Edmonton, Alberta, Cana-
da. 238 pages.
Soper, J. D. 1951. The mammals of Elk Island National Park,
Alberta Canada. Wildlife Management Bulletin Series 1,
Number 3. Canadian Wildlife Service, Ottawa, Ontario,
Canada. 27 pages.
Soper, J. D. 1964. The mammals of Alberta. The Hamley
Press, Ltd. Edmonton, Alberta, Canada. 402 pages.
Spalding, D. J., and J. Lesowski. 1971. Winter food of the
cougar in south-central British Columbia. Journal of Wild-
life Management 35: 378-381.
Received 19 December 2003
Accepted 23 December 2004
608
THE CANADIAN FIELD-NATURALIST
Vol. 118
First Confirmed Occurrence of a Wolf, Canis lupus, South of the
St. Lawrence River in Over 100 Years
Mario VILLEMURE! and HELENE JOLICOEUR?
'Université de Sherbrooke, Département de Biologie, Sherbrooke, Québec JIK 2R1 Canada Current address: 11A, chemin
St-Francois, St-Mathieu-du-Parc, Québec GOX INO Canada
*Société de la faune et des parcs du Québec, Direction du développement de la faune, 675, boulevard René-Lévesque Est. .
11" floor, box 92, Québec, Québec GIR 5V7 Canada
Villemure, Mario, and Helene Jolicoeur. 2004. First confirmed occurrence of a Wolf, Canis lupus, south of the St. Lawrence
River in over 100 years. Canadian Field-Naturalist 118(4): 608-610.
A large canid was snared near Sainte-Marguerite-de-Lingwick, Québec, in January 2002. DNA analysis confirmed the ani-
mal to be a Wolf (Canis lupus). Wolves were extirpated from this region around 1850-1900 and this is the first confirmed
observation since then.
Key Words: Wolf, Canis lupus, range, dispersal, St. Lawrence River, Québec.
Historically, Wolves (Canis lupus) were distributed
across most of North America. They were extirpated
in the southern portion of their range by the turn of
the century (Nowak 1983). In Québec, Wolves disap-
peared from the south shore of the St. Lawrence River
around 1850-1900 (Peterson 1966). The extermination
of the Wolf and the development of agriculture in the
mid-1900 facilitated the extension of Coyote (Canis
latrans) range. Wolves are now mostly limited to the
northern and less populated regions of North America
(Wayne et al. 1992).
On 19 January 2002, a male Wolf was trapped
near the village of Sainte-Marguerite-de-Lingwick
(45°36'15"N, 71°17'15"W) in the Eastern Townships
of southern Québec. The Wolf weighed 29.1 kg, sim-
ilar to the weight of an adult from Papineau-Labelle
(Potvin 1986*) or a yearling from the Laurentides
region (Jolicoeur 1998%*). A tissue sample was collected
from the temporal muscle for genetic identification
of the species. DNA analyses were performed by the
Natural Resources DNA Profiling and Forensic Center
(Trent University, Peterborough, Ontario K9J 7B8 Can-
ada) following the method described in Wilson et al.
(2000). The Eastern Townships sample was profiled at
the mitochondrial DNA (mtDNA) control region and
8 microsatellite loci. The genetic profile was compared
to samples of canids representing the Eastern Wolf (C.
lupus lycaon) from Algonquin Provincial Park; West-
ern Coyotes (C. latrans) from Texas, North Carolina
and Ohio; and Wolves (C. lupus) from Pukaskwa Na-
tional Park, northeastern Ontario and the Laurentide
Wildlife Reserve region north of Québec City. The
above populations were used to compare the Eastern
Townships sample against C. lupus lycaon, C. latrans
and C. lupus to assess the species-of-origin or hybrid
genotype.
The sample had a mtDNA consistent with C. 1. lycaon/
C. latrans and the microsatellite genotype suggested
95.0% shared ancestry with Eastern Wolves from
Algonquin Provincial Park. The sample had a DNA
profile consistent with an Eastern Wolf. The Eastern
Wolf is generally described as being smaller than other
Gray Wolf subspecies (Nowak 1995, 2002). Although
it has been proposed as a distinct species (C. lycaon)
by Wilson et al. (2000), its status as a subspecies is
still generally accepted. Some authors suggest it may
result from hybridization between C. rufus and C.
Tupus (Nowak 2002). In Québec, the Eastern Wolf is
found mostly in the southern deciduous and mixed
forests (Jolicoeur and Henault 2002*) Coyote genes
found in the mitochondrial DNA of the specimen have
been reported before in Wolves in eastern Canada
(Lehman et al. 1991; Wilson et al. 2000). Wolves and
Coyotes are most likely to interbreed when Wolf den-
sity is low relative to Coyotes and when the species
are similar in size. In southern Québec, male Coyotes
weigh 14.6—18.7 kg (Fortin and Huot 1995*; Dumond
and Villard 2000; Villemure 2003*).
Wolf dispersal has been monitored in southern Qué-
bec (Messier 1985; Potvin 1987: Jolicoeur 1998*;
Villemure 2003*, but Wolves have not been docu-
mented crossing the St. Lawrence River. Harrison and
Chapin (1998) identified two potential corridors link-
ing Wolf populations north of the St. Lawrence River
to potential habitat in Maine and New Hampshire.
However, movements of Wolves south of their current
range are thought to be unlikely because of potential
barriers such as the St. Lawrence Seaway and regions
with high human population, high road density and
intensive agriculture (Wydeven et al. 1998). Potential
core habitat for Wolves has been identified in New
England as well as the Eastern Townships and Beauce
regions of Québec (Harrison and Chapin 1998; Mlade-
noff and Sickley 1998; Carroll 2003*; Jolicoeur and
Etcheverry, in preparation”).
Wolves are highly mobile and frequently move over
long distances (Van Camp and Glukie 1979; Fritts
1983: Mech 1987). Some of the longest dispersal move-
ments documented (460-555 km) occurred across a
mixture of forest, farmland, and 4-lane highways in
the upper Midwest (Mech et al. 1995; Wydeven et al.
1995). A Wolf in Alberta crossed rivers 0.5 - 2.0 km
' wide during summer (Van Camp and Glukie 1979),
| and Wolves have crossed 24 km on a frozen lake (Mech
1966). Wolves have increased in Minnesota (Fuller et
) al. 1992), and since the mid-1970s have naturally re-
colonized portions of northern Wisconsin and, more
recently, Upper Michigan (Mech and Nowak 1981;
Fuller et al. 1992). Wolves from Canada have recolo-
nized Montana for at least the past decade (Boyd et al.
1995). In a review of Wolf dispersal and recoloniza-
| tion, Wydeven et al. (1998) reported that 31 to 63%
of dispersing Wolves successfully settled and formed
pairs in new territories.
It is unclear whether Wolves have begun re-estab-
_ lishing in the Eastern Townships, or whether this Wolf
was simply a dispersing individual. While the Eastern
Townships may be a sink habitat for Wolves, this Wolf
was caught only 30-50 km from potential Wolf habi-
tat in Maine (Carroll 2003*). Further investigation is
necessary to confirm other possible Wolf observa-
tions in these regions. Reporting of Wolf sightings or
accidental Wolf captures south of the St Lawrence
river should be encouraged.
| Acknowledgments
We are grateful to Laurent Cloutier, trapper and for-
mer Eastern Townships Wildlife Protection Officer,
for providing the specimen and details of the capture
location. DNA analysis were funded by the Société
de la Faune et des Parcs du Québec. Thanks to C.
| Carroll, M. Festa-Bianchet, C. Reining and P. Struh-
| sacker for comments on an earlier draft of this manu-
| script.
Documents Cited (marked * in text)
Carrol, C. 2003. Carnivore restoration in the Northeastern
U.S. and Southeastern Canada: a regional-scale analysis of
habitat and population viability for wolf, lynx, and marten.
Progress report 1: Wolf viability analysis. Prepared for
The Wildlands Project. Orleans, California: Klamath Cen-
ter for Conservation Research. 38 pages.
Fortin, C., and J. Huot. 1995. Ecologie comparée du coyote,
du lynx et du renard roux au pare national Forillon. Report
prepared for Parks Canada. Département de Biologie,
Universite Laval. Ste-Foy, Québec. 291 pages.
_ Jolicoeur, H. 1998. Le loup du massif du lac Jacques-Cartier.
Québec, Ministére de l’Environnement et de la Faune,
Direction de la Faune et des Habitats, Direction de la
conservation et du patrimoine écologique. 132 pages.
Jolicoeur, H., and M. Hénault. 2002. Repartition géogra-
phique du loup et du coyote au sud du 52° paralléle et
estimation de la population de loups du Québec. Québec,
Societe de la faune et des pares du Québec, Direction du
développement de la faune et Direction de l’aménagement
de la faune des Laurentides. 51 pages.
| Jolicoeur, H., and P. Etcheverry (in preparation). Habitat
potentiel pour le loup sur la rive sud du St-Laurent. Québec,
Sociéte de la faune et des parcs du Québec, Direction du
développement de la faune.
Potvin, F. 1986. Ecologie du loup dans la reserve de Papi-
neau-Labelle. Québec, Ministére du Loisir, de la Chasse
et de la Péche, Direction générale de la Faune. 103 pages.
NOTES
609
Villemure, M. 2003. Ecologie et conservation du Joup dans la
region du parc national de la Mauricie. Mémoire de Maitrise.
Département de Biologie, Universite de Sherbrooke. Sher-
brooke, Québec, Canada. 89 pages.
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body condition of coyotes (Canis latrans) in eastern New
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Fritts, S. H. 1983. Record dispersal by a wolf from Min-
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Fuller, T. K, W. E. Berg, G. L. Radde, M. S. Lenarz, and
G. Blair Joselyn. 1992. A history and current estimate of
wolf distribution and numbers in Minnesota. Wildlife
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Harrison, D. J., and T. G. Chapin. 1998. Extent and con-
nectivity of habitat for wolves in eastern North America.
Wildlife Society Bulletin 26: 767-775.
Lehman, N., A. Eisenhawer, K. Hansen, L. D. Mech, R.
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Introgression of coyote mitochondrial DNA into sympat-
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104-119. ‘
Mech, L. D. 1966. The wolves of Isle Royale. U.S. National
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aspects of wolf dispersal from a Minnesota pack. Pages
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Chepko-Sade and Z. Tang Halpin. University of Chicago
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Mech, L. D., S. H. Fritts, and D. Wagner. 1995. Minnesota
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—a spatial prediction of favorable habitat and potential
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1-10.
Nowak, R. M. 1983. A perspective on the taxonomy of wolves
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L. N. Carbyn. Canadian Wildlife Service. 145 pages.
Nowak, R. M. 1995. Another look at wolf taxonomy. Pages
375-397 in: Ecology and conservation of wolves in a chang-
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Nowak, R. M. 2002. The original status of wolves in eastern
north america. Southeastern Naturalist 1: 95-130.
Peterson, R. L. 1966. The mammals of eastern Canada.
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610
Potvin, F. 1987. Wolf movement and population dynamics
in Papineau-Labelle reserve, Québec. Canadian Journal
of Zoology 66: 1266-1273.
Van Camp, J., and R. Glukie. 1979. A record long distance
move by a wolf (Canis lupus). Journal of Mammalogy 60:
236-237.
Wayne, R K., N. Lehman, M. W. Allard, and R. L. Honey-
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Genetic consequences of population decline and habitat
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G. Granacki, D. Pennock, J. B. Theberge, M. T. The-
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DNA profiles of the eastern Canadian wolf and the red
wolf provide evidence for a common evolutionary history
THE CANADIAN FIELD-NATURALIST
Vol. 118
independent of the gray wolf. Canadian Journal of Zoology
78: 2156-2166.
Wydeven, A. P., T. K. Fuller, W. Weber, and K. Mac Donald.
1998. The potential for wolf recovery in the Northeastern
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sional Publication Number 35. 642 pages.
Received 11 August 2003
Accepted 24 December 2004
Is Cost of Locomotion the Reason for Prolonged Nesting Forays of
Snapping Turtles, Chelydra serpentina?
SHANE R. DE SOLLA and KIM J. FERNIE
Canadian Wildlife Service, Environment Canada, Canada Centre for Inland Waters, 867 Lakeshore Road, P.O. Box 5050,
Burlington, Ontario L7R 4A6 Canada
de Solla, Shane R., and Kim J. Fernie. 2004. Is cost of locomotion the reason for prolonged nesting forays of Snapping Turtles,
Chelydra serpentina? Canadian Field-Naturalist. 118(4): 610-612.
Prolonged nesting forays were observed in five gravid Snapping Turtles (Chelydra serpentina), in 1999 and 2001. For all
observations, the females began exploratory nest excavations but failed to oviposit. Subsequently, all five females sought
refuge either by burying themselves in substrate, or by seeking shade under vegetation, presumably to wait until the following
day to resume nesting activities. By contrast, most observations of failed nesting resulted in the females abandoning the
nesting site and returning immediately to water. Although prolonged nesting attempts in other turtle species (i.e. kinosternids)
likely are associated with rainfall or predation risk, we speculate that these prolonged nesting attempts in Snapping Turtles
reduced the cost of terrestrial travel.
Key Words: Snapping Turtles, Chelydra serpentina, oviposition, nesting behaviour, cost of locomotion, Ontario
Nesting behaviour of Snapping Turtles (Chelydra
serpentina) has been described in detail elsewhere
(see Ernst et al. 1994), and is generally characterized
by behaviour that minimizes exposure on terrestrial
habitats. Briefly, nesting behaviour starts with emer-
gence from water, followed by nest site selection.
Females typically dig with their front limbs, and often
poke their noses into the substrate, presumably to deter-
mine if the soil type and/or hydration are adequate.
Subsequently, the rear limbs are used first to excavate
the nest cavity, then position the eggs during oviposi-
tion, and finally to bury the eggs. Subsequently, the
female leaves the nesting area, and returns to the water.
Although Snapping Turtles have been known to travel
more than 0.5 km overland to nesting sites (Obbard
and Brooks 1980), normally they nest at a site much
closer to the water. Regardless if the female was suc-
cessful in nesting or not, generally she returns to water
immediately afterwards. Nesting normally occurs in
the early morning or late evening, although females
may nest in the afternoon following rain. By mini-
mizing the distance or time traveled on land, female
Snapping Turtles may avoid energetic costs, or the risks
of dehydration or predation. Baudinette et al. (2000)
found that terrestrial locomotion was 2.6 times more
energetically costly than aquatic locomotion for the
Murray Short-necked Turtle (Emydura macquarii).
Snapping Turtles are particularly vulnerable to water
loss compared to other turtles (Ernst 1968) due to their
exposed skin. Although depredation of adults is rare,
adult females are occasionally taken by large predators,
such as bears or coyotes (Ernst et al. 1994). Here we
document five instances of prolonged nesting forays
in Snapping Turtles, which have not previously been
documented, and discuss possible reasons for this
behaviour.
Study Site
Observations were made from two locations in
Ontario, both known for many years to be nesting sites
for Snapping Turtles. The first nesting site, the north-
western shoreline of Coote’s Paradise, Hamilton
(43°16'N, 79°56'W), consists primarily of a communi-
ty vegetable garden and a wood chip pile on Ontario
Power Generation property. The nesting site is sepa-
rated from the open water by approximately 150 m,
first by a steep hill with thick shrub cover, and sec-
-ondly by dense cattails. The second nesting site, at
‘! Wheatley Provincial Park (42°5'N, 82°26'W), consists
of a series of sand, dirt, and wood chip piles in a main-
tenance area. Although normally open water is relative-
ly close to the nesting site (~ 50 m), in 2001 when the
observations were made, water levels were extremely
low, and most water in the park had drained into Lake
Erie, leaving bare mudflats. We observed many turtle
| tracks in the exposed mud leaving the park into Lake
Erie (de Solla, personal observation). Thus, at both
sites, the nesting females did not have nearby access
to water.
| Nesting Observations
De Solla et al. (2001) reported the deaths of two
gravid Snapping Turtles that buried themselves in a
| composting wood chip pile at Cootes Paradise, Hamil-
ton, on 7 and 9 June 1999. Both gravid turtles remained
in the wood chip pile until their deaths. Results of post-
mortem examinations were consistent with death due
to hyperthermia (de Solla et al. 2001); however, no
reasons for their behaviour were suggested. The behav-
iour of both females was consistent for females search-
| ing for suitable nesting sites, except after failing to
| successfully nest, both buried themselves in the wood
chip pile. A third female Snapping Turtle was also
| observed 8 June 1999 on the wood chip pile. Follow-
| ing apparently unsuccessful attempts to nest, the female
| was observed to be motionless for a few hours under
| the shade of burdock (Arctium spp.) and other vege-
| tation, which provided the only shade in the area. De
Solla did not touch her until later in the morning, but
| the turtle was found to be gravid. She remained in the
shade after being disturbed.
On 9 June 2001 at 1045, a female turtle was found
on a storage area for sand, dirt, and wood chips at
Wheatley Provincial Park. There were numerous tracks
on both the wood chips and dirt piles, possibly by
more than one female. There was abundant shade at
this site. She was sitting in shade under vegetation on
a small dirt pile, with no apparent movement, and no
evidence of nesting. She was left alone until 1200, at
which time the female was about 2 m from her previ-
ous location, further in shade under vegetation. She
did not move by 1300. At this time she was palpated,
found to be still gravid, and a blood sample was taken.
She was released at the same spot she was found,
where she remained for at least one hour, but she was
not subsequently observed. No temperature readings
were taken; however, the weather was sunny and hot.
On 12 June 2002, a female was seen in the vegetable
garden at Coote’s Paradise at approximately 2130.
Nearby were at least 10 digging attempts in freshly
cultivated soil, and she was observed digging with
her front limbs and poking her head into the soil. She
was observed for approximately an hour, but did not
show any signs of nesting. At approximately 2230, she
NOTES
611
was observed to have buried herself, with only the top
of her carapace showing. There was relatively little
shade by vegetation available. At approximately 0745
hrs, 13 June 2002, a female was seen walking very
near where the female from the previous night was
observed. This female was heavily covered with dirt,
suggesting that she was the same female that had buried
herself. No nesting attempts were made by 1000 hrs;
subsequently we left and she was not observed again.
Discussion
The five observations of nesting attempts by Snap-
ping Turtles had two common features; the delay was
prior to oviposition, and the turtles sought terrestrial
refuge by burying themselves in soil or wood chips,
or by staying in shade. We have no observations of
females remaining at the nesting ground after suc-
cessful oviposition. We are unaware of any published
reports of such behaviour in Snapping Turtles.
Various kinosternid species prolong their nesting
forays, typically by burying themselves before and/or
after oviposition (Iverson 1990; Burke et al. 1994; Wil-
son et al. 1999) adjacent to the nest. The duration of
nest attendance in species other than Chelydra appears
to be linked to the timing or duration of rainfall (Burke
et al. 1994: Ernst et al. 1994). Intensive disturbance
may also delay successful oviposition, and competitive
nesting by Green Turtles (Chelonia mydas) at high
densities may delay oviposition by a few days (Jessop
et al. 1999). Typically, after a failed nesting attempt
Snapping Turtles return to the wetland immediately
following cessation of nesting behaviour (de Solla,
persional observation).
We speculate that the prolonged nesting attempts
we observed in Snapping Turtles was to avoid the cost
of making a second trip between the water and nest-
ing site. All instances of prolonged nesting attempts
that we observed occurred a considerable distance from
water. Abandoning a nesting attempt would therefore
result in a relatively long journey to the water, and
back again to the nest site for a second oviposition
attempt. To avoid this cost, once a female aborts a
nesting attempt, she may burrow under substrate or
hide under vegetation until the following day. Females
nesting closer to wetlands are more likely to leave the
nest site and come back at a later time. At the Wildlife
Research Station (Algonquin Park), Snapping Turtle
nesting has been monitored on a dam at the southern
end of Lake Sasajewun for > 25 years, and all observed
nesting attempts that failed were followed by the imme-
diate withdrawal to the water (~ 5 m) by the female
(R. J. Brooks, University of Guelph, personal com-
munication). Similarly, at eight other nesting sites in
Ontario that the authors visited, all of which were
close to wetland habitat, females withdrew to water
following a failed nesting attempt. We did not count
the number of these observations, but de Solla has
frequently observed this behaviour.
612
In two of the five observations of prolonged nesting
attempts, the turtles died of hyperthermia after bury-
ing themselves in composting wood chips (de Solla
et al. (2001). We speculate that in most cases where
females bury themselves, they use non-composting
material, and thus are not at risk of hyperthermia.
Acknowledgments
We thank Wheatley and Algonquin Provincial Parks,
and Ontario Power Generation for permission to enter
their properties to look for turtle nests. Ron Brooks
and anonymous reviewers gave valuable comments
on earlier drafts.
Literature Cited
Baudinette R. V., A. M. Miller, and M. P. Sarre. 2000.
Aquatic and terrestrial locomotory energetics in a toad and
a turtle: a search for generalisations among ectotherms.
Physiological and Biochemical Zoology 73: 672-682.
Burke V. J., J. W. Gibbons, and J. L. Greene. 1994. Pro-
longed nesting forays by common mud turtles (Kinosternon
subrubrum). American Midland Naturalist 131: 190-195
THE CANADIAN FIELD-NATURALIST
Vol. 118
de Solla S. R., D. Campbell, and C. A. Bishop. 2001.
Hyperthermia induced mortality of gravid snapping tur-
tles, Chelydra serpentina, and eggs in a wood chip pile.
Canadian Field-Naturalist 115: 510-512.
Ernst, C. H. 1968. Evaporative water-loss relationships of
turtles. Journal of Herpetology. 2: 159-161.
Ernst, C. H., J. E. Lovich, and R. W. Barbour. 1994. Turtles
of the United States and Canada. Smithsonian Institution
Press. Washington.
Iverson, J. B. 1990. Nesting and parental care in the mud
turtle, Kinosternon flavescens. Canadian Journal of Zoology
68: 230-233.
Jessop, T. S., C. J. Limpus, and J. M. Whittier. 1999. Plasma
steroid interactions during high-density green turtle nest-
ing and associated disturbance. General and Comparative
Endocrinology 115: 90-100.
Obbard M. E., and R. J. Brooks. 1980. Nesting migrations of
the snapping turtle (Chelydra serpentina). Herpetologica
36: 158-162.
Wilson D. S., H. R. Mushinsky, and E. D. McCoy. 1999.
Nesting behavior of the striped mud turtle, Kinosternon
baurii (Testudines: Kinosternidae). Copeia. 1999: 958-968.
Received 11 October 2003
Accepted 23 November 2004
Significant Vascular Plant Records from the Hamilton Area, Ontario
CARL ROTHFELS
Royal Botanical Gardens, 680 Plains Road W., Burlington, Ontario L7T 4H4 Canada
Rothfels, Carl. 2004. Significant vascular plant records from the Hamilton area, Ontario. Canadian Field-Naturalist 118(4):
612-615.
Four additions to the known vascular flora of Ontario (Aesculus pavia, Ambrosia x helenae, Anthriscus caucalis, Verbena
bonariensis) and ten other provincially significant records are discussed. Of the 14 taxa listed, two (Actaea x ludovici and
Ambrosia X helenae) are native.
Key Words: adventive species, flora, rare species, distribution, Hamilton, Halton, Ontario.
Field and herbarium work centred around Royal
Botanical Gardens on the border between Hamilton
and Burlington, Ontario (43°29.00'N, 79°88.00'W), has
resulted in the following 16 provincially significant
vascular plant records in 2002. For locally significant
records, see Rothfels (2003). All records are supported
by specimens in the Royal Botanical Gardens herbar-
ium (HAM).
Taxa preceded by an asterisk (*) are not native to
the Hamilton Region. Taxon names are followed by
their subnational rank (Srank) as of 1998, where appli-
cable (see Newmaster et al. 1998). An Srank of S1
indicates a very rare native taxon, with generally five or
fewer occurrences in Ontario; a rank of SE1 is similar,
but refers to a non-native taxon; and a rank of SEH
(historical) indicates a non-native species that has
typically not been recorded in Ontario in the past 20
years (Newmaster et al. 1998). The names used follow
Kartesz and Meacham (1999*).
Actaea x ludovici B.Boivin. Hybrid Baneberry S1
RANUNCULACEAE
One clump of this hybrid was collected from the
Devil’s Punchbowl Environmentally Significant Area,
in Hamilton (43°11.80'N, 79°38.50'W). Both parental
species (Actaea rubra (Aiton) Willd. and Actaea
pachypoda Ell.) were in close proximity. Despite the
overlapping ranges of the parental taxa, the hybrid is
rare (Voss 1985), perhaps due to differing phenology
(Pringle, personal communication). In Canada, it is
recorded from Ontario and Quebec (Kartesz and
Meacham 1999*). (C. J. Rothfels 305).
* Aesculus pavia L. Red Buckeye HIPPOCASTANACEAE
This species is an addition to the flora of Ontario
(Newmaster et al. 1998). Over ten young trees were
found naturalized in the Red Hill Creek escarpment
valley, City of Hamilton, by Megan Ogilvie and Albert
Garofalo. These plants are likely spreading from trees
2004
| planted in 1927 (Bruce Duncan, personal communica-
) tion). A species of the southern United States, it
| reaches its northern limit in Kentucky, West Virginia,
and southern Illinois (Kartesz and Meacham 1999*),.
| It differs from A. glabra Willd. and A. hippocastanum
| L., the other two species reported from Ontario, by its
/ smooth fruit (Edmondson 1997), among other features.
| It is, due to its reddish flowers, perhaps most likely to
| be confused with the frequently-planted Aesculus
_ xcarnea Hayne, which differs in its size (A. pavia is a
| small tree or large shrub, A. xcarnea is a large tree),
_ leaf shape (A. pavia has lanceolate leaves unlike the
| obovate leaves of A. xcarnea) and petal shape (A.
_ pavia has dissimilar petals with two broad lateral
_ petals and two long-stalked spoon-shaped petals; all
_ petals of A. xcarnea are large and shaggy) (Krussman
_ 1984). (M. Ogilvie, A .Garofalo et al. s.n.; HAM 16221).
_ * Aethusa cynapium L. Fool’s-parsley SE1 APIACEAE
This species was found new for both the City of
Hamilton (Goodban 1995) and Lambton County (Tiedje
and Tiedje 2002) in 2002. In Hamilton, it is fairly
common along wooded paths along the base of the
Niagara Escarpment in the Devil’s Punchbowl Envi-
ronmentally Significant Area (43°12.20'N, 79°40.70'W).
_ The Hamilton specimen was determined only to the
_ specific level. The Lambton County specimen was
_ determined as A. cynapium ssp. cynapioides (M. Bieb.)
_ Nyman, the larger woodland subspecies (using Tutin
1968) and it was common on the Ausable River flood-
plain in the Rock Glen Conservation Area (43°05.10'N,
81°06.80'W). Aethusa cynapium has been found in the
Great Lakes States, and in Quebec, New Brunswick,
and Nova Scotia (Kartesz and Meacham 1999*). The
early Canadian reports describe this species as a garden
weed “introduced with garden seeds from Europe”
(Macoun 1883), and list it from Hastings and North-
umberland Counties in Ontario, and as “occasional”
in New Brunswick (Macoun 1883). (J. Rothfels & J.
Shearer 243; C. J. Rothfels 274).
* Amaranthus blitum L. Purplish Amaranth SEH
AMARANTHACEAE
This species is new for Halton Region (Varga et al.
2000). A purple-leaved amaranth, it is scattered irreg-
ularly in the lawns at Royal Botanical Gardens Centre
(43°17.40'N, 79°59.70'W) where it appears to be dis-
persed by Canada Geese. Scoggan (1978) reports this
species as introduced in waste ground in Elgin County,
Huron County, and Waterloo Regional Municipality
in Ontario, and from Masson, Montreal and Quebec
City in Quebec. (C. J. Rothfels & D. Gugler 303).
Ambrosia x helenae Rouleau Hybrid Ragweed
ASTERACEAE
This taxon is an addition to the flora of Ontario
(Newmaster et al. 1998). It is a hybrid between Com-
mon Ragweed (Ambrosia artemisiifolia L.) and Giant
Ragweed (Ambrosia trifida L.). Although the ranges
NOTES
613
of these two species overlap frequently, the hybrid is
very rare (Wagner 1958). It was collected along the
north shore trails of the Cootes Paradise Nature Sanc-
tuary in Hamilton (43°16.90'N, 79°54.10'W). The
type locality is in Quebec (Wagner 1958), and it has
also been found in Michigan, New York State, and
Ohio (Kartesz and Meacham 1999*). (D. Gugler s.n.:
HAM 15959).
* Anthriscus caucalis M. Bieb. Bur-chervil APIACEAE
This species is an addition to the flora of Ontario
(Newmaster et al. 1998). It was abundant on disturbed
ground near the Royal Botanical Gardens’ Laking
Garden (43°17.50'N, 79°53.30'W). Shortly after the
discovery, the site was mowed by the owner. This
species is known in Canada only from Nova Scotia, but
is scattered widely across the United States (Kartesz
and Meacham 1999*), and is easily distinguished from
its more common congener (A. sylvestris (L.) Hoffm.)
by the hooked hairs on the fruit (e.g., Gleason and
Cronquist 1991). (C. J. Rothfels & J. L. Reader 115).
* Anthyllis vulneraria L. Lady’s-fingers SE1
FABACEAE
This species is new for the City of Hamilton (Good-
ban 1995). It was fairly common, but local, in disturbed,
weedy, poorly drained ground (a pipeline right of way)
in the Beverly Swamp Environmentally Significant
Area (43°21.10'N, 80°06.80'W). It has been reported
from British Columbia, Ontario, Quebec, Newfound-
land, and New Brunswick (Kartesz and Meacham
1999*). Scoggan (1978) notes that it is “locally intro-
duced into clover fields and waste places,” a description
that concords closely with this report, and lists records
from Oxford, Waterloo and Wellington Counties in
Ontario, from “slaty banks of the Restigouche River
near Matapedia” in Quebec, and from Newcastle in
New Brunswick. (C. J. Rothfels 143).
* Cardamine impatiens L. Narrow-leaved Bittercress
SE1 BRASSICACEAE
This species is new for the City of Hamilton (Good-
ban 1995). Four plants were found along the north
shore of the Cootes Paradise Nature Sanctuary, near a
small boat-storage facility, along a partially disturbed
forest edge (43°16.90'N, 79°54.00'W). This is an up-
right Cardamine, with distinctly auriculate pinnately-
divided leaves (e.g. Voss 1985). Mulligan (2002) only
saw a single Canadian specimen, collected by J. M.
Weber in 1980 for Port Credit, Ontario, and notes that
this species is “sporadic and uncommon” in the United
States. This species was not listed by Scoggan (1978).
(C. J. Rothfels 88).
* Coronopus didymus (L.) J.E.Sm. Lesser Wart-cress
SEI BRASSICACEAE
This strange little mustard is new for the City of
Hamilton (Goodban 1995). It is a common weed in
some of the Royal Botanical Gardens’ Rock Garden
614
flower beds (43°17.20'N, 79°53.60'W). This is the
second confirmed record for Ontario (Oldham personal
communication). It first established a foothold in the
east — Scoggan (1978) lists five counties in Nova
Scotia and two in New Brunswick containing this
species — but it also occurs across the country (a single
record each in British Columbia, Alberta, Quebec, and
Newfoundland (Scoggan 1978). The first Canadian
records are from Gaspé Basin, Quebec, and North
Sidney, Nova Scotia, in 1862 and 1883, respectively
(Mulligan 2002). Coronopus didymus can be differen-
tiated from Coronopus squamatus (Forssk.) Aschers.
(which is also weedy) by its wrinkled cordate fruits that
are notched at the summit. The fruits of C. sguamatus
are conspicuously apiculate at the summit (e.g.
Holmgren 1998). (C. J. Rothfels 71).
* Euonymus fortunei (Turcz.) Hand.-Mazz. Wall-
creeper SE] CELASTRACEAE
This species has been known from Royal Botani-
cal Gardens’ sanctuary lands for several years (Smith
2003), but has not been collected until this year. It is
widespread but local in the Cootes Paradise Nature
Sanctuary, where it occasionally forms small dense
patches on the oak-hickory slopes (43°1620'N,
79°55.10'W). It seems to be increasing in southern
Ontario, and may become a problem in some natural
areas (Oldham, personal communication 2003). (C.
J. Rothfels 235).
* Macleaya cordata (Willd.) R. Br. Plume-poppy
SEH PAPAVERACEAE
This species is new for the City of Hamilton (Good-
ban 1995). This large plant is occasionally planted as
an ornamental. Its occurrence on the east shore of the
Cootes Paradise Nature Sanctuary (43°16.80'N,
79°53.50'W) is mysterious; it could be a persistent
population from some unknown source or it could be
“spontaneous”. Voss (1985) describes it as “seldom
escaping” in Michigan, and Scoggan (1978) lists it as a
“garden escape” that is “scarcely established” in Nor-
folk County in Ontario and Missisquoi County in
Quebec. (C. J. Rothfels 318).
* Myrrhis odorata (L.) Scop. Scented Myrrhis SE1
APIACEAE
This large umbellifer is new for Halton Region
(Varga et al. 2002). It is escaping from the Royal Bot-
anical Gardens’ Scented Garden into the neighboring
ravines (43°17.50'N, 79°52.60'W). Currently, its spread
is limited, and will be tracked in future years. It is
reported from two other Ontario locations: St. Thomas,
Elgin County, and Manitoulin Island, Manitoulin
District (Pringle 1994); as well as from British Colum-
bia, Nova Scotia, Michigan, Pennsylvania, and Oregon
(Kartesz and Meacham 1999*). The smooth fruit and
large size help differentiate this species from the native
Osmorhiza species (Pringle 1994). (C. J. Rothfels
190).
THE CANADIAN FIELD-NATURALIST
Vol. 118
* Sorghum bicolor (L.) Moench ssp. bicolor. Sorghum
SE] POACEAE
This species is new for the City of Hamilton (Good-
ban 1995). It was common with other weeds on freshly
disturbed ground at the Royal Botanical Gardens’
outdoor compost facility (43°17.10'N, 79°53.70'W).
It has been found in Quebec and most U.S. states,
and is a noxious weed in three states (Kartesz and
Meacham 1999). (C. J. Rothfels 317).
* Verbena bonariensis L. Purpletop Vervain VERBE-
NACEAE
This species is an addition to the flora of Ontario
(Newmaster et al. 1998). One plant was found on the
Osprey Marsh Christmas tree carp barrier (a row of
old Christmas trees erected in the mud to prevent carp
from travelling from Grindstone Creek into Osprey
Marsh), in the Hendrie Valley Nature Sanctuary, Halton
Region (43°17.40'N, 79°52.90'W). It might have ar-
rived in the treads of the machinery used to place the
trees in the winter. This species is not in the Royal
Botanical Gardens’ cultivated plants database, and
thus has theoretically never been planted on RBG
property. One individual of this species was seen at
the Childrens’ Garden in Westdale (not operated by
RBG) in 2002, approximately 3.5 km from the Osprey
Marsh population. This species is introduced to the
southern States, and has also been reported from Ore-
gon, New York State, New Jersey, and New Hampshire
(Kartesz and Meacham 1999*). It has not been re-
ported from Canada. (C. J. Rothfels & I. Vaithilingam
435). A previously-overlooked specimen was also
uncovered at HAM. It is an undated specimen from a
“river bank” at “Lake Erie,’ and was identified by J.
S. Pringle in 1964 (K. Stanley s.n.). In light of the
2002 discovery, it seems reasonable that this record
could also have been “spontaneous”.
Discussion
The eight taxa found new for Hamilton add to the
current published list of 1304 species (Goodban 1995),
and the four new taxa for Halton bring that region’s
tally to 1305 (Varga et al 2000). Additionally, four of
the taxa are new for Ontario. Twelve of the fourteen
records discussed are non-native occurrences, several
of which, especially Aethusa cynapium, Euonymus
fortunei, and Sorghum bicolor, should be watched for
invasive tendencies.
Acknowledgments
Thanks to Jim Pringle for assistance in the deter-
mination of Aethusa cynapium, Amaranthus blitum,
Anthriscus caucalis, Cardamine impatiens, Coronopus
didymus, and Macleaya cordata; thanks to Jim Pringle
and Michael J. Oldham for helpful earlier reviews of
this manuscript, and to Megan Ogilvie, Albert Garofalo
and Dean Gugler for submitting their records. Con-
tribution from Royal Botanical Gardens Number 1 14.
2004 NOTES 615
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Carolina Botanical Garden. Compact disc. Rothfels, C. J. 2003. Significant 2002 Hamilton Study Area
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Zaje. 2000. Distribution and status of the vascular plants
of the greater Toronto Area. Ontario Ministry of Natural
Resources, Aurora District. August 2000. 102 pages.
Voss, E. G. 1985. Michigan Flora: Part II Dicots (Saururaceae
to Cornaceae). Cranbrook Institute of Science Bulletin
59. University of Michigan Herbarium. 724 pages.
Wagner, W. H., Jr. 1958. The hybrid ragweed, Ambrosia
artemisiifolia x trifida. Rhodora 60: 309-316.
Received 10 November 2003
Accepted 21 December 2004
Do Rhinoceros Auklet, Cerorhinca monocerata, Fledglings Fly to the
Sea from Their Natal Burrows?
JAMES L. HAYWARD and JERE K. CLAYBURN
Biology Department, Andrews University, Berrien Springs, Michigan 49104-0410 USA
Hayward, James L., and Jere K. Clayburn. 2004. Do Rhinoceros Auklet, Cerorhinca moncerata, fledglings fly to the sea
from their natal burrows? Canadian Field-Naturalist 118(4): 615-617.
The mode of departure of Rhinoceros Auklet fledglings from their nest burrows has remained uncertain. Both walk-down
and fly-down hypotheses have been proposed. Here we use the unique geography of Protection Island, Washington, to eval-
uate the fly-down hypothesis. Some fledglings raised on Protection Island do appear to walk to the water, but our results
suggest that many of the island’s fledgling Rhinoceros Auklets fly to the sea.
Key Words: Rhinoceros Auklet, Cerorhinca monocerata, fledgling departure, Washington.
Rhinoceros Auklets (Cerorhinca monocerata) are
the most abundant puffins in the waters of the Pacific
Northwest. Unlike Tufted and Horned puffins (Frater-
cula cirrhata and F: corniculata, respectively), which
also breed along western North America, members of
most populations of Rhinoceros Auklets leave their
nesting colonies before dawn to feed and return after
sunset (Wilson and Manuwal 1986; but see Thoresen
1980). Consequently, some basic information on the
behavior of these birds remains obscure, despite grow-
ing knowledge of their breeding biology (Richardson
1961; Scott et al. 1974; Leschner 1976; Summers and
Drent 1979; Vermeer 1978, 1979, 1980; Thoresen 1980,
1983; Wilson and Manuwal 1986; Wilson 1993; Gaston
and Duchesne 1996).
One elusive piece of information involves the mode
of departure from nest sites by newly-fledged Rhinoc-
eros Auklets. Young Atlantic Puffins (F. arctica) walk,
616
flutter, or fly to the water from their burrows (Lockley
1934: Richardson 1961; Gaston and Jones 1998), where-
as fledgling Cassin’s Auklets (Ptychoramphus aleuti-
cus) fly to the sea after making short “practice flights”
(Manuwal 1974). Leschner (1976) found Rhinoceros
Auklet fledglings that were too small to fly “crouched
under rocks or crevices in the morning” on Destruction
Island, Washington; this suggested to her “that fledg-
lings walk or flutter to the water.” Similarly, Wilson
(1977) observed fledgling Rhinoceros Auklets on Pro-
tection Island, Washington, “walking down the grass
covered slopes” to the sea. But Richardson, (1961) who
also worked on Protection Island, wrote that “flight
[capability] ... appears to develop precociously,’ and
that like the “half-grown young” of murres, fledgling
Rhinoceros Auklets “fly down to the water.”
On Protection Island, hundreds of Rhinoceros Auk-
lets nest along a sandy cliff that rises above Violet Point,
a gravel spit that contains a large Glaucous-winged
Gull (Larus glaucescens) colony. Each summer, scores
of auklet fledglings are found dead within a relatively
defined area of the gull colony, across an artificial
channel and marina from the cliff. The distribution of
dead fledglings and the unique semi-natural geography
of Protection Island allowed us to evaluate Richard-
son’s fly-down hypothesis.
Methods
Protection Island, Jefferson County, Washington
(48°08'N, 122°55'W), consists of a 35—76-m high pla-
teau surrounded by steep, grass-covered, sandy cliffs
ideally suited for Rhinoceros Auklet burrowing. The
largest Rhinoceros Auklet colony in Washington is
located here, with approximately 27 549 burrows (Wil-
son and Manuwal 1986). Violet Point, a gravel spit that
extends 800 m east from the upper island, contained
around 5 100 of Glaucous-winged Gull nests during
this study (J. G. Galusha, personal communication).
In July and August 1992, 1993, and 1997 the location
of each auklet fledgling found dead on Violet Point was
plotted by measuring its north or south distance from
a transect that measured its eastward distance from the
base of the island’s east-facing cliff. To estimate age at
death, culmen and tarsal lengths, if still present, were
measured in 1992 and 1993. The height of the highest
(60 m) nesting burrows on the cliff in relation to the
distribution of dead fledglings on Violet Point was used
to approximate a range of presumed fledgling flight
path angles trigonometrically.
Results
One hundred and twenty-one dead fledglings (43 in
1992, 11 in 1993, and 67 in 1997) were counted between
106 m east of the cliff base, at the western margin of the
gull colony, and 398 m east of the cliff base, toward
the center of the gull colony (Figure 1). The fledglings
apparently died as a result of hitting the spit or being
attacked by resident gulls. No dead fledglings were
THE CANADIAN FIELD-NATURALIST
Vol. 118
A. Aerial view
Strait of
Juan de Fuca
Protection
Island
60-m cliff
with auklet
burrows
Violet Point
(Exeter Of quill COL Cy)
_—_—_—_——_——_——[$ (478 m - longest estimated fledgling flight)
See! (111 m - shortest estimated fledgling flight)
bt (292 m - range Of dead fledglings)
B. Side view
Ficure |. A. Aerial view of Violet Point, Protection Island,
Washington. Dots indicate locations of dead fledgling
Rhinoceros Auklets found during July and August, 1992,
1993, and 1997. Lines below indicate approximate extent
of the spit occupied by the gull colony, extent of fledgling
auklet corpses, and estimated extents of fledgling auklet
flight distances. B. Side view of Violet Point showing the
estimated range of Rhinoceros Auklet fledgling flight
paths, sloping from 7°—18° from the highest (60 m) natal
burrows above the gull colony; fledgling flights from
lower burrows would exhibit progressively shallower
angles.
found beyond 398 m. The pooled mean (+ SD here
and below) distance of fledgling corpses from the base
of the nest cliff was 303 + 58.0 m (n = 54, range =
106-398 m). Mean culmen length was 24.4 + 3.0 mm
(n = 35), and mean tarsus length was 37.9 + 1.6 mm
(n = 48); Rhinoceros Auklets of this size are about
45 days old (Wilson and Manuwal 1986). During late
July and early August, we occasionally found live
Rhinoceros Auklet fledglings hiding in grass between
the nesting cliff and the channel/marina, and we reg-
ularly observed fledglings swimming in the water of
the marina/channel.
Discussion
Large numbers of dead fledglings found in gull ter-
ritories east of the marina/channel water and across
from the nesting cliff support the hypothesis that these
fledglings flew down and over the water from their
natal burrows. Alternate means of reaching the east
side of the marina/channel were highly unlikely: (1)
walk/flutter down slope, enter the marina/channel
water from the west shore, leave the water on the east
shore, enter the gull colony, be killed; (2) walk/flutter
2004
down slope, enter the colony north of the marina/
channel, walk/flutter through a gauntlet of gull terri-
tories to the east side of the water, be killed; (3) walk/
flutter down slope, enter the colony north of the
marina/channel, be killed, then be transported to dis-
tant points east of the water by gulls. With respect to
(3), it should be noted that fledging Rhinoceros Auk-
lets exhibit an average mass of 360 g (Wilson and
Manuwal 1986), 34% of the average mass of 1051 g
(Vermeer 1963) for adult Glaucous-winged Gulls in
this region; thus it appears unlikely that auklet corpses
could be moved very far from the place where they
were killed.
Our data, with those of Richardson (1961), Lesch-
ner (1976), Wilson (1977), and Wilson and Manuwal
(1986), support the following scenario for the depar-
ture of fledgling Rhinoceros Auklets from their nest
burrows on Protection Island: In late July and early
August, some fledgling auklets walk and flutter, but
also many fly directly away from their natal burrows.
Fledglings cannot sustain prolonged flight, however,
and from the highest nests lose altitude at a rate of
13-32 m/100-m distance, with a slope of 7°-18°
(Figure 1B); fledgling flights from lower burrows
would exhibit progressively shallower angles. Fledg-
lings from preferred nest sites located directly above
the ocean (Richardson 1961) reach the water success-
fully. Fledglings that fly from nest sites along the cliff
above Violet Point hit the gull colony where they are
killed, unless they veer to the ocean or are fortunate
enough to land in the marina/channel. Whether this
scenario applies to fledgling departures at other Rhi-
noceros Auklet colonies remains unknown.
Acknowledgments
We thank Robert Edens, Jean Takekawa and Kevin
Ryan for permission to work on Protection Island
National Wildlife Refuge, Ulrich Wilson for valuable
discussions about Rhinoceros Auklets, Shandelle Hen-
son for comments on the manuscript, and Walla Walla
College Marine Station for logistical support during
this study. Funding was provided by faculty grants to
JLH from Andrews University.
Literature Cited
Gaston, A. J., and S. B. C. Dechesne. 1996. Rhincoceros
Auklet: Cerorhinca monocerata. The Birds of North Amer-
NOTES
617
ica (212). American Ornithologists’ Union, Washington,
D. C., and Academy of Natural Sciences, Philadelphia,
Pennsylvania. 20 pages.
Gaston, A. J., and I. L. Jones. 1998. The Auks: Alcidae.
Oxford University Press, Oxford. 349 pages.
Leschner, L. L. 1976. The breeding biology of the Rhinoceros
Auklet on Destruction Island. M.S. thesis, University of
Washington, Seattle. 77 pages.
Lockley, R. M. 1934. On the breeding habits of the puffin:
With special reference to its incubation and fledgling peri-
ods. British Birds 27: 214-223.
Manuwal, D. A. 1974. The natural history of Cassin’s Auk-
let (Ptychoramphus aleuticus). Condor 76: 421-431.
Richardson, F. 1961. Breeding biology of the Rhinoceros
Auklet on Protection Island, Washington. Condor 63: 456—
473.
Scott, J. M., W. Hoffman, D. Ainley, and C. F. Zeillemaker.
1974. Range expansion and activity patterns in Rhinoceros
Auklets. Western Birds 5: 13-20.
Summers, K. R., and R. H. Drent. 1979. Breeding biology
and twinning experiments of Rhinoceros Auklets on Cle-
land Island, British Columbia. Murrelet 60: 16-22.
Thoresen, A. C. 1980. Diurnal land visitations by Rhinoceros
Auklets. Western Birds 11: 154.
Thoresen, A. C. 1983. Diurnal activity and social displays of
Rhinoceros Auklets on Teuri Island, Japan. Condor 85: 373—
SU
Vermeer, K. 1963. The breeding ecology of the Glaucous-
winged Gull (Larus glaucescens) on Mandarte Island,
B. C. Occasional Papers of the British Columbia Provin-
cial Museum Number 13. 104 pages.
Vermeer, K. 1978. Extensive reproductive failure of Rhi-
noceros Auklets and Tufted Puffins. Ibis 120: 112.
Vermeer, K. 1979. Nesting requirements, food and breeding
distribution of Rhinoceros Auklets, Cerorhinca monocer-
ata, and Tufted Puffins, Lunda cirrhata. Ardea 67: 101—
110.
Vermeer, K. 1980. The importance of timing and type of prey
to reproductive success of Rhinoceros Auklets Cerorhinca
monocerata. Ibis 122: 342-350.
Wilson, U. W. 1977. A study of the biology of the Rhinoceros
Auklet on Protection Island, Washington. M.S. thesis, Uni-
versity of Washington, Seattle. 98 pages.
Wilson, U. W. 1993. Rhinoceros Auklet burrow use, breeding
success, and chick growth: Gull-free vs. gull-occupied habi-
tat. Journal of Field Ornithology 64: 256-261.
Wilson, U. W., and D. A. Manuwal. 1986. Breeding biology
of the Rhinoceros Auklet in Washington. Condor 88: 143—
156.
Received 6 February 2004
Accepted 25 October 2004
A Tribute to Thomas Henry Manning 1911-1998
BRENDA CARTER
R.R. #4. Merrickville, Ontario KOG 1NO Canada
Carter, Brenda. 2004. A tribute to Thomas Henry Manning 1911-1998. Canadian Field-Naturalist 118(4): 618-625.
I first met Tom Manning on his Merrickville farm
in the spring of 1965, during lambing time. Andrew
and Betty Macpherson who had both travelled with
him in the Arctic, brought me out to see Arctic Foxes.
These captive animals were part of a research program
on the influence of light on moult timing. On the way
to. Merrickville, I listened to their stories about Tom’s
legendary explorations and scientific expeditions. I was
therefore prepared for the prospect of meeting an Arc-
tic hero. Instead, I found a quiet, stocky man in his
fifties, dressed in faded and ragged overalls tending
his sheep. The stub of a hand-rolled cigarette hung from
his lower lip — perpetually unlit. He did not seem pleased
at extra company and bluntly asked why I had been
brought out. Later, over glasses of his lethal home-
made cider, I realized that here was a man who was
much more than he seemed. By the end of that day we
had become firm friends — a friendship that was to last
until his death in November of 1998.
Few knew Tom Manning well; and few indeed were
given a chance to comprehend, as a whole, the com-
plexity and sheer bulk of his phenomenal life’s work.
Except for a very few close friends, Tom was deeply
private, and even withdrawn. He was a relentless and
dogged scientist who spared no effort to find either
the original source of any information, or to redo any
questionable measurements — even if they were his
own. Applying his logical and inquiring mind to all
kinds of life-forms, natural phenomena and expedi-
tion challenges, Tom also had the skill, intuition and
knowledge to assess and react appropriately in critical
situations. He did so with a rapidity I found astonishing.
His mental brilliance, awesome physical endurance,
good looks and charm, combined with great modesty
and fondness for red sportscars, contributed to a re-
markable personality.
On the 22 of December, 1911, Thomas Henry Man-
ning was born into a gentleman’s life. Even as an infant,
he defied prediction and showed his amazing capacity
for endurance. Except for a surgeon who “did not want
to commit murder on Christmas Day” and reluctantly
operated, Tom might soon have died, a victim of pyloric
stenosis. Tom was the only child of Dorothy (nee Ran-
dall) whose brother was the last gentleman jockey in
England, and Thomas Edward Manning, (TEM) who
managed the family brewery and was cricket Captain
for Northamptonshire. Their privileged son was neither
destined nor inclined to follow in his father’s foot-
steps.
Tom once told me that his first childhood memory
was of being put out on a blanket in the sun before he
could walk. He remembered his excitement and free-
dom at being outside. Tom never lost his passion for
open air which propelled him into a life of exploration
and adventure. His scientific career began and ended
with eggs. As a boy, he had a passion for collecting eggs,
and this hobby directed him into a career as a biologist,
rather than a brewery owner as his father expected. A
friendly gardener sparked his interest in nests, and Tom
undoubtedly learned to keep notes and data for his tro-
phies. This mixture of intense interest and attention
to detail stood him in good stead as he completed, at
the age of seventy, his last pioneering scientific work on
weight lost by eggs during incubation for the Canadian
Field-Naturalist.
Tom was educated at Harrow, and like his father,
attended shooting parties and rode with the famous
Pytchley Hunt. There were, however, some interesting
dissimilarities. He cleaned the skulls of the mammals
and birds shot, drying them in his mother’s linen cup-
board. Eventually, he escaped from the hunt meets be-
cause he disliked the formalities and confining clothes.
While at Harrow, Tom took a cycling trip with a
school friend and discovered an unsuspected physical
trait. As the pair wound their way through country
lanes toward the southern coast of England, he found
himself farther and farther ahead. With characteristic
independence and detachment from social niceties,
he left his friend far behind and continued on, solely
interested in how far he could travel in one day. At the
end of that journey, he was surprised by his endurance.
Although he would never admit it, this ability was
more than unusual.
After his death, I discovered a buried manuscript,
transcribed from a 1931 diary. It gives an account of
his first expedition to Iceland and the Faroe Islands
with Harrow school friend, “Twitch” Mitchell. Tom’s
descriptions of unidentified gulls and seabirds revealed
how scrupulous his note-taking was at the young age
of twenty. Equally remarkable, for a twenty-year old,
was the care he took in logistical planning; from
deciding on exact food supplies and arranging trans-
618
CARTER: THOMAS HENRY MANNING
Thomas Henry Manning with Massey Medal presented by the Royal Canadian Geographical Society in 1977 with portrait
of former Government-General Vincent Massey in background.
portation, to sorting out necessary visas. This thor- pithy comments about the unfortunate “Twitch”, dis-
oughness remained as long as I knew him. Having _ gruntled bureaucrats and miserable weather.
travelled with him, I could also recognize in that early After Harrow, Tom read Natural Sciences at Jesus
diary his trademark dry and ironic humour, hidden in College, Cambridge. This academic subject captivat-
620
ed him and provided a continuum with his childhood
interest in natural history. Owing to several circum-
stances, the most prominent being boredom, he never
took his degree. Instead, in the summer of 1932, at the
age of twenty-one, he embarked on a serious journey,
walking the length of the Atlantic coast of Norway
on his own. Joined later by Reynold Bray, his close
school friend from Harrow, the pair proceeded east-
ward into Finland, making a winter trip by reindeer
sledge through Lapland. In 1932, near the end of their
trip, they trespassed into Russia. Tom told me they were
arrested by villagers armed with pitchforks, who sus-
pected them of spying. They subsequently spent three
weeks in a Leningrad jail, being fed on increasingly
weakened soup, until the British Consul secured their
release.
Exploration, travel and adventure were now Tom’s
calling. From 1933-1935, he made a solitary expedi-
tion to Southampton Island, northern Hudson Bay, to
study a Snow Goose colony. He mapped the island
under the auspices of the Royal Geographical Soci-
ety and collected birds and mammals for the British
Museum (Natural History). His longest journeys were
made by dogsled in winter. From the Inuit of Coral Har-
bor (on the island’s southern coast) he learned how to
build an igloo, drive a dog team and hunt seal and
caribou. When I once asked why he had an aversion to
dumplings, he replied that during that first summer he
had been given flour and baking powder by the Hud-
son’s Bay Company Manager. Given no instructions
and being too proud to ask what he should make, he
existed on a tiresome diet of dumplings until rescued
by the Inuit who showed him how to make bannock.
Tom had no sooner returned to England in 1935 than
he started to organize a larger expedition to South-
ampton Island, and Foxe Basin. The five members of
the British-Canadian Arctic Expedition, consisting of
Tom, Graham Rowley, Reynold Bray, Pat Baird, Richard
(Dick) Keeling and Peter Bennett (who later replaced
Dick); arrived in Churchill in May of 1936. A smaller
team consisting of Tom, Graham and Pat sailing in the
Polecat, a 30-foot open whaleboat, established their
main base at Coral Harbor. Each pursued his own
investigation in biology, archaeology and geology.
The expedition was later marred by the tragic death
of Reynold Bray, who drowned after being blown out
to sea in a collapsible boat.
By the summer of 1938, Tom was alone in the field,
at a camp in the Cape Dorset area of southern Baffin
Island. He sent a message by Inuit dog team and radio
to Montreal to Miss Ella Wallace Jackson (Jackie), a
nurse from Nova Scotia whom he had met on the ship
that took him back to England in 1935. He invited her
to join him in the north. Jackie accepted, and the day
after she arrived they were married, using a ring made
from a brass fitting by the ship’s engineer. A few days
later they headed north in a whaleboat. For the next
eighteen months they conducted mapping and zoolog-
THE CANADIAN FIELD-NATURALIST
Vol. 118
Tom Manning photograph by Borg Mesch, Kiruna, north-
ern Sweden, 1932.
ical studies on the west coast of Baffin Island. Jackie
later published two books, /gloo for the Night, The
University of Toronto Press, 1946 and A Summer on
Hudson Bay, Hodder and Stoughton Ltd., 1949 about
their travels together. Although Jackie and Tom spent
many years together, the couple separated in the 1960s.
Tom often visited her in Ottawa where she still resides.
Late in 1939, Tom had a dream that caused him to
head south; he and Jackie arrived in Cape Dorset on 2
January 1940 to learn that World War II had been rag-
ing for four months. Anxious to join the war effort,
they discovered that the annual resupply ship — due
in August — could not get them to Montreal before
October. Tom decided they would make their own
way back, continuing around the Foxe Basin coast of
Baffin Island, hoping to reach Churchill by August. It
was 20 January 1941, however, before they reached
Churchill, after an epic journey of nearly 2500 miles
by boat and dog team, mapping as they went.
Tom received a commission in the Royal Canadian
Navy Voluntary Reserve, but was soon seconded to
the U.S. Army Engineers to provide advice on the sit-
CARTER: THOMAS HENRY MANNING
62)
Tom Manning and Reynold Bray (1911-1936) on expedition 21 October 1932. Photograph T. Dahill of Kiruna, northern
Sweden.
| ing, construction and operation of an airfield and
| weather stations on Southampton Island. He spent the
| rest of the war on defence-related geodetic surveys in
| the north, as well as the design and development of
| Arctic clothing and equipment for the armed services.
Tom served in the navy from 1941 to 1945, leaving
| with the rank of Lieutenant Commander.
Following the war, Tom’s services were sought by
the Defence Research Board, the Geodetic Survey, the
_ Geographical Branch, and other agencies of the Cana-
_ dian Government. Assignments included the exploration
_ of islands discovered in Foxe Basin by air photographs
in 1948, a survey of Banks Island, an oceanographic
survey in the Beaufort Sea, and many coastal surveys.
Throughout his travels, Tom continued to collect spec-
_imens of birds, mammals, plants and occasionally
_ insects. The National Museum of Canada was one of
the fortunate recipients of these valuable specimens.
_ In 1949 Tom introduced the seventeen year old Andrew
Macpherson to the Arctic. They became fast friends
and made several expeditions together, collaborating
on many reports of their findings. These journeys,
with their combined achievements in the fields of sci-
ence and exploration, are well known. Accounts of
Tom’s work have appeared over the last few years in
newspapers and journals around the world. In these
articles writers have paid extensive tribute to his work.
Many of his colleagues and acquaintances noticed that
Tom was as much at ease at a formal dinner as on the
snow-scoured rock of the Arctic Barrens. However, he
preferred the familiar landscape of the Barrens and
was able to make himself comfortable in surroundings
and circumstances that many civilized people could
not endure.
After leaving the North, in 1941, Tom lived briefly
in Montreal. Later, he and his wife bought a house in
Ottawa on Linden Terrace where they entertained many
of their northern friends. Tom started the Arctic Circle
Club, 14 November 1947, when the guests no longer
fitted around the huge oak dining-table that he had
made himself. He was an expert craftsman, making
cabinets for his house and building book shelves for his
huge library. He and Jackie also spent hours patiently
binding many of the collected volumes.
When I first met him in 1965, Tom had given up his
Arctic exploration and much of his scientific work. In
the tradition of his grandfather T. A. Manning (TAM),
he had become a farmer, an occupation which had
622
always interested him. However, Tom’s grandfather in
Northampton, had forsaken farming and instead, found-
ed a brewery continued by his son TEM. The prospect
of this confining tradition was one of the forces that
drove Tom to some of the most remote regions on the
planet. However, he made some reconciliation with
his heritage about 1960, by purchasing and working
over 500 acres of hayfield, pasture and woodlot in the
Merrickville countryside, some fifty km south of Otta-
wa. He, and his Arctic friends, built a cabin on the largest
portion of property which he also used for pasture. Tom
went on to renovate a stone house and rework the fer-
tile land into a self-sustaining farm with a huge and
immaculate vegetable garden, cattle, sheep, chickens
and geese.
Tom and I talked a great deal about his northern trips.
I finally convinced him that he should go back to his
scientific work, and that I would make an excellent assis-
tant! He cut back on the livestock and farming opera-
tions, making them manageable for summer and occa-
sional fieldwork. Our first trip was to western Canada
collecting birds, mammals and plants. We travelled in
a truck, which Tom had skillfully rebuilt as a home on
wheels, complete with woodstove. He said it remind-
ed him of caravan holidays as a child, and he always
took immense pleasure in its rugged simplicity — often
preferring to sleep in it, even when it was parked at
home.
My suggestion led to four decades of collaboration.
I usually acted as assistant, and collected and prepared
the birds with the hunting and skin preparation skills
that Tom had taught me. There was ample opportunity
for me to paint landscapes and wildlife studies on all
the expeditions we made; and Tom was always encour-
aging and supportive of my work. Occasionally I could
provide help with illustrations or maps for his scientific
papers. My first trip North with him was to Cape
Henrietta-Maria, tagging polar bears for the Canadian
Wildlife Service, under the direction of Dr. Charles
Jonkel. Although I saw no bears, I fell in love with the
land and, from then on, understood and shared Tom’s
passion for this fabulous country. I was soon to see
many bears, and we worked together from 1968 to 1973
on the Circumpolar Polar Bear Project.
During these travels, I had a firsthand chance to see
Tom’s unique skills. As always, he collected as many
types of specimens as he could, and kept extensive
field notes and descriptions of everything we encoun-
tered. Unlike many Arctic explorers of his time and
previously, Tom had a broader range of interests, and
documented everything he considered important. At
the time, I did not fully comprehend either Tom’s skills
or his decision-making process. Later, through field
experience, I began to understand the brilliance of his
mind and abilities.
On one occasion he piloted an open boat in dense fog
through seven miles (about 11 km) of the unforgiving
waters of James Bay, using dead reckoning and expe-
THE CANADIAN FIELD-NATURALIST
Vol. 118
=
Tom with beached hull of former 1949 expedition ship Nauya
behind him, Igloolik, 1983, Photograph by Brenda
Carter.
rience to arrive at South Twin Island, exactly on target.
On another occasion, attempting an open water cross-
ing on the Belcher Islands, we ran into a dangerous
pack-ice jam. This hazard was further compounded by
an early snowstorm and a five-foot (1.5 m) tide rip.
To stay meant being stranded. To leave meant facing
rough water in an overloaded canoe. Tom’s choice lit-
erally meant life or death. As usual, he made the right
decision — elegant in its simple, straightforward truth.
Despite the blinding snow he found a path through the
heavy waves and got us safely ashore. He always kept
part of his mind tuned to the essential core of any sit-
uation, a trait which was the quiet binding of his life.
From 1975 to 1986, Tom continued his collecting
trips by truck in the summer, spending winters writing
papers (a task he disliked) interspersed with his favour-
ite seasonal activities of gardening, cutting fence-posts
and filling the woodshed from his hardwood bush.
Renewing his interest in his boyhood pursuit of eggs,
he began to locate and weigh the eggs of different
species. He could often be seen in nearby swamps with
his odd, long-legged wooden table, a set of scales and
an umbrella to shade the eggs. We both enjoyed the
nest hunting and Tom became very interested in the
results of his weight loss experiments, but the statistics
proved daunting. I often wonder if a modern comput-
2004
er would have helped him with his puzzles. However,
his resulting papers were successful, and the most re-
| quested from scientists around the world.
In 1983 Tom and I made our last trip north together.
As we left Iqaluit for Igloolik, we had a poignant ex-
change. Looking down at the shorelines and islands that
| Tom had explored and mapped as a young man, | said
that I thought I had come into his life fifteen years too
late, and asked him what he felt as he looked down. He
| said that he thought he also had arrived in the North
fifteen years too late! At the age of seventy-five, he
| continued to dream of an unmapped place and an era
when the Arctic was truly beyond the reach of ordi-
nary travel.
On that trip, I noticed that Tom was walking badly;
_ and for the first time since I met him, I realized that I
| was able to outwalk him. This was startling and worry-
| ing and we soon learned that he had Parkinson’s dis-
| ease. However, he continued to work with great energy
| on the farm. When Parkinson’s disease forced him to
| give up his Arctic work, Tom donated his extensive col-
lection of rare Arctic books along with his field journals
and papers to the newly formed library in Iqaluit. He
| also made a very generous gift of one million dollars
| to the University of Cambridge towards their new lib-
| rary at the Scott Polar Research Institute. He is remem-
| bered there in a special room, the “Manning Archives”.
Then, following a broken hip, Tom had to have an
| operation. This trauma caused the Parkinson’s disease
| to accelerate. After 10 years of his usual bravery and
| independence, Tom became extremely ill. However, he
| exhibited the same stoic patience that he had while
| waiting out a blizzard. One of his last projects was to
| slowly dig two new flower beds. His dry humour never
| vanished, but the struggle became very difficult. In
| November of 1998, at the age of 86 he died. He was in
| hospital in Smiths Falls near his home, and remarkably
| at peace. He left many legacies behind, including a
| gift of $100 000 to the Ottawa Field Naturalist Club.
| The council decided that 80% of interest from this
bequest would go to assist authors with publication
charges for the Canadian Field-Naturalist, primarily
_ for northern papers.
Tom was a renowned Arctic explorer and zoologist
| whose life was characterized by a love of adventure,
_ self-reliance, and an ever-inquiring mind. In fact as
| Graham Rowley describes in his wonderful book, Cold
Comfort: My Love Affair with the Arctic, (McGill-—
Queen’s University Press, 1996) what Tom accom-
_ plished will never be equalled. He was also a wonder-
ful companion and brilliant teacher, showing by exam-
ple how to use intuition and logic to unravel a crisis and
how to see both facts and beauty in the natural world.
| He was quiet to the point of being taciturn, and slow to
| join in the mindless customs of society. But, his loy-
alty to his friends and to his family in England was
complete. Those who were privileged to know him well
miss him in many, many ways.
CARTER: THOMAS HENRY MANNING
623
Other tributes to Tom have appeared in several news-
paper articles as well as an obituary in Arctic 52 (1):
104-105 [March 1999] by Andrew H. Macpherson.
Tributes to his disciple Andrew Hall Macpherson (1932-
2002) and Manning’s role as his mentor have appeared
in The Daily Telegraph (London, England) 22 June
2002 and in Arctic 55(4): 403-406 (December 2002)
by Frank L. Miller.
Awards
1944 — Bruce Medal of the Scottish Geographical Society
and the Philosophical Society of Edinburgh.
1948 — Patron’s Medal of the Royal Geographical Society
1959 — Guggenheim Fellowship held for Arctic research
1974 — Officer of the Order of Canada
1977 — Massey Medal of the Royal Canadian Geographical
Society
1977 — Queen’s Jubilee Award
1979 — Honorary LLD from McMaster University
1992 —Doris Huestis Speirs Award in recognition of his
pioneering work on birds in the Canadian North
Positions in Scientific and Professional Societies
Fellow: Royal Geographical Society; Royal Canadian Geo-
graphical Society (also a term as Director) Arctic
Institute of North America (also Executive Director
1955-1956).
Member: American Ornithological Union; Wilson Ornitho-
logical Club; Cooper Ornithological Club; Wildlife
Society; American Society of Mammalogists; Society
for American Archaeology. Founder: Arctic Circle
Club; 1947 (also Secretary 1948-1950)
Research Associate: Canadian Museum of Nature (1970-1990)
Bibliography
Publications
Manning, T. H. 1936. Some notes on Southampton Island.
Geographical Journal 88: 232-242.
Manning, T. H. 1942. Remarks on the physiography, Eskimo
and mammals of Southampton Island. Canadian Geograph-
ical Journal 25: 17-35.
Manning, T. H. 1942. Notes on some fish of the eastern
Canadian Arctic. Canadian Field-Naturalist 56: 128-129.
Manning, T. H. 1942. Blue and Lesser Snow geese on South-
ampton and Baffin Islands. Auk 59: 158-175.
Manning, T. H. 1943. Notes on the coastal district of the east-
ern barren grounds and Melville Peninsula from Igloolik to
Caper Fullerton. Canadian Geographical Journal 26: 84-105.
Manning, T. H. 1943. The Foxe Basin coasts of Baffin Island.
Geographical Journal 101(5, 6): 225-251.
Manning, T. H. 1943. Notes on the mammals of south and
central west Baffin Island. Journal of Mammalogy 24:
47-59.
Manning, T. H. 1943. Notes on the birds of Southampton
Island, Baffin Island and Melville Peninsula. Auk 60: 504-
536. [prepared partially from the notes of R. J. O. Bray,
who died on the expedition]
Manning, T. H. 1944. Hunting implements and methods of
the present day Eskimos of north-west Hudson Bay, Mel-
ville Peninsula, and south-west Baffin Island. Geographi-
cal Journal 103: 137-152.
Manning, T. H., and E. W. Manning. 1944. The preparation
of skins and clothing in the eastern Canadian Arctic. Polar
Record 28: 156-169.
624
Manning, T. H. 1944. Lesser Snow and Blue Geese on South-
ampton Island. Auk 61: 146-147.
Manning, T. H. 1946. Ruins of Eskimo stone houses on the
east side of Hudson Bay. American Antiquity 11(3) 201-
202.
Manning, T. H. 1946. Bird and mammal notes from the east
side of Hudson Bay. Canadian Field-Naturalist 60: 71-85.
Manning, T. H. 1947. Explorations on the east coast of Hud-
son Bay. Geographical Journal 109: 58-75.
Manning, T. H. 1948. Eskimo stone house ruins on the east
side of Hudson Bay: A correction. American Antiquity 13
(3).
Manning, T. H. 1948. Pipestems of the Caribou Eskimos.
American Anthropologist 50: 162-163.
Manning, T. H. 1948. Notes on the country, birds and mam-
mals west of Hudson Bay between Reindeer and Baker
lakes. Canadian Field-Naturalist 62: 1-28.
Manning, T. H. 1949. The birds of northwestern Ungava.
Pages 155-224 in A Summer on Hudson Bay by Mrs. T.
H. Manning. Hodden and Stoughton Ltd.
Manning, T. H. 1949. The varying lemming in captivity in
Ottawa. Arctic Circular 3: 20-21.
Manning, T. H. 1950. Tidal observations in Arctic waters:
Notes on the tides along the south Hudson Bay and west
James Bay coasts. Arctic 3: 95-100.
Manning, T H. 1950. Eskimo stone houses in Foxe Basin.
Arctic 3: 108-112.
Manning, T. H. 1950. A mixed Cape Dorset-Thule site on
Smith Island, east Hudson Bay. Annual Report of the
National Museum of Canada 1949-50, Bulletin 123: 64-71.
Manning, T. H., et al. 1950. The voyage of C. G. M. V. Nauja
to Foxe Basin in 1949. 158 pages, plus maps, photographs.
Manning, T. H. 1951. Remarks on the tides and driftwood
strand lines along the east coast of James Bay. Arctic 4:
122-130.
Manning, T. H. 1952. Birds of the west James Bay and south-
erm Hudson Bay coasts. National Museum of Canada Bul-
letin 125: 1-114.
Manning, T. H., and D. F. Coats. 1952. Notes on the birds
of some James Bay islands. Annual Report of the National
Museum Canada 1950-51, Bulletin 126: 195-207.
Manning, T. H., and A. H. Macpherson. 1952. Birds of the
east James Bay coast between Long Point and Cape
Jones. Canadian Field-Naturalist 66: 1-35.
Manning, T. H. 1953. Narrative of an unsuccessful attempt
to circumnavigate Banks Island by canoe in 1952. Arctic
6: 170-197.
Manning, T. H. 1953. Notes on the fish of Banks Island.
Arctic 6: 276-277.
Manning, T. H. 1954. Remarks on the reproduction, sex ratio,
and life expectancy of the varying lemming, Dicrostonyx
groenlandicus, in nature and captivity. Arctic 7: 36-48.
Manning, T. H. 1956. The northern red-backed mouse, Cleth-
rionomys rutilus (Pallas), in Canada. National Museum of
Canada Bulletin 144: 1-67.
Manning, T. H. 1956. Narrative of a second Defence Research
Board expedition to Banks Island, with notes on the coun-
try and its history. Arctic 9(1, 2): 1-77.
Manning, T. H., E. Q. Hohn, and A. H. Macpherson. 1956.
The birds of Banks Island. National Museum of Canada
Bulletin 143: 1-144.
Manning, T. H., and A. H. Macpherson. 1958. The mammals
of Banks Island. Arctic Institute of North America Tech-
nical Paper 2: | -74.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Macpherson, A. H., and T. H. Manning. 1959. The birds and
mammals of Adelaide Peninsula, N.W.T. National Museum
of Canada Bulletin 161: 1-63.
Manning, T. H. 1960. The relationship of the Peary and bar-
ren ground caribou. Arctic Institute of North America Tech-
nical Paper 4: 1-52.
Manning, T. H. 1961. Comments on “Carnivorous Walrus
and Some Arctic Zoonoses”. Arctic 14(1): 76-77.
Manning, T. H., and A. H. Macpherson. 1961. A biological
investigation of Prince of Wales Island, N.W.T. Transactions
of the Royal Canadian Institute 33: 116-239.
Macpherson, A. H., and T. H. Manning 1961. Pack dogs in
the Canadian Arctic. Polar Record 10: 509.
Manning, T. H. 1964. Age determination in the polar bear,
Ursus maritimus Phipps. Canadian Wildlife Service Occa-
sional Paper 5: 1-12.
Manning, T. H. 1964 Geographical and Sexual Variation in
the Long-tailed Jaeger, Stercorarius longicaudus Vieillot.
Biological Papers of the University of Alaska. (7): 1-16.
Manning, T. H. 1969 Wreckage on Banks Island. Beaver
Autumn: 21.
Manning, T. H. 1971. Geographical variation in the polar bear
Ursus maritimus Phipps. Canadian Wildlife Service Report
Series 13: 1-26.
Manning ,T. H. 1974. Variations in the skull of the bearded
seal. Biological Papers of the University of Alaska (16).
Manning, T. H. 1976. Birds and mammals of the Belcher,
Sleeper, Ottawa and King George islands, Northwest Ter-
ritories. Canadian Wildlife Service Occasional Papers 28:
1-42, maps, tables.
Morrison, R. I. G., T. H. Manning, and J. A. Hager. 1976.
Breeding of the Marbled Godwit, Limosa Fedoa, in James
Bay. Canadian Field-Naturalist 90: 487-490.
Morrison, R. I. G., and T. H. Manning 1976. First breed-
ing records of Wilson’s Phalarope for James Bay, Ontario.
Auk 93(3): 656-657.
Manning, T. H., and B. Carter. 1977. Incidence of runt eggs
in the Canada Goose and Semipalmated Sandpiper. Wilson
Bulletin 89: 469.
Manning, T. H. 1978. Measurements and weights of eggs
of the Canada Goose, Branta canadensis, analyzed and
compared with those of other species. Canadian Journal
of Zoology 56: 676-687.
Manning, T. H. 1979. Density and volume corrections of
eggs of seven passerine birds. Auk 96: 207-211.
Manning, T. H. 1981. Analysis of weight lost by eggs of ele-
ven species of birds during incubation. Canadian Field-
Naturalist 95: 63-68.
Manning, T. H. 1981 Birds of the Twin Islands, James Bay,
N.W.T., Canada. National Museum of Natural Sciences,
Syllogeus 30: 1-50.
Manning, T. H. 1982. Daily Measurements of Variation in
weight loss of eggs of seven Passerine Species before and
during natural incubation. National Research Council of
Canada 60: 3143-3149.
Barker, A. J., J. L. Eger, R. L. Peterson, and T. H. Manning.
1983. Geographic variations and taxonomy of Arctic
Hares. Acta Zoologica Fennica 174: 45-48.
Unpublished Reports
Manning, T. H. 1944. Descriptive report to the Geodetic
Service of Canada on a survey of the east Hudson Bay
coast. 64 pages plus maps, photographs.
2004
' Manning, T. H. 1945. Report on Exercise Lemming to the
Geodetic Service of Canada. 21 pages plus 4 pages, plus
photographs.
|Manning, T. H. 1945. Descriptive report to the Geodetic
Service of Canada on a survey of northern Manitoba and
southeast Keewatin. 54 pages, plus photographs.
Manning, T. H. 1945. Technical report to the Geodetic Ser-
vice of Canada on a survey of northern Manitoba and
southeast Keewatin. 179 pages, plus maps, photographs.
Manning, T. H. 1946. Report to the Geodetic Service of
Canada on Exercise Muskox and on the Cambridge Bay
___ observation station. 25 pages, plus photographs.
| Manning, T. H. 1946. Descriptive report to the Geodetic
Service of Canada on a survey of Ungava, east Hudson
Bay, and the south coast of Hudson Strait. 133 plus 49 pages,
photographs and maps.
| Manning, T. H. 1946. Technical report to the Geodetic Ser-
vice of Canada on a survey of Ungava, east Hudson Bay,
| and the south coast of Hudson Strait. 90 pages, maps.
| Manning, T. H. 1947. Preliminary report on a background
| study of the caribou, Rangifer caribou caribou (Gmelin) and
Rangifer arcticus caboti Allen of the Labrador Peninsula
and the Province of Quebec north of the St. Lawrence.
(Mimeo).
| Manning, T. H. 1947. Descriptive report to the Geodetic Ser-
vice of Canada on a survey of the west James Bay and
southern Hudson Bay coasts. 166 pages, plus maps, pho-
tographs.
| Manning, T. H. 1947. Technical report to the Geodetic Ser-
vice of Canada on a survey of the west James Bay and south-
ern Hudson Bay coasts. 64 pages, plus maps.
| Manning, T. H. 1948-49. Reports to Defence Research Board.
1. South coast of Hudson Bay, 147 pages, plus photographs,
maps, charts, etc. II. West side of James Bay, 185 pages, plus
photographs, etc. FV. East coast of James Bay, 295 pages,
plus photographs, etc.
Professional Experience
| 1931 (summer) — Traveled in Iceland and Faro Islands.
1932-33 (winter) — Traveled through Norway, Sweden, Fin-
land, and Russia (Bergen to Murmansk) on foot and
with reindeer.
| 1933-35 — Mapped Southampton Island and also studied
and made collections of birds and mammals.
1936-41 — Leader, surveyor and ornithologist on the British
Canadian — Arctic Expedition, working in Southamp-
ton and Baffin islands and Repulse Bay areas: includ-
ed two years in Foxe Basin which was circumnavi-
| gated by whale boat.
1941-45 — Royal Canadian Navy. Seconded as an advisor to
the U.S. Army in connection with the sighting and con-
struction of the air field and establishment by tractor
train of outlying weather stations on Southampton
| Island; and later to the Geodetic Service (Canada) to
| fix ground controls for air photographic survey of
northern Canada (until 1947).
| 1944 — Geodetic work in Ungava by aircraft and Peterhead
| boat.
j 1945 — Geodetic work in west Hudson Bay by aircraft.
| 1946 — Geodetic work in Ungava, east Hudson Bay and west
Hudson Strait by aircraft and Peterhead boat.
_ 1947 — Geodetic work by canoe along the west James Bay
and southern Hudson Bay coasts.
CARTER: THOMAS HENRY MANNING
625
1948 — Consultant to Defence Research Board.
1949 — Leader, Geographical Bureau’s expedition in C. G.
M. V. Nauja to “new” islands in Foxe Basin: includ-
ed circumnavigation of Foxe Basin. Soundings and
tidal observations taken.
1950 — Canoe journey to collect birds and mammals along
east James Bay.
1951 — Leader, Defence Research Board expedition to the
Beaufort Sea and Master C.G.M.V Cancolim (includ-
ed “circumnavigation” of Alaska). About 4000 miles
of soundings taken.
1952 — Leader, Defence Research Board expedition to Banks
Island: included attempted circumnavigation of the
Island by canoe.
1953 — Completion of circumnavigation of Banks Island.
1954 — Worked up results of Banks Island Expedition under
contract with Defence Research Board, and others.
1960 (June to July) — West Coast of North America with
Diana Rowley
1967 — Introduction of caribou from Coats Island to South-
ampton Island for Canadian Wildlife Service.
1968 (June 14 — August) — Western Canada collecting by
truck assisted by Brenda and Charlotte Carter; (Sep-
tember) — Cape Henrietta-Maria with Brenda Carter,
Dick Russell and Chuck Jonkel for Canadian Wildlife
Service.
1969 — Alaska collecting by truck assisted by Z. E. Ellshoff
1970 (July 21 — August) — South Twin Islands, polar bear
trapping with Brenda Carter for Canadian Wildlife
Service. :
1971 (May 2 — September) — Belcher Islands, Sleeper Islands
and Ottawa Islands with Brenda Carter for Canadian
Wildlife Service.
1972 (May — June) — UK and Norway measuring bear
skulls with Charlotte Carter; (September 10 — Octo-
ber 18) -North Twin Island, polar bear trapping with
Brenda Carter for Canadian Wildlife Service.
1973 (March 22 — April 17) — Fort George and Belcher
Islands, helicopter polar bear tagging with Brenda
Carter for Canadian Wildlife Service; (May 2 — Au-
gust 1) — North Twin Island, polar bear work with
Brenda Carter for Canadian Wildlife Service; (August
13 — September 12) — Foxe Basin helicopter work
with Brenda Carter for Canadian Wildlife Service.
1975 (May 15 — July 16) — Collecting at North Point, James
Bay.
1977 — Yukon collecting by truck and making a floral and
faunal inventory of the Dempster Highway assisted
by Jan Rowell and Wendy Earl (who departed Daw-
son City). Robert Porsild and his wife were visited.
1980 — New Brunswick collecting by truck.
1982 — Manitoulin Island collecting by truck assisted by Doug
Perkins
1983 — Igloolic Wildlife description. Advisor to adult Inuit
for Igloolic Education Council.
1983 — USA (Mississippi, Louisiana, Nevada, Utah and
Texas) collecting by truck assited by S. C. Tuutz.
1986 — Yukon collecting by truck (age 77) assisted by Brid-
get Ryan.
Most of the specimens collected on these trips were sold either
to the National Museums of Canada or Carleton
University.
A Tribute to Victor Kent Prest 1913-2003
A. S. DyKE!. D. A. Hopcson!, E. L. BouSFIELD?, and R. E. BEDFORD?
: Terrain Sciences Division, Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario K1A OE8 Canada
~ 301-540 Dallas Road, Victoria, British Columbia V8V 4X9 Canada
; 524 Penhill Avenue, Ottawa, Ontario K1G 0V6 Canada
Dyke, A. S., D. A. Hodgson, E. L. Bousfield, and R. E. Bedford. 2004. A Tribute to Victor Kent Prest 1913-2003. Canadian
Field-Naturalist 118(4): 626-629.
With the death of Dr. Victor Kent Prest on 2003 Sep-
tember 26, Canada lost one of its most distinguished,
best-known, and most influential Quaternary geolo-
gists. Vic was active as a leader of Canadian Quater-
nary science for a remarkably long time and he posi-
tively influenced the careers of almost everyone else
in the field in this country as well as his many friends
abroad. His work became basic to discoveries by other
scientists in related fields such as plant and animal
biogeography, both terrestrial and aquatic*>°. He came
to personify the Quaternary Geology of Canada both
domestically and internationally. This identity arose
from his unstinting and deep interest in the subject,
his long view of the evolution of ideas, his intimate
knowledge of the ever-growing knowledge base, and
especially the very genuine interest he took in the work
of all others. Tentative, junior researchers and graduate
students always met with as much respect and encour-
agement as did his senior colleagues and Vic often took
the time to send notes of encouragement and compli-
ment.
Victor K. Prest was born in Edmonton Alberta, 2
April 1913, the only child of John (Jack) Prest and
Elizabeth Buckley (Prest). His early education was
obtained at the MacKay Avenue School in Edmonton.
In 1925 the family moved to Toronto for a brief period,
and relocated in London, Ontario, where Vic completed
his early schooling at Tecumseh Public School and
London South Collegiate High School. In 1930 the
Prests moved to Winnipeg where Victor completed his
secondary education at Kelvin High School. Unreal-
ized by Vic, his future wife Patricia Horder was also
attending Kelvin, in the same grade, but in a different
classroom. Her father, a Canadian Pacific Railway offi-
cial, had been transferred from Montreal to Winnipeg
in 1926. Vic received his B. Sc. (Honours) from the
University of Manitoba in 1935 and his M. Sc. a year
later. Growing stronger during these university days
was his friendship with Patricia Horder who was active
in music, drama, and art, and in the Canadian Girl
Guide Association.
Vic worked as a summer assistant for the Manito-
ba Mines Branch in 1934 and the Geological survey
of Canada in 1935 and 1936. While registered for
Ph.D. studies at the University of Toronto, Vic was
Party Chief, Ontario Department of Mines, from 1937-
1940, mainly mapping bedrock outcrops in Northern
Ontario. In 1941 Vic received his Ph.D. degree at “Tor-
onto” where he also served as an assistant in both the
Geology Department and the Royal Ontario Museum
and later as Lecturer. The newly minted Dr. Prest
joined the International Nickel Company as a geolo-
gist for a year (1941-1942).
Vic and Pat were married in Toronto in 1942 and
moved immediately to Harbour Grace, Newfoundland,
where Vic served with the RCNVR from 1942-1945.
Their first child, Sherron (Sherry) Gail was born there
in 1944. Following the surrender of Nazi Germany in
early May, 1945, Lieutenant Prest was a member of the
naval party accepting the surrender of submarine U190
in St. John’s Harbour.
During the next five years Vic was a permanent staff
member of the Ontario Department of Mines, based in
Toronto, where his son Wayne Horder Prest was born
in 1946. In 1950, he transferred to the Geological Sur-
vey of Canada in Ottawa. Vic served as Chief of the
Pleistocene Engineering and Groundwater Section,
first in a third-floor office of the Victoria Memorial
Museum building and, following its completion in
1960, in the newly constructed Geological Survey
building on Booth Street. Vic formally retired from
government service in 1979, but maintained a con-
sultantship office at the Booth St. building until very
recently.
Dr. Victor K. Prest is probably best known because
of the Glacial Map of Canada (Prest et al. 1968), a
work of such veracity that it has yet to be superceded
for the country as a whole. This map followed an ear-
lier version initiated by J. Tuzo Wilson, to which Vic
contributed as co-compiler (Wilson et al. 1959). The
1968 Glacial Map was followed by the beautiful blue-
shaded “pancake map” depicting the Retreat of Wis-
consin and Recent Ice in North America (Prest 1969),
and his masterful Quaternary Geology chapter in the
Geology of Canada volume (Prest 1970). That trilogy
was the masterpiece of a generation, which adorned
many an academic hallway and classroom. Its impact
places it among the most outstanding contributions of
the Geological Survey of Canada (GSC) and fixes it as
its premier Quaternary contribution. It was the most
626
2004
DYKE, HODGSON, BOUSFIELD, and BEDFORD: VICTOR KENT PREST
627
VICTOR KENT PREST
cogent, persuasive, and attractively illustrated synthesis
available and it has served as the baseline for almost
everything else that has followed.
As a great builder of Quaternary science in Canada,
Vic had wide knowledge of geological and other sci-
_ ences. He resumed mapping the Precambrian geology
of northern Ontario for ODM (1945-1950) where he
authored more than 30 maps and annual reports. He
was one of the first to combine Quaternary and bedrock
mapping with the release of his map of Red Lake-
Lansdowne House. His first Quaternary publication was
the Pleistocene geology of the Vermillion River system
with special reference to placer gold (Prest 1949).
Vic’s early Pleistocene colleagues at GSC includ-
ed Jack Armstrong, Wes Blake, Jr., Bruce Craig, Bob
Fulton, John Fyles, Nelson Gadd, Eric Henderson,
Owen Hughes, Bert Lee, and Archie Stalker, all of
whom were to become major regional authorities, and
Jaan Terasmae and Bob Mott, leaders in the develop-
ment of Quaternary paleoecology in Canada. Addi-
tion of his academic and provincial geological survey
friends, Bill Matthews (University of British Colum-
bia), Earl Christiansen (Saskatchewan), Alexis Drei-
manis (University of Western Ontario), Con Gravenor
(University of Windsor), Paul Karrow (Waterloo Uni-
versity), Pierre LaSalle (Quebec), and John Elson
(McGill University) largely completes the Prest cohort
of Canadian Quaternary geologists.
Although he departed senior management for full-
time research in 1964, even those who joined the Sur-
628
vey later, and many in outside agencies, identified the
Quaternary group with Vic Prest more than with any-
one else. Vic became a sort of mentor-at-large, with
great moral authority and prestige, and engendered
pride in the work of others. By building Quaternary
science at the Survey and by mentoring and infor-
mally supervising graduate students, Vic profoundly
contributed to the Canadian Quaternary community.
Vic was an enthusiastic participant in numerous field
excursions in southern Canada, the northern USA,
Alaska, and internationally. His GSC fieldwork took
him on a High Arctic voyage that reached Ellesmere
Island (Prest 1958), mapping projects in Ontario (Prest
1963), Quebec (Prest 1966; Prest and Hode-Keyser
1977) and the Maritimes. He had a special passion for
the Maritimes, where his map of Prince Edward Island
(Prest 1973) remains seminal, and where, with his pro-
tégé Douglas Grant, he formulated the concept of an
Appalachian Ice Complex (Prest and Grant 1969; Prest
et al. 1972; Prest 1977) to encapsulate the style of
regional glaciation, as distinct from Laurentide glacia-
tion. This model is still favoured by regional geolo-
gists. The Magdalen Islands in the Gulf of St. Law-
rence long held his interest, because of the perplexing
lack of direct evidence of Late Wisconsin glaciation
and its record of older events (Prest et al. 1976). This
evidence led him to portray on his ice recession map
what Doug Grant termed “Prest’s Problematical Pleis-
tocene Prong”, a reference to the glaciological improb-
ability of leaving the Magdalen Islands ice free while
allowing ice to extend to the edge of the Continental
Shelf. The portrayal revealed Vic’s preference for
field evidence over theory.
Vic formally retired from GSC in 1978, and formed
Veekay Consultants (1978-1994) to receive Ontario
Geological Survey (OGS) surficial mapping contracts
in northwestern Ontario and a Department of Indian
Affairs and Northern Development contract to work
in the Bebensee Lake area (Prest 1985). He continued
fieldwork into his seventies, including long traverses
into dense bush around the famous Red Lake gold
mining camp. This work yielded a series of detailed
maps (e.g., Prest 1980) that formed the basis for recent
drift prospecting programs. His major syntheses includ-
ed Canada’s Heritage of Glacial Features (Prest 1983),
the Late Wisconsin Glacier Complex paper and map
(Prest 1984), a synthesis of glacial lake history in the
Lake Ontario basin with Ernie Muller (Muller and
Prest 1985), and maps of North American paleogeog-
raphy (Dyke and Prest 1987). His two final publications
dealt with the history of interpretation of the Laurentide
Ice Sheet (Prest 1990) and a more specific passion, the
long-distance dispersal of the distinctive erratics that
he termed “omarsi” from the central part of the ice sheet
(Prest et al. 2000).
Vic was an accomplished athlete and maintained a
life-long interest in several sports. During the half cen-
tury of his residence in Ottawa, Vic’s love of tennis
THE CANADIAN FIELD-NATURALIST
Vol. 118
became super-seded by a passionate devotion to curl-
ing. He was a charter member of the City View Curl-
ing Club, founded in 1957, and President the follow-
ing year. Over the years, he won many curling bonspiels
both in men’s and mixed rink events, and was ever a
formidable shot-maker and curling strategist. He was
Honorary Governor General’s Curling Club President
(1972), Canadian Branch (Royal Caledonia Curling
Club), Council of Management (1978-1980) and Life
Member (1986). With support from the Ottawa Val-
ley Curling Association, Vic introduced Junior Curl-
ing in Eastern Ontario in 1975, and co-ordinated play
with the Canadian Branch in Quebec. He also intro-
duced “Little Rock” curling in 1983, and organized
Junior and Little Rock bonspiels for the OVCA over
a period of ten years. After more than 50 continuous
years of winter curling, he “pushed” his last rock at
age 89.
Vic’s professional career accomplishments received
due recognition in the form of the Johnston Medal
from the Canadian Quaternary Association (the first
awarded), the Gold Medal from the Royal Canadian
Geographical Society, the Kirk Bryan and the Distin-
guished Career Awards from the Quaternary Geology
and Geomorphology Division of the Geological Society
of America (1993), election as a Fellow to join the
distinguished scientists of the Royal Society of Cana-
da, and election as Honorary Member of the Interna-
tional Union for Quaternary Research.
Vic and Pat enjoyed more than sixty years of mutual
accomplishment. He loved the out-of-doors and experi-
enced great pleasure whenever he had a chance to stand
on a good piece of Precambrian bedrock. Vic was also
very generous in his support of charitable organiza-
tions, and agencies promoting wildlife conservation
and the natural sciences. He will be greatly missed by
his family, and by his many friends and scientific col-
leagues.
References
Dyke, A. S., and V. K. Prest. 1987. The Late Wisconsin and
Holocene history of the Laurentide Ice Sheet. Géogra-
phie physique et Quaternaire 41: 247-264.
Muller, E. H., and V. K. Prest. 1985. Glacial lakes in the
Ontario basin. Edited by P. F. Karrow, and P. E. Calkin in
Quaternary Evolution of the Great Lakes. Geological
Association of Canada, Special Paper 30: 213-229.
Prest, V. K. 1939. Geology of the Keezhik-Miminiska Lake
area. Ontario Department of Mines, Annual Report 48,
Part 6, 8 pages.
Prest, V. K. 1941. The Precambrian of the Miminiska-Port
Hope area. Unpublished Ph.D. thesis, University of Toronto,
93 pages.
Prest, V. K. 1949. The Pleistocene geology of the Vermillion
River system near Capreol, District of Sudbury, Ontario
(with special reference to placer gold), Ontario Department
of Mines Open File.
Prest, V. K. 1952. Notes on the geology of parts of Ellesmere
and Devon islands. Geological Survey of Canada, Paper
52-32, 15 pages.
2004
| Prest, V. K. 1963. The Red Lake-Lansdowne House area,
northwestern Ontario — Surficial geology. Geological Sur-
vey of Canada, Paper 63-6, 23 pages.
Prest, V. K. 1966. Glacial studies, northeastern Ontario and
northwestern Quebec. In Report of Activities May to Octo-
ber 1965. Geological Survey of Canada, Paper 66-1: 202-
203.
Prest, V. K. 1969. Retreat of Wisconsin and Recent ice in
North America. Geological Survey of Canada, Map 1257A,
scale 1:5 000 000.
Prest, V. K. 1970. Quaternary geology of Canada. Edited by
R. J. W. Douglas in Geology and Economic Minerals of
Canada. Economic Geology Series (1): 676-764.
Prest, V. K. 1973. Surficial deposits of Prince Edward
Island. Geological Survey of Canada, Map 1366A, scale
1:253 444.
Prest, V. K. 1977. General stratigraphic framework of the Qua-
ternary in eastern Canada. Géographie physique et Qua-
ternaire 31: 7-14.
| Prest, V. K. 1980. Quaternary geology of the Red Lake area,
District of Kenora. Ontario Geological Survey, Preliminary
Map 2484, scale 1:50 000.
Prest, V. K. 1983. Canada’s heritage of glacial features. Geo-
logical Survey of Canada, Miscellaneous Report 28: 119
pages.
Prest, V. K. 1984. Late Wisconsinan Glacier Complex. Edited
by R. J. Fulton, in Quaternary Stratigraphy of Canada —
A Canadian contribution to IGCP Project 24. Geological
Survey of Canada, Paper 84-10: 21-38.
Prest, V. K. 1984. Late Wisconsinan Glacier Complex. Geo-
| logical Survey of Canada, Map 1584A, 1:7 500 000.
Prest, V. K. 1985. Glacial geology of the Bebensee Lake map-
area (NTS 86M), Great Bear Lake region, Northwest Ter-
ritories. Edited by J. A. Brophy in Contributions to the
Geology of the Northwest Territories, 63-70.
Prest, V. K. 1990. Laurentide ice-flow patterns: a historical
review, and implications of the dispersal of Belcher Islands
erratics. Géographie physique et Quaternaire 44: 113-136.
Prest, V. K., and J. A. Donaldson. 1963. Bedrock-drift dis-
tribution, Red Lake-Lansdowne House area, Ontario. Geo-
logical Survey of Canada, Map 4-1963.
Prest, V. K., J. A. Donaldson, and H. D. Moores. 2000.
The Omar story: The role of Omars in assessing glacial his-
DYKE, HODGSON, BOUSFIELD, and BEDFORD: VICTOR KENT PRES1
tory of west-central North America. Géographie physique
et Quaternaire 54: 257-270.
Prest, V. K., and D. R. Grant. 1969. Retreat of the last ice
sheet from the Maritime Provinces — Gulf of St. Lawrence
region. Geological Survey of Canada, Paper 69-33, 15 pages.
Prest, V. K., D. R. Grant, H. W. Borns, I. A. Brookes, R. H.
MacNeill, J. G. Ogden, J. F. Jones, T. W. Hennigar, and
M. L. Parsons. 1972. Quaternary geology, geo-morphology
and hydrogeology of the Atlantic Provinces. XXIV Inter-
national Geological Congress, Excursion Guidebook A61-
C61, 79 pages.
Prest, V. K., D. R. Grant, and V. Rampton. 1968. Glacial
Map of Canada. Geological Survey of Canada, Map 1253A,
scale 1:5 000 000.
Prest, V. K., and J. Hode-Keyser. 1977. Geology and engi-
neering characteristics of surficial deposits, Montreal Island
and vicinity, Quebec. Geological Survey of Canada, Paper
75-29, 29 pages.
Prest, V. K., J. Terasmae, J. V. Matthews, and S. Lichti-
Federovich. 1976. Late-Quaternary history of Magdalen
Islands, Quebec. Maritime Sediments, 12(2): 39-59.
Wilson, J. T., G. Falconer, W. H. Mathews, and V. K.
Prest. 1959. Glacial Map of Canada. Geological Associ-
ation of Canada, scale 1:3 801 600.
Examples of research publications in periph-
eral fields of science for which the work of V.
K. Prest was basic:
Bousfield, E. L., and M. L. H. Thomas 1975. Postglacial
changes in distribution of littoral marine invertebrates in
the Canadian Atlantic Region. Proceedings of the Nova Sco-
tia Institute of Science 27, Supplement 3: 37-42, 8 figures.
Dadswell, M. J. 1974. Distribution, ecology, and postglacial
dispersal of certain crustaceans and fishes in eastern North
America. National Museum of Canada Publications in
Zoology 11: 110 pages, 20 maps.
Pielou, E. C. 1991. After the Ice age. University Chicago Press.
Chicago. 366 pages.
Acknowledgments
For providing biographical material, photographs, and per-
sonal recollections, the authors are especially grateful to
Patricia Prest (wife) and Sherry Armstrong (daughter).
Book Reviews
ZOOLOGY
Birds of Australia (Seventh edition)
By Ken Simpson and Nicolas Day. 2004. Princeton Univer-
sity Press, 41 William Street, Princeton, New Jersey,
USA, 08540-5237. iv + 92 pages, U.S.$39.50.
When Simpson and Day’s first edition appeared (as
Birds of Australia, later changed to The Princeton Field
Guide to the Birds of Australia) it meant Australia had
a bird guide that was equivalent to North America’s
National Geographic guide (Dunn 2002). It provided
complete coverage of Australian birds in color, with
accompanying text and range maps. Curiously the print-
ing was, and still is, poorer than that of the National
Geographic.
As with the original this book covers all six states
(including Tasmania), three territories and 10 island
territories. The new edition has a double page map of
the continent, but does not show the island territories.
This revised edition has undergone significant
changes from the original. Although much of the con-
tent is the same it has been reorganized. More impor-
tant 19 of the plates have been repainted (actually I
counted 24 plates with changes). The illustrations now
include more plumage variations than before, such as
female, juvenile, winter and different races. In addition
to over 2000 colour images there are almost 1000 sup-
plementary black-and-white drawings. One noticeable
difference is that the illustration of the dead White-
throated Needletail has been replaced with a represen-
The Bird Almanac
By David M. Bird. 2004 Key Porter Books Ltd. 70 The Espla-
nade, Toronto, Ontario, MSE 1R2 Canada. 460 pages, Can
$24.95 Paper.
Within this book is a massive amount of bird-related
information! This review could actually end right here.
However, I will elaborate somewhat.
Information in this book is presented in three ways:
line drawings (restricted to the anatomy chapter), tables/
lists as well as glossary-style entries. These are all ap-
propriate and lead the reader to finding information
rather quickly. There is both birding information and
ornithological information (and a massive amount of
overlap which is shared by both). A glossary of over
20 pages contains over 1000 terms — surely the word
you're looking for must be there!
There are simply too many categories of information
to give more than a smattering of examples here. Both
traditional and genetically-based classifications of bird
families are given, followed by the massive list of all
tation of a live, flying one. Some extra space was gen-
erated on the main plates by moving the vagrants to a
separate section. This is a better method of dealing
with these rare birds.
The introductory material has been reorganized to
give a more logical flow. Two small sections — on DNA
and prehistoric birds — have been replaced by more
pertinent material. All the range maps have been up-
dated. The result is the book is slightly smaller than
the original, so the book remains portable in the field.
Within the field information I noted only a few points
I would question. The authors tend to lump species that
more recently have been separated. These include the
Royal and Macaroni Penguins, the Lesser and Greater
Snow Petrels and the Yellow and Crimson Rosellas. The
Paradise Parrot is still included, despite not having
been seen since 1927.
This revised edition, with the original, simpler title of
Birds of Australia and the expansion of information,
makes this field guide a more useful book than the
original.
Reference
'Dunn, Jon L. 2002. National Geographic Field Guide to the Birds of
North America: 4'" edition Revised and Updated. National Geo-
graphic Society, Washington, D.C.
Roy JOHN
2193 Emard Crescent, Beacon Hill North, Ottawa, Ontario
K1J 6K5 Canada
known bird species. Significant people are listed in sev-
eral tables, ornithological award recipients, world-class
listers, Taverner Cup winners, bird artists and more.
Bird watching clubs, ornithological societies, magazines
and journals are listed from sources around the planet.
To compare this book with Leahy’s The Birdwatch-
er’s Companion, a recent tome of similar intent, would
be to have The Bird Almanac come on top. The former
is essentially all in dictionary format, and therefore
lacks the comparative ease (or the ease of comparisons)
of the thematically-organized, tabular format in Alma-
nac. There are more in-depth definitions and descrip-
tions in Companion (it is also a much bigger book),
and the bibliography is better- organized, but I believe
birders will much more enjoy flipping through Almanac.
RANDY LAUFF
Department of Biology, St. Francis Xavier University, Anti-
gonish, Nova Scotia B2G 2W5 Canada
630
2004
Book REVIEWS
63]
Handbook of Birds of the World: Volume 9 Cotingas to Pipits and Wagtails
Edited by Josep del Hoyo, Andrew Elhott and David Christie.
2004. Lynx Edicions, Barcelona, Spain. 850 pages, illus-
trated. Cloth $195 US.
This volume of the Handbook of Birds of the World
covers 819 species, including Cotingas, Manakins,
Tyrant-flycatchers (over 50 % of the book), New Zea-
land Wrens, Scrub-birds, Lyrebirds, Larks, Swallows
and Martins and Pipits and Wagtails. With the publi-
cation of this volume Handbook has now covered 60%
of the world’s 197 families of birds. Under the current
schedule Volume 10 will be published in 2005 and the
final volume, 16, is due in 2011.
It has become very difficult to review these books.
Most reviewers, including myself, have already praised
the content, the artwork, the scholarship, the format and
so on. The quality of all aspects has been remarkably
consistent. This volume is no different and it is equiv-
alent to the other volumes.
Volume 9 opens with an essay on ornithological
nomenclature by Richard Banks. This is a description
of the history, the rules of nomenclature and some of
the pitfalls. The author has tabulated some of the most
frequently used species names (cinereus and its vari-
ants is the most used). He also notes that after Linnaeus,
the originator of the nomenclature system, Philip Lutley
Sclater, a British bio-geographer and taxonomist, has
officially named the most birds.
This is a timely essay for Volume 9 because it pre-
cedes an unusual situation. Research has shown that a
proposed sub-division of the Tyrannidae had not been
formally recognized. Therefore the editors published a
description of the proposed tribe as required by inter-
national protocol. While HBOW is a little different than
the usual scientific journal, there is no reason why it
should not publish this text.
The breadth of coverage starts with the wildly col-
oured and sometimes oddball Cotingas, not just the
dazzling Cock-of-the-Rock but the bellbirds and um-
brellabirds too. The manakins are smaller but also bril-
liant. [remember stopping dead at the sight of a Red-
capped Manakin and being so transfixed I almost missed
a much rarer flycatcher; the Sulphur-rumped. But in
this edition the flashy birds are overshadowed by the
“little brown jobs - LBJs.” Just under half of the 429
Tyrannids are olive-grey-brown. Most of the larks and
pipits are LBJs too. In fact, about 75% of the species in
this volume fall into this category. This includes the
dozen or so notorious Empidomax flycatchers and the
two dozen tropical Elaenias. To separate these birds you
need a good view plus either their song or geographical
location to stand a chance at identification. Earlier
this year, a colleague and I spent 15 minutes studying a
close and very still (it was drizzling) Mountain Elaenia
before we were satisfied with its identity.
Even when the Tyranid is brightly coloured with a
yellow underside and a black-and-white striped head,
then you have 14 look-alikes to contend with. Again
geography helps but separating Social and Lesser
Kiskadee flycatchers can be tricky.
One of the qualities I have learnt to appreciate more
and more about HBOW is the perspective I get by hav-
ing the entire world taxonomy and distribution at my
fingertips. For example, when I encountered a new
species, one of the eight African longlclaws (in Mac-
ronyx) I was able to read about their relationship with
other pipits. This despite my tendency to regard them as
little meadowlarks (of the purely America Sturnella),
from their appearance and habits. HBOW brings a focus
to the biogeography and family ties to these widespread
families.
This access to worldwide taxonomy also raises ques-
tions. How can the Temminck’s (Horned) Lark of north-
ern North Africa be a different species from the Horned
Lark of Europe and North America? The variation in
plumage of the latter easily overlaps the paleness of the
former (especially Eromophila alpestris bicornis,
E.p. brandti and E.p. teleschowi). Indeed, some years
ago, I saw a Horned Lark in Manitoba that was remark-
ably pale and very close to Temmink’s Lark. I have
never doubted it was nothing more than a pale version
of our common Horned Lark. So I wonder why is Tem-
minck’s separate from the Horned Lark, which in turn
is split into 42 subspecies? I look forward to Volume
10 to see how the authors handle the stonechats, in
particular the very distinctive Madagascan Stonechat.
The editors are continuing to maintain their uni-
form, high standard and have settled in to a one-
per-year production. In this volume they have made
another useful change. Previously the plates identi-
fied the species by a number only. You needed to turn
to the text to match the number with a name. The
names of all the species depicted on a plate are now
given along with the species number in a footnote
opposite the plate.
Roy JOHN
2193 Emard Crescent, Beacon Hill North, Ottawa, Ontario
K1J 6K5 Canada
British Columbia: A Natural History. Revised and Updated
Richard Cannings, and Sydney Cannings. 2004. Greystone
Books, Douglas and McIntyre, Vancouver, British Colum-
bia, Canada. 341 pages, 209 figures. $39.95.
This paperback reprint is a gem. As the title indicates,
it is a revised and updated version of a hardcover book
first published in 1996, which won the Bill Duthie
Bookseller’s Choice Award for the “best work pub-
lished in British Columbia” that year, “The Lieutenant-
Governor’s Award for Historical Writing in British
Columbia,” and the Science in Society Award of the
632
Canadian Science Writers’ Association for the best gen-
eral work. It is an informative, attractive, extremely
well-organized book.
The Cannings brothers (identical twins), their broth-
er, Robert, and their late father, Steve, have each con-
tributed masterful photographs. All four are well-known
naturalists who have done much to encourage and fur-
ther the study of natural history through print, radio,
and television in western Canada.
The Cannings’ book succeeds at a number of levels.
Visually it is a delight, with superb, eye-catching maps
and photographs, enhanced by informative captions.
On initial browse, one is stimulated by the pithy, in-
formative, boxed vignettes, such as “when is a seagull
not a seagull?” and “Western Sandpipers.” These vig-
THE CANADIAN FIELD-NATURALIST
Vol. 118
nettes will please even the most jaded of naturalists.
Finally, the main text provides a wealth of well-organ-
ized and thoughtfully developed information. Topics
such as geology, the ice age, forests, mountains, grass-
lands, and water are clearly and incisively presented, as
the Cannings’ knowledge and enthusiasm shine through.
British Columbia is most fortunate to have such mas-
terful and able presenters; nature lovers everywhere
will benefit from this book. Only superlatives apply. I
cannot think of a single word of criticism.
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N 0J8
Canada
Field Guide to Bird Nests and Eggs of Alaska’s Coastal Tundra
By T. D. Bowman, 2004. U.S. Fish and Wildlife Service
Anchorage, Alaska. Published by Alaska Sea Grant Col-
lege Program. 81 pages, U.S. $25.00 Paper
This little publication is an interesting add-on for the
field practitioner in Alaska and the arctic. This region
includes some of the most productive bird nesting areas
in North America, and probably in the world. It shows
in detail nest and egg features of 70 bird species (loons,
waterfowl and crane, jaegers, gulls and terns, owls,
ptarmigan, alcids, shorebirds and passerines). Tavern-
er’s Canada Goose and Cackling Canada Goose receive
separate chapters. The species included in this guide
were selected based on their occurrence in Alaska and
by their “relative abundance”. Some rare species like
Sanderling, Surfbird and Yellow-rumped Warbler are
unfortunately not included, which will not really help
to bring us any closer to their nest discoveries.
This is a convenient book designed to be used in
the field. Bird species in this book are ordered by egg
size, which makes an interesting presentation. The book
design and the photo arrangements are done nicely, but
sometimes I find the egg photos a little overdone and
repetitive; sometimes wing photos are hard to differ-
entiate. For each species, the photos show the bird
(often male and female), bird on the nest, the actual
nest, eggs and (down) feathers; but this format is not
always strictly followed. Personally, I find it somewhat
a shortcoming that chicks are rarely presented in this
Guide to Hawk Watching in North America
By Donald S. Heintzelman. 2004. Globe Pequot Press, Guild-
ford, Connecticut. 425 pages, U.S. $16.95 Paper.
The Guide to Hawk Watching in North America,
written by ornithologist Donald Heintzelman, is an up-
dated version of his A Guide to Hawk Watching in
North America, published in 1979. The new edition
includes updated information about “hawk” (including
vultures, eagles, harriers and falcons) biology, identi-
fication and seasonal migration movements, as well
guide. Of interest is the concept of a “Sizing Chart’,
which “provides a quick reference to help reduce the
number of prospective species to which an egg could
belong”. Further, the book offers for geese “Parting
Shots...” in order to identify escaping birds. A quick
reference guide is provided for “Dark Goose Nests.”
Six short introduction text pages provide basic back-
ground about the species and the book concept. I ad-
mire the challenges and amount of field work involved
in compiling the specific nest and egg colour photos
(over 450). A great photo collection is presented which
includes not only, those done by the author but also
contributions from over 70 other contributors. As I
tend to be creative while in the field, I miss some free
pages to write on during field work.
The competent author has over 15 years of experi-
ence working in the arctic, and is inspired by the
“...dedication to improving the reliability and accu-
racy of scientific data...”. Therefore, it can be hoped
that these photos eventually might occur on the internet
/www for a free use by the general and interested public.
Overall, I think this interesting book serves it pur-
pose well as a quick field reference and fills a vacant
niche. I am sure it will also prove useful for Arctic
regions of Canada as well as Russia.
FALK HUETTMANN
Institute of Arctic Biology, Institute of Wildlife Biology,
University of Alaska-Fairbanks, Fairbanks Alaska 99775
USA
as numerous additional sites to watch raptors. The new
edition adds a separate section on where to view Bald
Eagles.
The book is divided into two main parts. The first
concentrates on general information, including species
accounts for a wide variety of raptors other than owls,
tips on how to identify and study hawks, a description
of the migration seasons, an overview of different types
of hawk watching, an introduction to field equipment
for the activity, and an explanation of the mechanics of
2004
hawk flight. The second part of the book focuses on
hawk watching sites, including U.S. hawk migration
watch sites, Canadian hawk migration watch sites, Bald
Eagle viewing areas, and places to view raptors out-
side the migration season.
The species accounts provide excellent identification
information on new world vultures, ospreys, kites,
hawks, eagles, harriers, caracaras and falcons. Each
species 1s described in terms of wingspread, total length,
field recognition features, flight style, voice, nest, eggs,
maximum recorded longevity, food, habitat, and North
American range. It makes for an excellent species sum-
mary, even if it lacks references to the bird’s conser-
vation status.
I found the chapter on mechanics of hawk flights
particularly interesting. Although my general under-
standing of hawk migration was fairly good when I
started reading this book, I had never looked into it in
great detail. So I was fascinated to read about the influ-
ence of general weather conditions, and the use migrat-
ing raptors make of deflective updrafts, lee waves, ther-
mals, thermal streets, squall lines, and leading lines.
I was also interested to read about hawk migration
watch sites throughout Canada, including Alberta’s
Canmore Collegiate High School, Nova Scotia’s Brier
Island near Digby, Ontario’s Holiday Beach Migration
observatory near Windsor, and Quebec’s Morgan
Book REVIEWS
633
Arboretum at the west end of Montreal — a sampling
of Canadian migration watch sites with high ratings.
Canadian entries in the Bald Eagle watch sites section
include British Columbia’s Active Pass in the Gulf Is-
lands, Pacific Rim National Park on Vancouver Island,
the Fraser Valley Bald Eagle Festival near Mission, the
Squamish Valley, the Greater Vancouver Area, and
Prince Rupert.
The section on other raptor viewing areas also offers
sites in Canada, including Amherst Island and Wolfe
Island in Eastern Ontario, both featuring Rough-Legged
Hawks and various owls during the winter season. The
other Canadian sites for concentrations of raptors out-
side the migration season are the Yukon’s North Klon-
dike Highway and South Klondike Highway. Both
areas offer year-round opportunities to see a wide vari-
ety of eagles, hawks, falcons and owls.
The Guide to Hawk Watching in North America is
an extensive and practical information source for any-
one interested in raptor watching on this continent.
My only objection about the book is its title, which I
feel should be changed to Guide to Hawk Watching in
the United States and Canada, since it lacks any ref-
erence to sites outside those two countries.
R. SANDER-REGIER
RR5 Shawville, Quebec JOX 2YO Canada
Locust: The Devastating Rise and Mysterious Disappearance of the Insect that Shaped the
American Frontier
Jeffrey A. Lockwood. Basic Books, New York. Hardcover.
294 pages, Can. $39.00 Paper.
Locust is much more than an account of a single
species of insect. In fact, it is everything the dust cover
promises: “A fascinating detective story” that delves
into “history, culture, religion, and especially ecology,
interwoven by the life story of a common insect. ...with
vivid prose, epic thoroughness and scientific precision.”
I would add geography and science to that list. Lock-
wood writes engagingly. He shares his years of detec-
tive work, providing details that only a professional
entomologist could. His historical delvings put most
historians to shame, and his writing skills exceed those
of almost any living science writer.
The book opens in Dodge County, Nebraska, in July
1875, a drought year, with clouds of locusts obscuring
the sky, their wings crackling like a horrific blaze.
Limbs of willows bent to the ground under the weight
of the insects, as adjacent cornstalks were stripped
bare. When a sheet of insects six inches thick passed
over a perpendicular ledge of rock, they caused a roar-
ing noise similar to a cataract of water. In Utah, locust
eggs were counted at 743 million eggs per acre. The
voracious insects literally ate the clothing off human
limbs, then entered homes to eat objects such as win-
dow blinds. When domestic chickens gorged on the
locusts, their eggs and flesh became inedible. Farmers
and their families lost their gardens and crops, and
were on the brink of starvation.
The U.S. Army under General Ord saved many farm
family lives by far exceeding normal army routine.
Ord issued thousands of infantry coats, shoes and mil-
itary blankets, as well as large amounts of army rations.
Lawmakers apportioned money to distribute wheat seed
for planting the following spring. Without Ord, thou-
sands would have died.
North America was blessed with hundreds of species
of grasshoppers, but only a single species of locust, the
Rocky Mountain locust, Melanoplus spretus, named
by Benjamin Dann Walsh back in 1866, caused such
vast destruction. Ingenious but rather ineffective ma-
chines such as suction machines and flame throwers
were invented to combat the locust; two men and a team
of horses could incinerate ten acres of locust-infested
fields in a day. One Minnesota community alone had
a thousand coal-tar hopperdozers that could harvest
150 000 locusts per hour.
On the scientific front, three entomologists did their
best to help combat the locust. Charles Valentine Riley
was the state entomologist for Missouri. Cyrus Thomas
and Alphaeus Spring Packard, Jr., held similar posts
in Illinois and Massachusetts. Riley was able to show
that the locust had the potential to increase its popu-
lation 100-fold from one generation to the next; he
argued that for every bushel of locust eggs destroyed,
100 acres of crop could be saved. He founded the Na-
634
tional Insect Collection and through his efforts a branch
unit in economic ornithology arose. This office became
the Bureau of Biological Survey and later metamor-
phosed into today’s U.S. Fish and Wildlife Service.
Locust has important Canadian content. Entomolo-
gist Norman Criddle of Manitoba devised a widely-
used mixture of copper acetoarsenite, molasses and
horse manure to combat later outbreaks of somewhat
less harmful grasshoppers. Criddle also collected the
world’s last two specimens of Melanoplus spretus on
19 July 1902. Three Saskatchewan men, Paul Riegert,
Bill Chapco, and Bob Randell, also helped solve prob-
lems discussed in later chapters.
Why did the Rocky Mountain grasshopper become
extinct? Five different theories in turn held sway: the
spread of alfalfa; the demise of the Bison; changes in
weather; overgrazing of grasslands; widespread prairie
fires — but each was discredited, though two were later
revisited as contributing factors..
To allow DNA studies and do radiocarbon dating,
Lockwood determined to find locust specimens en-
tombed in glacial ice for a century or more. His first
try, in 1987, yielded a quarter pound of dried grass-
hopper parts; when results were submitted to a leading
entomological journal, the editor rejected the paper
and informed Lockwood that “you have mistaken
natural history for science.” In 1988, Lockwood and
colleagues collected 134 specimens of twenty species
of grasshopper, but no locust, on the glacier. In 1989,
they obtained 4 mg of grasshopper parts, including
mandibles that appeared to match those of extant pre-
served specimens of Melanoplus spretus. Finally, in
Mammals of the World: A Checklist
By A. Duff and A. Lawson. 2004. Yale University Press, P.O.
Box 209040 New Haven, Connecticut 06520-9040 USA.
312 pages, U.S.$45.00.
Perhaps I should have bought this book some time
ago, or at least its predecessor; Mammal Species of
the World (Edited by D. E. Wilson, and D. M. Reeder,
1993, Smithsonian Institution Press), which contains
the names of the recognized species of mammals doc-
umented at that date. So many times I have struggled
to understand which species are present in a specific
area. With birds this is fairly easy to resolve. English
names are reasonably standard and scientific names
are the ultimate guide. With birds I have rarely had to
probe recent literature to catch up on the latest splits.
With mammals this is much more difficult. It took
some time to clarify the species and distribution of
fur seals. The confusion of English names for wilde-
beest left me very perplexed. My latest book on African
mammals was particularly mystifying. It is a transla-
tion from German to English and uses different Eng-
lish names for the plates and the text. The scientific
names are not current. Starting with this book it took
a lot of work to create a list of lemurs that showed the
THE CANADIAN FIELD-NATURALIST
Vol. 118
1990, at the melting edge of glaciers, they collected 250
locust bodies, including 14 males with well-preserved
abdomens and genitalia, allowing unequivocal identi-
fication and DNA analysis. These insect bodies had
taken about 150 years to travel 300 m as the ice moved
from the crevasses where they had been entombed.
Why, indeed, had Melanoplus spretus become
extinct? For once, the unplanned effects of human activ-
ity had an effect for the better. Lockwood explains that
the “base locality” of the locust was, between out-
breaks, restricted to a few relatively small areas in val-
leys within the Rocky mountains, where eggs could
be deposited in sand and gravel. Following European
settlement, floods occurred more often due to overgraz-
ing on the slopes, irrigation periodically flooded the
valleys, and the locust eggs lost their vitality. Plough-
ing and harrowing destroyed the eggs. The new alfal-
fa crops were inimical to development of the locust
nymphs. The enigma has been solved.
Lockwood is a consummate writer. His eminently
readable book is a detective story, keeping the reader in
suspense to the final chapter. Admittedly this review
has given away the ending and thus has spoiled some
of that suspense, but the pleasure of this book lies more
in its details and insights than it does in the suspense.
I strongly recommend this book to everyone with an
interest in a good story well told.
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N 0J8
Canada
currently known species and sub-species. With Mam-
mals of the World this exercise is simple.
This current list contains 5069 species. From the
Wilson and Reader list of 4629 the authors have sub-
tracted 41 species that were extinct prior to 1800. These
include such creatures as Steller’s Sea Cow, hunted to
extinction by 1768. More recently extinct species are
left in, presumably as, in theory, there is a chance of
still finding one alive. The Thylacine comes to mind.
Duff and Lawson have added 522 “new” species. A
large portion of these come from two sources. Juliette
Clutton-Brock’s work on domestic animals has elevat-
ed numerous creatures to species status (the Domestic
Pig goes from Sus scrofa to Sus domesticus for exam-
ple). The second source of change is the assignment of
species status to numerous sub-species (Colin Groves
of the Australian National University has been active in
this exercise). Finally, 41 species have been demoted in
synonymy. Sadly this loses us the Queen of Sheba’s
Gazelle (now a subspecies of the Arabian Gazelle), a
romantic loss at least. The changes in all the above
categories are fully explained in the appendices. Also
included are the nomenclatural changes in scientific
names.
2004
The authors say they have followed Wilson and
Coles (Common Names of Mammals of the World.
2000. Smithsonian Press) version of the English names
with corrections and conversion to “well-established
names.” Generally they do not list alternative names
so an animal like the Cougar, or Mountain Lion, or
Catamount only gets listed as Puma. When I used the
index, being uncertain of the author’s choice, I looked
up Lion (Panthera leo) knowing that Cougar would
be nearby. The most odd name I found was Sewellel,
the Chinook Indian name for the Mountain Beaver.
This was the first time I had seen this name although
Audubon used it on his painting of Aplodontia rufa.
Naturally I compared the list of lemurs that I had
created to that of Duff and Lawson. I was not surprised
to find many that I had as sub-species had been elevat-
ed to full species. Otherwise the lists were the same
except for Grey-brown Mouse Lemur (Microcebus
griseorufus). R. M. Rasoloarison, S. M. Goodman, and
J. U. Ganzhorn first described this cute, hamster-like
lemur in 2000. I have since been fortunate to see this
little beast in South-western Madagascar. This omis-
BooK REVIEWS
635
sion is surprising as the author’s references go up to
2002, but to be fair this is a family undergoing con-
stant change.
I was also surprised that Canada was not mentioned
in the range of the Red Wolf (Canis rufus). John The-
berge’s work has shown that Algonquin wolves are
closer to Red Wolves than the more common Timber
Wolf (Canis lupus). This information is far more wide-
ly known.
For those of us that like to travel and see mammals
in their native habitat this book is a good and useful
guide. However, it is only a list and, although it will
not resolve all taxonomic questions, it will bring
clarity and order to your research and therefore it is a
valuable reference book. As it is based on Wilson and
Reeder’s out-of-date book it is more up-to-date, but I
understand a revised edition of Wilson and Reeder
will be published soon — should we wait?
Roy JOHN
2193 Emard Crescent, Beacon Hill North, Ottawa, Ontario
K1J 6K5 Canada
Parental Behavior in Lepidosaurian and Testudinian Reptiles: A Literature Survey
Louis A. Somma, 2003. Krieger Publishing Company, Mal-
abar, Florida. x + 184 pages, U.S.$33.50 Cloth.
This book is exactly what it purports to be. It is a
summary and exhaustive bibliography of literature on
parental behaviour in lizards, snakes, amphisbaenians,
tuatara and turtles. Passing reference is also made to
literature on other vertebrates including dinosaurs.
This book focuses exclusively on behaviour as opposed
to physiological adaptations and so, while parental
behaviour in some species of snakes and lizards is well
known, many readers will be astonished to find turtles
included. Yet Somma cites references that provide
some evidence of parental behaviour for seven species
of turtles.
Fifteen categories of parental behaviour are discussed
including defence, thermo- and hydro-regulation, assis-
tance during hatching and facilitated feeding. For those
unfamiliar with research in this fascinating field the
range and diversity of parental behaviours in these
reptiles will intrigue and astonish you. Unfortunately,
description and discussion of these behaviours is lim-
ited to the first 11 pages of the book. This is followed by
46 pages of tables summarizing the results and guiding
the reader to literature on various topics and taxa. The
remainder of the book consists of 100 pages of refer-
ences and an index to subjects and taxa. Readers should
be aware that the index is inconsistent as to whether
it includes references to taxa within the tables (for
example, it does for Trachemys stejnegeri malonei but
not for Eumeces fasciatus).
The primary purpose of the book seems to be to raise
the profile of parental behaviour in non-avian reptiles
and encourage further research on this understudied
phenomenon. It is unfortunate that having read such an
enormous amount of information on this topic, Somma
does not provide more insights into its evolution and
ecological ramifications but perhaps the field is too
young for such a synthesis. Certainly for anyone inter-
ested in embarking on research into this topic it is an
invaluable and relatively inexpensive reference. For
those who are most keen on this topic, Somma has also
published an addendum to the book (Somma, 2003).
Reference
Somma, L. A. 2003. Parental Behaviour in Lepidosaurs and Turtles:
Source Addendum. Bulletin of the Chicago Herpetological Soci-
ety 38(4): 65-76.
CAROLYN SEBURN
7210 Clarenda Street, Ottawa, Ontario K2B 7S5 Canada
Prairie Ghost: Pronghorn and Human Interaction in Early America
By Richard E. McCabe, Bart W. O’Gara, and Henry M.
Reeves. 2004. 176 pages, U.S.$29.95 Cloth.
The Pronghorn, Antilocapra americana, formerly
called “antelope,” is the “most American” of the con-
tinent’s terrestrial wildlife, since it is found nowhere
else. It is the world’s second fastest land animal, and
perhaps the most inquisitive. Protuberant eyes allow it
a nearly 360-degree field of vision. Large lungs, heart
and trachea permit it to achieve great speed.
This historical look at the Pronghorn is thoroughly
researched, with informative tables, extensive refer-
ences, and well-chosen, sumptuous illustrations. It
636
delves deeply into anthropology. The Pronghorn rep-
resented fleetness, alertness, and pertinacity, and was
a catalyst in the social structure and welfare of most
plains tribes. It is no wonder that many place names
today derive from this one species, but who would have
expected 108 such instances in Arizona and 79 in Wy-
oming? Two detailed appendices list dates of eyewit-
ness accounts between 1540 and 1896, and the names
of the Pronghorn in each native language. Historical
accounts go back to Sahagun in 1569 and Hernandez
in 1651, both in Mexico. Lewis and Clark popularized
it during their exploratory journey of 1804-1806, and
George Ord gave the Pronghorn its binomial Latin
name in 1815.
Before Europeans reached the Americas, aborigines
hunted the swift-footed Pronghorn with three instru-
ments: sling, atlatl, and bow-and-arrow. A well-condi-
tioned, determined native could sometimes, in spite of
his much slower pace, outlast and eventually tire and
kill a Pronghorn. More often, stalking, pursuing, sur-
rounding, luring, calling, impaling, ambushing, netting,
driving with v-shaped fences, setting prairie fires, and
making pitfalls, were the methods used to kill them
for food. Pronghorn hunting required more prepara-
tion and more co-operative effort than did hunting of
the larger Bison. The Pronghorn was then one of the
natives’ most important food sources, especially where
Bison were scarce near the edge of their range. An
antelope skin was thinner and lighter than that of a
Bison, and thus more suitable for clothing. A native
would obtain about 45000 calories from a 43-pound
Pronghorn carcass.
Pronghorn bones were used as toys, rattles, awls,
pipes, fishhooks and decorations. Sinew served as
strings for bows, and for sewing. A skin stretched tight-
ly over a section of hollowed tree formed a drum.
Marrow was rubbed on sunburned or chapped lips and
THE CANADIAN FIELD-NATURALIST
Vol. 118
skin. A Pronghorn fawn was used as bait on branches
above a pit where an Indian patiently waited to catch
a Golden Eagle for its feathers. Images of the Prong-
horn were used to decorate native pottery, on the walls
of caves at ten known sites, and as effigies.
Hunting became much easier after guns spread north
from Mexico and guns and ammunition were obtained
in trade, but this soon led to squandering of the once-
precious resource by a veritable army of 5000 white
hunters. From 1874 through 1877, more than 100 000
Pronghorn hides were shipped from the plains annually.
As the Bison almost vanished, the Pronghorn became
even more important as a food source, and their num-
bers dwindled as well, from about forty million to fewer
than 15000 in 1910. Bereft of their two largest natural
food sources, native peoples were overwhelmed, sub-
jugated, displaced, and pauperized of their culture, iden-
tity and social options, losing much of their spirit and
vitality.
Although three of the four last sections tell a grim
story, dealing with the near demise, in turn, of the
Bison, the people, and the Pronghorn, the book ends on
a positive note with the birth of the conservation ethic.
In 1887, Theodore Roosevelt convened a dinner meet-
ing in Manhattan to launch the Boone and Crockett
Club; he and the other founders had a strong affection
for the Pronghorn, which eventually benefitted from
the conservation ethic and philosophy of this fledgling
movement.
This attractive, scholarly, modestly-priced book
belongs in major libraries. It would make a perfect gift
for anyone interested in history, geography, anthro-
pology, or big game hunting on the plains.
C. STUART HOUSTON
863 University Drive, Saskatoon, Saskatchewan S7N 0J8
Canada
A Guide to the Birds of St. Helena and Ascension Island
By N. McCulloch. 2004. The Royal Society for the Protection
of Birds, The Lodge, Sandy, Bedfordshire, SG19 2DL
Great Britain. iv + 92 pages, 11 GBP.
The booklet is intended for the visitor and has three
parts. The first is an overview of island history from
time immemorial to present. The second is a site guide
giving where to find birds on these islands. The last
part is the bird accounts.
The bird accounts cover 31 species for St. Helena
and 46 for Ascension that a visitor is likely to see in a
day trip around each island. Of these 11 are seabirds
and 10 are shorebirds on St. Helena and 13 are seabirds
and 16 shorebirds on Ascension So only about 30 % of
the island species are land birds, with most of them
being introduced. There have been 41 other attempts
at introduction on St. Helena and 9 on Ascension
The account of the history is fascinating and so
typical of remote islands, especially after its “discov-
ery” by humans. This is not good bedtime reading
though. The destruction of the islands ecosystem is the
usual unpleasant tale of wanton destruction misguided
mistake and foolish carelessness. There have been 41
failed attempts to introduce everything from a white-eye
to an ostrich to St. Helena and 9 attempts on Ascension.
This includes the introduction of House Sparrows in
1986 (to be company for a ship-assisted vagrant who
arrived in 1985). Will we never learn? On a happier note
there are programs underway to restore habitat for
around 40 species of endemic plant and 9 species of
creepy crawlies (one — the Golden Sail Spider — is
illustrated) as well as birds. There are also programs
to reduce cats, goats and the like.
The bird finding section is typical of current field
guides, portraying the bird on the left and giving infor-
mation on the right. It covers 28 species. Half of these
are seabirds. The remainder are land birds, almost all
introduced. The English names are fairly consistent
with other texts, but there are no references to alter-
2004
| native names. For example Maderan vs. Band-rumped
Petrel or Parasitic Jaeger vs. Arctic Skua. The text here
along with the rest of the book is good and clear.
The author has added a table of accidental species
for the two islands (31 on St. Helena and 46 on Ascen-
sion. This did not quite match my own list, but I think
the difference is due to the political boundary that in-
cludes Tristan de Cunha and Gough Islands, thus add-
ing several Antarctic species)
The artwork consists of watercolours that are refined
sketches of birds during their normal activities. This
gives a better idea of their jizz than the more formal-
ized field guide style of the recent books, and is more
_ akin to the style of postwar books. Indeed, my favour-
ite is a perky field sketch of a Java Sparrow that fronts
| the section of land birds on which you can almost
| count the small number of brush strokes. The reader
| can compare this with the more “finished” plate in the
accounts section.
I found it ironic that the endemic Madagascar Fody
| was introduced, not from Madagascar but from Mau-
| ritius (where it is an introduced threat to the endemic
| BOTANY
BooK REVIEWS
637
Mauritius Fody) and became so numerous it was part
of the St. Helena cage bird trade. How convoluted we
make the world.
So why go to these remote places? First there is the
attraction of wild oceanic islands. While they are no
longer the lush paradise first seen by the Portuguese
they still are dramatic. The rich brown cliffs surround-
ed by blue sea set off the white, guano-capped islands.
Second, however diminished, there are good seabird
colonies; always exciting places. And last, for the hard
core, they are the only places to see Ascension Island
Frigate and Wirebird. While remote, these islands are
not inaccessible. There are some tours that include them
on a cruise, although these are very expensive. Routine
commercial sailings leave from Cardiff, Wales and Cape
Town, South Africa a few times a year. They dock in
St. Helena and Ascension for a day or two — enough
time with this guide to see most of the islands birds
Roy JOHN
2193 Emard Crescent, Beacon Hill North, Ottawa, Ontario
K1J 6K5 Canada
| Flora and Climatic Conditions of the North Pacific: A Collection of Scientific Papers
| Edited by A. N. Berkutenko, H. G. Lumsden, and D. Lumsden.
2001. Institute of Biological Problems of the North, North-
East Scientific Center, Far East Branch, Russian Academy
of Sciences. Magadan. 189 pages, No price available.
The subtitle — A collection of papers — better indi-
| cates the contents of this book than does its lead title.
| What we have here is a nicely produced small book
| consisting of papers on flora and vegetation, for the
| most part, but also one paper each on fungi and eth-
nobotany, two on seed biology, and one on the influ-
| ence of air masses from the Sea of Okhotsk on sum-
mer temperatures in Japan. An odd mix, but perhaps
| the inevitable result of the need to collect sufficient
| papers, achieve critical mass, and gain publication.
| To one interested in floristics and taxonomy, several
_of these papers are informative and useful. Since the
| book is entirely in English, it opens to a wider audi-
ence than usual the results of botanical studies in the
Russian Far East. The prime mover for this collection
was A. N. Berkutenko who wrote entirely or con-
_ tributed to six of the collected 15 papers. Since it is
difficult to generalize the disparate contributions, I
will give a précis of each.
Yakuboy et al. provide a brief sketch of the physical
_ setting, a history of botanizing, and an annotated check-
| list of 235 species for the flora of Avachinsky volcano.
| The next paper by Mochalova describes the very
small flora of very small islands of the Commander
archipelago and the effects of bird colonies on the veg-
etation there. Two papers by Khoreva and by Berku-
tenko et al. discuss the vegetation and flora of two
islands in the Sea of Okhotsk and provide checklists
for the Yams Islands and Nedorasumenia Island, the
latter with the unexpected occurrence of the Asiatic
shrub Caragana jubata.
Sinelnikova gives a synopsis of the plant cover and
a checklist for 454 species of vascular plants found at
the Orotuk field station in the upper Kolyma River
region. The station lies in larch taiga near the Koly-
ma floodplain. The Chosenia arbutifolia and Populus
suaveolens of the gallery forest and the Pinus pumila
communities farther upslope are among the memorable
botanical images I took away from my trip to the
region. A short paper by Berkutenko and Khoreva, in
a structure now familiar, provides a sketch of the veg-
etation and a checklist to the 98 species found at the
Mount Kamenny Venets nature monument, which in-
cludes the endemic willow Salix magadanensis. Thus
ends the first 117 pages. From here on, the papers have
less to do with each other or to what has gone before.
A list of 161 macromycetes in the Magadan Preserve
by Sazanova is followed by a report by Berkutenko
and Yukawa of the first record for the orchid Liparis
kumokiri for mainland Russian Far East.Next Misako
proposes that morphological variation in the Japanese
Sanguisorba tenuifolia has originated from hybrids
between S. parviflora and S. officinalis occurring in
coastal Russian Far East. In a brief, idiosyncratic but
interesting essay, Berkutenko contrasts with ethnobotan-
ical anecdotes the changes that have taken place in
people’s live since Krasheninnikov reported on 18"
century habits of the local people on Kamchatka. She
includes some differences between practices in the
Russian Far East and Alaska as well. This paper is fol-
638
lowed by comments on the germination of 78 species
by Andrianova and Berkutenko: which taxa require
pretreatments and which kinds of treatments are effi-
cacious. A paper by Kryukov reports briefly on the
relative germination success of 27 species following
different periods of storage. Haese describes a phytoso-
ciological analysis of coastal tundra using the methods
of Braun-Blanquet, and provides tables typical of this
analysis. Hanno and Oka in a short paper that reads
more like a proposal noted that the Sea of Okhotsk
affects the climate of eastern Japan. Pachomov and
ENVIRONMENT
The Russian Far East
By Josh Newell. Second Edition, 2004. Daniel and Daniel,
Publishers, McKinleyville, California, USA. 486 pages,
U.S.$59.95. Paper.
This is a massive and thorough compendium. The
subtitle reads, “A reference guide for conservation and
development.” The format is a series of chapters each
concerning one of the major administrative divisions
of the huge region, abbreviated as “RFE.” These divi-
sions are: Primorsky Krai, Khabarovsk Krai, Jewish
Autonomous Oblast, Amur Oblast, Republic of Sakha,
Magadan Oblast, Chukotsky Autonomous Okrug (Chut-
kotka), Koryak Autonomous Okrug (Koryakia), Kam-
chatka Oblast, Sakhalin Oblast. There are over 50 maps,
and a host of tables, figures and photographs, as well
as an index.
Vegetation is organized into the classic Tundra and
Taiga formations. This book divides Tundra into two
parts: “Arctic Tundra” and “Tundra” (referred to in
much Russian ecological literature as “High Arctic”
and “Low Arctic.”) Taiga is defined correctly as “the
large mass of the boreal forest that forms the heart of
the RFE.” The southern taiga, which in much of Russ-
ian ecological literature is known as Ussuri Taiga, is
also known as “Dark Taiga” because of the high per-
centage of spruce and pine.
This division serves to differentiate it from the
northern part of the Taiga which is widely known in
the Reindeer literature as “Light Taiga’” because of the
very large percentage of the forest cover of deciduous
larch. The Reindeer literature, and much ecological
literature, also designates the southern-most tundra,
combined with the northern-most taiga as ‘‘Forest-
Tundra.” This recognition of it as a separate entity is
undoubtedly because the Forest-Tundra is particularly
important as winter pasture for the semi-domesticated
Reindeer.
The Ussuri taiga is relatively familiar to English-
speaking biologists because of translations of works by
such authors as Sdobnikov and Arseniev, as well as
Kurosawa’s famous 1975 film about Arseniev and
Dersu. The number and distinctiveness of the species
of plants and animals of the RFE is legendary, espe-
cially the Ussuri taiga.
THE CANADIAN FIELD-NATURALIST
Vol. 118
Sinelnikova present six years of observations on the
effect of artificial warming on the growth of four tun-
dra plants at or near the field station described by
Sinelnikova (see above). I fear these studies in support
of the International Tundra Experiment (ITEX) proj-
ect will be lost to the [TEX community in these pages;
it belongs with others of its ilk.
DAvID F. MURRAY
University of Alaska Museum of the North, Fairbanks, Alaska
Each of these 10 administrative regions receives a
section of the book. Each begins with an overview,
ranging from a paragraph or so to a number of pages,
followed by extensive entries on: location, size, climate,
geography and ecology (including carbon stocks), major
ecosystems, protected areas and their problems, bio-
diversity hotspots, political status, natural resources,
main industries, infrastructure, foreign trade, economic
importance in the Russian Federation, general outlook.
This latter section is particularly interesting for such
items as a full-page table of major environmental issues
and problem areas of each of the regions: fishing,
energy, timber, mining, agriculture. There are pertinent
discussions of the weaknesses of various Russian gov-
ernmental regulations concerning oil, gas and mining
operations compared to the (already-weak) United
States and Canadian regulations.
There is discussion of various schemes with poten-
tially-severe effects as well as prospects for a sustain-
able economy, ENGOs, the UN Global Environment
Facility, foreign government aid agencies, other prom-
ising sectors such as ecotourism and NTFP (Non Tim-
ber Forest Products). There is rather detailed consid-
eration of the degradation of zapovedniks (“protected
areas”) by tourism, poaching (salmon, caviar), bear
killing (for paws and gall bladders).
The forests of Kamchatka are particularly vulnerable
and critical for mitigating floods and protection of
salmon spawning grounds. (Remember British Colum-
bia?). In the RFE the largest emitter of atmospheric
CO, is fossil fuels combustion, but second place is de-
forestation leading to loss of carbon-rich boreal forest
and replacement by pioneer types of forests and shrub-
by vegetation. More than 90 percent of the logging in
the RFE is by clearcut. Even plantation-forests do not
recover pre-logging stocks of CO,; managed planta-
tion-forests usually contain only 4 to 4 the carbon
that undisturbed forests do.
Activities to “Save Tropical Forests” are having
adverse effects on the taiga of the RFE... “Plywood
manufacturers are promoting Russian larch (tamarack)
as a green alternative to tropical luan timber and have
been steadily increasing levels over the past decade...
|More than 98 percent of all Russian larch grows on
/some form of permafrost (continuous, discontinuous,
| sporadic) making large-scale logging of the species an
| unwise proposition” (page 31).
“The sheer size of the Siberian and RFE forests and
| the diversity of their plant and animal life and habitats
| make these forests a tremendously important factor in
|}Russia and the world. Loss of habitat, mostly from
| forest exploitation, fire, disease and inappropriate man-
| agement is the most serious threat to the unique bio-
diversity of climax forests. The survival of endangered
| species, such as the Siberian Tiger ... depends on the
/maintenance of large, undisturbed forest areas. Frag-
‘ile permafrost areas must be recognized as environ-
‘mentally critical and the forests’ large contributions to
carbon sequestration must not be jeopardized. Such
environmental considerations are currently inadequate-
ly incorporated in the planning process or not properly
) addressed in forest management and harvesting activ-
|ities. As a general requirement for attending to these
environmental concerns large forested areas must re-
‘main undisturbed and forests outside protected areas
/need appropriate and complementary management.”
(page 32)
The Russian Far East has the endangered Siberian
Tiger (Panthera tigris altaica) while Canada has the
}endangered Woodland Caribou (Rangifer tarandus
caribou) (Pruitt and Baskin 2004; Schaefer 2003). Pages
35 — 39 also bring problems in the RFE directly home
to Canada: “A major problem is the lack and loss of
| field scientists and field workers because of dramatic
cuts in government funding...” We can compare the
situation in the RFE with the massive cuts in scientif-
ic staff of Canadian Wildlife Service, National Parks
| Canada, Canadian Meteorologial Service and the Cana-
| dian Museum of Nature, beginning with the Mulroney
Conservatives and not restored by later governments.
In Canada, the problem is compounded by the growing
infatuation of university biology, botany and zoology
| departments with “computer models” or “keyboard
ecology” instead of learning about real animals and
| plants (Ehrenfeld 1993; Futuyma 1998; Noss 1998).
__ The book is almost overwhelming in its information:
history of European invasions, lists (with comments)
of major species of plants and animals, lists of endan-
gered species (usually with comments regarding threats
to survival), lists of protected areas by type, size, date
of establishment, biodiversity hotspots, human econ-
-omy and environmental impact.
The sections on Indigenous Peoples and their decline
_in numbers, relations and their problems with “modern”
BooK REVIEWS
639
extractive economy (mining, logging, etc.) is particu-
larly instructive because of the great resemblance to
the history of similar Aboriginal groups and their ex-
ploitation or rejection by Canadian governments and
industries.
We read much in the western press about the wide-
spread pollution and environmental destruction dur-
ing the Soviet era, but “While the focus has been on
nuclear, air, and water pollution and, somewhat less, on
the wanton waste of resources caused by inefficient
production, scholars have largely ignored what may be
the most significant environmental legacy from the
Soviet era, and what is Russia’s greatest legacy to the
planet: wilderness.” (page 29).
Although the Russian Far East is well over the shoul-
der of the world from Canada, the unity of the taiga
(so-called “boreal forest’) is evident by the similarity
of its animals and plants to those in Canada. We can
also see in this compendium disturbing similarities to
the problems affecting the Canadian taiga (Pruitt and
Baskin 2004; Schaefer 2003). Comparison of amelio-
rating efforts will be valuable. There are many places
in Canada which should have copies of this valuable
compendium: Federal and Provincial departments of
Conservation, Natural Resources, Forestry, Wildlife,
Aquatic Resources, Fisheries. All University libraries,
the libraries of all ENGOs concerned with conservation
and sustainable use of renewable resources, anthropol-
ogy and aboriginal activists, everyone teaching Field
Biology, Ecology, Boreal Ecology, Resource Manage-
ment, Forestry, Wildlife Management, Fisheries Man-
agement or Sustainable Development course or seminar
should have access to a copy.
Literature Cited:
Ehrenfeld, D. 1993. Beginning again (pages 65-72). Oxford, Oxford
University Press. Pages xiv + 216.
Futuyma, D. 1998. Wherefore and whither the naturalist? American
Naturalist 151(1): 1-6.
Noss, R. F. 1998. Does conservation biology need natural history?
Wild Earth 8: 10-14.
Pruitt, W. O., Jr., and L. M. Baskin 2004. Boreal Forest of Canada and
Russia/Taiga of Canada and Russia. Bilingual, English and Russian,
parallel texts. Pensoft Publishers, Sofia, Bulgaria, illustrated: 163
pages ISBN 954-642-199-5.
Schaefer, J. 2003. Long-term range recession and the persistence of
Caribou in the taiga. Conservation Biology 17(5): 1435-1439.
WILLIAM O. PRUITT, JR.
Department of Zoology and Taiga Biological Station, Univer-
sity of Manitoba, Winnipeg, Manitoba R3T 2N2 Canada
640
THE CANADIAN FIELD-NATURALIST
Vol. 118
Resource and Environmental Management in Canada: Addressing Conflict and Uncertainty
Edited by Bruce Mitchell. 2004. Third Edition. Oxford Uni-
versity Press, Don Mills, Ontario, 608 pages. Can $46.50
Paper.
Canada is a resource-rich country. The nation’s his-
tory and folklore are a story of resource exploitation
and the people who trapped, fished, farmed, mined and
lumbered. In many ways, much has not changed as
evidenced by the national wealth accrued from natural
resources, the dependence of many towns and regions
on primary resource use, and the growing social con-
flicts centred on the type and intensity of resource use
and conservation.
It is generally acknowledged that all natural ecosys-
tems are more or less human-dominated. Recent, well-
cited studies have estimated that humans appropriate
over 30% of the total terrestrial net primary produc-
tion. This is a remarkable level of consumption for
humans that represent roughly 0.5% of the total het-
erotroph biomass on Earth. Spatially-explicit studies
have identified appropriation levels that range from
> 6% for South America to > 80% for south-central
Asia. North America falls in between with a human
appropriation level of 23%.
Given these levels of human domination of the
earth’s resources, it is understandable that the notions of
conflict and uncertainty would be chosen as thematic
foci for a book on resource and environmental man-
agement; conflict among differing values and ideolo-
gies, and uncertainties over adequate scientific and
social knowledge.
A long-standing textbook, now in its third edition,
Resource and Environmental Management is intended
primarily for undergraduate university students. The
book’s 20 chapters are broken down into three parts:
(1) emerging concerns, (2) enduring concerns, and (3)
contemporary responses to these concerns. Emerging
concerns include ecosystem health and ecological
integrity, globalization and neo-conservatism, First
Nations and resources, feminist perspectives, climate
change, and water security. Enduring concerns focus
on traditional resource issues such as fisheries, agricul-
ture, forestry, wildlife management, mining, and parks
and protected areas. The third part addresses some of
the approaches used to develop resource and environ-
mental visions. Among others, these include search
conferences, ecosystem approaches, adaptive manage-
ment, environment impact assessment, participatory
approaches, governance issues, and environmental jus-
tice. The majority of contributing authors are geogra-
phy and environmental studies academics.
In any collection of contributed essays, consistency
in style and quality is always a challenge. Conflict and!
uncertainty act as foundational themes and tie together
all chapters. Most, if not all authors, attend to this
theme and regularly make reference to other chapters
in the book. Many of the chapters have been rewritten
and updated for this edition and seven new chapters;
have been added. The editor has prefaced each major;
section with a good synthesis and summary of each)
chapter thus helping the reader to situate the individ-
ual contributions.
Authors provide a sound scientific and technical
analysis of each resource issue, generally up-to-date
resource statistics, and policy implications. The strength
of the edited volume is the authors’ attention to the
social, cultural and political dimensions of resource
and environmental management. A former forest ecolo-
gy professor of mine was wont to proclaim: “Forestry
is more about people than it is about trees.” The same
can be said for all other resource issues. Because of the
essential human dimension, ecosystem-based natural
resource management is not rocket science — it’s much |
more complicated than that. The amalgam of biophys-
ical, cultural and social complexities fuel conflict and
promote uncertainty. This inherent complexity of re-
source and environmental management is highlighted
throughout the text. Well discussed, as well, are a
number of significant mechanisms that attempt to deal
with the often intractable and inherently stochastic
dimensions of institutional human behavior.
I found some of the essays unnecessarily long-
winded and somewhat pedantic. Twenty chapters weigh-
ing in at over 600 pages do not make for easy or nec-
essarily enjoyable reading, especially given the diversity
of chapter topics. The chapter on forest management
is noticeably remiss in addressing contemporary sus-
tainable forest management paradigms. No mention
is given, for example, of the current developments in
the emulation of natural forest landscape disturbances,
a key concept in sustainable forest management. As
an edited book it does not possess the thrill or the
fast-paced narrative of a single author. As a textbook,
it has all the information, but you may find yourself
simply dipping into chapters of specific interest.
JOHN MCCARTHY
Holy Rosary Parish,
NIE 1V6 Canada
175 Emma Street, Guelph, Ontario
d
2004
| MISCELLANEOUS
By Jonathan A. Edlow. Second Edition, 2004. Yale Universi-
ty Press, New Haven and London. 304 pages. U.S.$29.95
Paper.
There have been few newly-emerging infectious dis-
;eases that have generated as much controversy as to
their etiology and treatment as Lyme disease. From
the “conventional” viewpoint, the disease is easily and
accurately diagnosed, and short-term antibiotic treat-
ment is effective; in the “alternative” point of view,
‘the diagnosis of late-presenting cases is often missed
_ due to inaccurate diagnostic tests, and long-term antibi-
_ Otic treatment of such cases is necessary for a cure. This
readable book gives a fair and balanced account of the
differing points of view of these two camps. It covers
| the history of the discovery of Lyme disease, the elu-
cidation of its causative agent, and the development
of diagnostic tests and of treatments for the disease.
| The disease was first recognized in North America
when, around 1975, doctors at the Yale University
School of Medicine noticed a new array of symptoms
in patients from the area of Lyme, Connecticut. These
symptoms consisted of a growing, ring-shaped rash
(the bull’s-eye) at the site of a tick bite, and swollen
joints. Sometimes the rash and the arthritis had ap-
peared without the patient’s being aware of a tick bite.
The author, Jonathan Edlow, M.D., is Vice-Chairman
of the Department of Emergency Medicine, Beth Israel
Deaconess Medical Center, and Assistant Professor
of Medicine, Harvard Medical School. He himself
describes the book as “a medical detective story” that
_| flowed from a combination of his interest in infectious
diseases, and the fact that relatives of his who had
| moved to the Lyme area in the 1980s were stricken with
symptoms of a bizarre arthritis, and/or rashes following
_| tick bites.
The author starts with a detailed and interesting
j; account of how, in the 1970s, residents of the Lyme area
were experiencing a baffling array of physical symp-
toms, including rashes, unexplained neurological symp-
toms and swollen joints, that eluded diagnosis by their
"| family doctors. Then two women, who together with
; their families and neighbours, had been ill for several
years, were separately urged by their doctors to visit
the Rheumatology Clinic at the Yale School of Medi-
cine in New Haven. After hearing their stories, the doc-
tors at the clinic realized that about thirty-five cases
) : : ae
clustered in the Lyme area were presenting similar
!
| Edited by Peter Kareiva and Simon A. Levin. Princeton
University Press, 41 William Street, Princeton, New Jer-
sey 08540. 427 pages. U.S.$53.00 Paper.
The ecological impact of the economic system we
subscribe to could be viewed as the largest of all pos-
BOOK REVIEWS
64]
Bull’s Eye: Unraveling the Medical Mystery of Lyme Disease
symptoms, and that an investigation into “what was
happening at Lyme” was required. At the same time,
U.S. Navy doctors at the nearby base in Groton, Con-
necticut, observed several patients with ring-shaped
rashes which spread over a large area. Their case report
in The Journal of the American Medical Association
(JAMA), was read by a family doctor at the eastern
end of Long Island who had patients with tick bites
surrounded by a rash, who thought that his patients
might have the same disease. He realized it was similar
to a disease that had been recognized in Europe since
1910 as erythema migrans (EM). In the European
reports, the disease was associated with tick bites and
thought to have a spirochaete as the causative agent.
Having set the scene, the author describes the iso-
lation of this causative agent by Willy Burgdorfer at
the Rocky Mountain Laboratories, U.S. Public Health
Service, who demonstrated that a spirochaete found in
the deer tick, Ixodes scapularis, caused Lyme disease.
The organism was later named Borrelia burgdorferi
in his honour. But this tick can carry other pathogens
(e.g., Babesia spp.) causing a co-infection in some
patients, complicating both diagnosis and treatment.
He further describes how, over time, a definite schism
arose between the two groups of doctors maintaining
the differing viewpoints mentioned. Patient advocacy
groups arose who mainly supported the “alternative”
position and, in 1993, a U.S. Senate Committee held
hearings on the subject. The author sums up the cur-
rent position by saying that debate remains about the
best way to diagnose the disease, the utility of long-
term antibiotic treatment, and the safety of a vaccine.
A drawback in the author’s style arises when he uses
analogies to try to explain scientific concepts. One
example is that of a five-page description (complete
with 5 Tables!) of the separation of peaches, apples,
oranges and nectarines by machine, in an attempt to
explain the meaning of the terms sensitivity and speci-
ficity in assessing the accuracy of laboratory tests. The
result is confusion.
Appendix A lists the symptoms of Lyme disease,
Appendix B lists tick-borne diseases in humans and
animals. The book does not have a bibliography but.
following the appendices, gives a list of sources for
each chapter.
PEARL PETERKIN
#801 — 240 Brittany Drive, Ottawa, Ontario K1K OR7 Canada
The Importance of Species: Perspective on Expendability and Triage
sible species removal experiments. Unfortunately for
us, this experiment is unreplicatable—we only get one
shot at it. From the mid-point things don’t look good.
When the consequences of our personal actions and
public policies are compared to the cataclysmic impact
of an asteroid (we are in the midst of the sixth and
greatest wave of extinctions on the planet after all) you
know we're in trouble. Still, the overwhelming number
of species facing imminent elimination has lead some
to ask if we need to protect every one? Surely of the
millions of species we “share” Earth with there must
be a few that we could afford to lose? Especially con-
sidering the expense and inconvenience of conserva-
tion programs.
“The importance of species” sets out to answer
that question. Or at least to summarize the collective
experiences of the ecological community in examin-
ing the idea of species expendability. The initial impe-
tus for this volume came from a symposium to hon-
our the accomplishments of Robert Paine. Dr. Paine’s
pioneering work on the importance of species began
nearly 40 years ago. His investigations were based on
a simple idea: if you want to understand the role of a
particular species in a community, remove it and see
what happens. He works primarily in rocky inter-tidal
zones. It was there he discovered that some species
are absolutely critical to that ecosystem: remove one
of these “keystones” and the community collapses.
This conclusion has since been reached by many other
ecologists working in different systems, and the book
provides a nice introduction to their work. However,
while keystone species have been identified in a variety
of settings, their redundant counterparts have been
harder to locate.
The strength of this book lies in the diversity of
voices that converge on a few common conclusions.
The most critical outcome of a great deal of research
is the recognition that identifying truly redundant spe-
cies is an extremely difficult and perhaps impossible
task. Each paper presents new obstacles. Louda and
Rand present a particularly nasty problem in the first
chapter. Native thistles of the Great Plains may ini-
tially appear to be expendable as a direct result of their
being essential! They argue that the native thistles serve
to inoculate the community against the invasion of their
exotic relatives. The presence of the native thistles sup-
ports populations of herbivorous insects which readily
switch to feeding on exotic thistle species that have
been introduced to the region. In areas where this has
been most successful the exotic thistles have been al-
most completely excluded from the community. Under
these conditions the exotic thistles do not appear to
pose a serious threat to the community, so the value
of the native thistles is not readily apparent.
More generally, the environmental context may
determine the relative importance of a species in a
community. A keystone predator at one location may
have negligible influence at another (Chapter 2). Sim-
ilarly, the influence of a species may vary greatly over
time (Chapter 3). Think of a herbivorous insect that
spends nine years in small, widely scattered populations
of minor importance, only to erupt in the tenth year
to devastate thousands of hectares of forest (and feed
THE CANADIAN FIELD-NATURALIST
Vol. 118
millions of birds...). At a broader temporal scale,
Stephen Palumbi (Chapter 15) notes that important
ecological associations can evolve rapidly. A species
that is redundant now may become an important com-
ponent of its ecosystem in a few decades. The blink
of an eye in evolutionary terms, but an eon measured
in funding cycles. Taking a different approach Daniel
Simberloff (Chapter 11) examines the impacts of the
extinctions or near-extinctions of species one could
reasonably assume to be important community mem-
bers (i.e., American Chestnut, American Elm, Bison
etc.). He reveals two related challenges: we have very
little data to objectively assess the impacts of these
losses, and there is no agreement on what constitutes
a significant “ecosystem consequence”.
As you would expect from a book with 28 authors
the treatment is a little uneven. Given the emphasis on
detailed natural history knowledge that many authors
present as critical to the question, I was not convinced
of the value of theoretical models in predicting which
species are expendable. Shahid Naeem’s (Chapter 6)
discussion of ecosystem reliability models starts from
the assumption that species are interchangeable, effec-
tively sidestepping the entire issue.
The most troubling essay is perhaps the most impor-
tant one in evaluating the concept of expendability.
Mary Ruckelshaus, Paul McElhany, and Michael Ford
collaborate in reviewing their efforts to conserve Pacific
salmon species as part of the American National Marine
Fisheries Service. Given that five of six of these pre-
sumably economically important species are threatened
or endangered, you might expect they would approach
their task with the objective of maximizing the viability
of the various stocks. On the contrary, they outline the
process they followed in determining how many more
populations they can afford to lose. This is a chilling
glimpse of the possible future of conservation biology.
The emphasis is not on how best to protect and enhance
our biological heritage. Rather, conservation goals are
set in a manner that minimizes their impact on eco-
nomic objectives.
Egbert Leigh’s contribution, “Social conflict, bio-
logical ignorance, and trying to agree which species
are expendable” (chapter 12) provides an insightful
review of the entire debate. He identifies a critical need
for basic natural history research if we are to have any
hope of understanding the relative importance of indi-
vidual species. More importantly, he reminds us “that
social conflict, whether latent or blatant, is the biggest
single obstacle to sound conservation. Suppose for a
moment that we were Laplacean demons, able to assess
the ecological consequences of each and every extinc-
tion. Would this circumstance really cause society to
close ranks behind conservation? As the world seems
organized to destroy any sense of community among
human beings, a greater knowledge of biology is not
likely to make it easier for society to agree on conser-
vation policy.” Leigh reinforces the value of natural
2004
| history in dealing with biological issues, while prop-
| erly identifying the question of species expendability
as part of a larger social problem.
This is an important book, and deserves the critical
attention of conservation biologists. In an age when we
_ are pressured to apply a business model to all aspects
of our society, it is important to examine the conse-
| quences in a rigorous way. The essays in this book
NEW TITLES
+Available * Assigned
Zoology
*Common Birds of Ontario. By D. Sept. 2004. Calypso
| Publishing, Box 1141, Sechelt, British Columbia VON 3A0.
| 93 pages, Can. $12.95.
) +Birding in Venezuela (revised edition). By M. Goodwin.
| 2004 Lynx Edicions Barcelona Spain. 332 pages, U.S.$25.60
| Paper.
| Birds of the Middle East (Reprint of 1996 edition). By R.
| Porter, S. Christensen and P. Schiermacker-Hansen. 2004.
Princeton University Press, 41 William Street, Princeton,
| New Jersey, USA, 08540-5237. 480 pages, U.S.$35. Paper,
| U.S.$65 Cloth.
| +Bumblebee Economics (2™ Edition). By B. Heinreich.
| 2004. Harvard University Press, 79 Garden Street, Cambridge,
Massachusetts 02138 USA. 245 pages, U.S.$19.95 Paper.
_ *Damselflies of Alberta — Flying Neon Toothpicks in the
| Grass. By John Acorn. 2004. University of Alberta Press,
! Ring House 2, Edmonton, Alberta T6G 2E1 Can. $29.95.
_ Experimental Approaches to Conservation Biology. Edit-
_ ed by M. S. Gordon and S. M. Bartol 2004. University of
California Press, 2120 Berkeley Way, Berkeley, California
94704-1012. 358 pages, U.S.$75.
*Frogs of Australia. By J. Turner. 2004. Pensoft Publishers.
Acad. G. Bonchevy Str., Bl. 6, 1113 Sofia, Bulgaria. 276 pages,
Eur 34.50 Cloth.
*How the Earthquake Bird got its name and Other Tales
of an Unbalanced Nature. By H. Shugart. 2005. Yale Uni-
versity Press, P.O. Box 209040, New Haven, Connecticut
06520-9040. 227 pages, U.S. $30. Cloth.
Hummingbirds. By L. Aziz. 2004. Firefly Books Ltd., 3680
Victoria Park Avenue, Toronto. 64 pages, Can. $9.95. Paper.
*Mammals of Australia. By J. Turner. 2004. Pensoft Pub-
lishers. Acad. G. Bonchev Str., Bl. 6, 1113 Sofia, Bulgaria.
216 pages, Eur 38.50 Cloth.
*The Peregrine Falcon Survey in Canada. Edited by U
Banasch and G. Holroyd. 2004. Canadian Wildlife Service
4999 — 98 Ave., Edmonton, Alberta T6X 2X3 Canada. No
price available.
Seabirds: a natural history. By A. Gaston. 2004. Yale Uni-
versity Press, Box 209040, New Haven, Connecticut 06520.
224 pages, U.S.$45.00.
BOOK REVIEWS
643
allow us to do that. The motivation behind identifying
redundant species is that it would allow us to maximize
the bang per conservation buck. However, cost-benefit
analysis is of very limited value when you cannot quan-
tify either costs or benefits.
TYLER SMITH
155 Avenue Vanguard, Pointe Claire, Quebec H9R 3T4 Canada
*Spiders of Australia. By T. Hawkeswood. 2004. Pensoft
Publishers. Acad. G. Bonchev Str., Bl. 6, 1113 Sofia, Bulgaria.
264 pages, Eur 34.95 Cloth.
*Venomous Reptiles of the Western Hemisphere. By J.
Campbell and W. Lamar. 2004. Cornell University Press,
512 East State Street, Ithaca, New York 14850. 1032 pages
(2 volumes), U.S.$149.95.
*Whales and Dolphins of the World. By M. Simmonds.
2004. The MIT Press, Five Cambridge Centre, Cambridge,
Massachusetts 02142. 160 pages, U.S.$29.95 Cloth.
Botany
Atlas of Plants of Nunavik Villages. By M. Blondeau and
C. Roy. 2004. Editions Multimondes, 930 rue Pouliot, Sainte-
Foy, Quebec G1V 3N9. Can. $34.95.
*Boreal Forest of Canada and Russia. By W. Pruitt and L.
Baskin. 2004. Russian Academy of Science, Leniasky pr.,
33, Moscow V-71, Russia. 163 pages, Price not known.
+Flower Chronicles (reprinted). By E. B. Hollingsworth.
2004 (original 1958). University of Chicago Press, 1427 East
60" Street, Chicago, Illinois 60637. 300 pages, U.S.$16.
*Gathering Moss — A Natural and Cultural History of
Mossess. By R. Kimmerer. 2004. Oregon State University
Press, 102 Adams Hall, Corvallis, Oregan 97331. 176 pages,
U.S.$17.95 Paper.
Environment
*Experimental Approches to Conservation Biology. Edit-
ed by M. Gordon and S. Bariol 2004 University of Califor-
nia Press. 343 pages, not illus. U.S.$ ?
+Rendevous with the Wild — The Boreal Forest. Edited by
J. Raffan (ed). 2004. BostonMills Press — Firefly Books Ltd..
3680 Victoria Park Avenue, Toronto, Ontario M2H 3K1
188 pages, Can. $39.95
Miscellaneous
The New Amateur Naturalist. By Nick Baker .2004. Harper
Collins HarperCollins Publishers Ltd., Bloor Street East,
20" Floor, Toronto, Ontario M4W 1A8. 288 pages, £14.99 —
approx. U.S.$38 Cloth.
Wildlife Spectacles. By Russell A. Mittermeier et al. 2004.
Conservation International 1919 M Street, NW Suite 600,
Washington, DC 20036. 324 pages, £39.50 — approx. U.S.$74.
News and Comment
RENEW. 2004. Recovery of Nationally Endangered Wildlife in Canada. Annual Report (14)
Contents (36 pages): Highlights of 2003-2004 [Of 160
Endangered, 108 Threatened, and 21 Extirpated species on
the November 2003 COSEWIC list: 206 species are wholly or
partially covered by recovery plans (completed or in develop-
ment); 117 species are included in ecosystem or multispecies
recovery, to the extent that their range overlaps with the geo-
graphic area; 53 show stable or increasing population trend.
$30.7 million was expended on recovery (salaries + expenses):
Employment was equivalent to about 142 salaried and 23 vol-
unteer people working full-time; 258 organizations made finan-
cial contributions; 348 organizations participated on recovery
teams] — Report from the Co-Chairs — Figures [4] — Species
Recovery — Responsible Jurisdictions — Financial Contributors
— Funding per Target — Canadian Wildlife Directors Commit-
tee [contacts for species at risk]. The report was produced
by the Canadian Wildlife Service of Environment Canada in
cooperation with the provinces, territories, Fisheries and
Oceans Canada, Parks Canada Agency, Wildlife Management
Boards and many individuals and non-government groups.
Readers are cautioned (inside front cover): “This informa-
tion is carefully reviewed but the Canadian Wildlife Service
disclaims responsibility for the accuracy of the information
contributed”.
Calendar: Endangered Reptiles of Canada 2004 and 2005
For 2004, 12 (one for each month) striking black-and-
white drawings by various artists portray five turtles, 1 lizard
and seven snakes whose surviving Canadian populations are
designated as Endangered (Blue Racer), Threatened (Black
Ratsnake, Eastern Foxsnake, Stinkpot, Eastern Ribbonsnake
[Nova Scotia population], Blanding’s Turtle [Nova Scotia
population], Eastern Massasauga), Special Concern (Wood
Turtle, Five-lined Skink, Eastern Ribbonsnake [Ontario pop-
ulations], Eastern Milksnake, Spotted Turtle), or Under Review
(Prairie Rattlesnake, Blanding’s Turtle [Quebec, Ontario]
populations). For each species there are brief remarks on ap-
pearance, occurrence, habitat and risks to its survival. A 13%
species, the Pacific Pond Turtle is featured on the cover as
designated “extirpated” despite the lack of credible records
that native populations ever existed in Canada with the spec-
ulative remark “There is no biogeographic basis for the Pacific
pond turtle’s range not to have extended in Canada, so cur-
rent efforts to rebuild populations in Washington State may
result in the return of the Pacific pond turtle to southwestern
British Columbia”. The fine artwork was contributed by Joe
Crowly (3), Kathryn Peiman (3), Mandi Eldridge (2), Kevin
Kerr (2), Sonya Amin, Marisa Bonofiglio, and Sarah Ing-
werson.
In the 2005 version the black-and-white art is replaced by
colour photography. The cover head of Western Rattlesnake
(Crotalus oreganus) from British Colombia [sic] is followed
by 7 snakes, 6 freshwater turtles, and one lizard each opposite
a monthly calendar page covering December 2004 to Decem-
ber 2005. Each has additional cameo shots of the same species
and a paragraph that highlights its status and characteristics.
Canadian Species at Risk November 2004
The latest version of the booklet Canadian Species at Risk
prepared after the November 2004 COSEWIC assessment
meeting is available on-line in both PDF and HTML formats
Species represented are Eastern Ratsnake (Elaphe obsoleta)
[= Western Ratsnake Elaphe spiloides of one recent study],
Eastern Foxsnake (Elaphe gloydi) [= Elaphe vulpina gloydi\,
Wood Turtle (Glyptemys insculpta), Spiny Softshell Apalone
spinifera), Stinkpot (Sternotherous odoratus), Massasauga
(Sisturus catenatus), Eastern Hog-nosed Snake (Heterodon
platirhinos), Five-lined Skink (Eumeces fasciatus), Blanding’s
Turtle (Emydoidea blandingi), Spotted Turtle (Clemmys gut-
tata), Racers (Coluber constrictor: 3 subspecies), Snapping
Turtle (Chelydra serpentina), Great Basin Gopher Snake
(Pituophis catenifer deserticola). The back of the calender
features 3 species supposedly extirpated from Canada: Timber
Rattlesnake (Crotalus horridus), Eastern Box Turtle (Terra-
pene carpolina carolina) and Pacific Pond Turtle (Actinemys
marmorata). Not mentioned 1s that the latter two were likely
introductions to Canada. Two other forms are not illustrated
but listed: Pacific Gophersnake (Pituophis catenifer catenifer)
and Pigmy Short-horned Lizard (Phrynosoma douglasii).
These calendars have been produced by “the Brooks lab”
at the Department of Zoology, University of Guelph, Guelph,
Ontario NIG 2W1 Canada; (519) 824-4120 extension 58360;
e-mail brookslab@hotmail.com. The selections for both cal-
endars are based on the latest status designations by the reptile
subcommittee (for which Brooks in chair) of the Committee
on the Status of Endangered Wildlife (COSEWIC). See website:
www.cosewic.ga.ca. All proceeds from sale of calendars goes
to support the Kawartha Turtle Trama Centre in Peterborough,
Ontario, established in 2002 to treat injured native turtles and
release them back in the wild (website: www.kawarthaturtle.
org) and reptile conservation research.
on the web site http://www.cosewic.qc.ca/eng/sct5/indexe.cfm
Paper format of this publication will now be available only
once a year, following the spring assessment meeting.
644
2004
Number 65 (Focus on Australia), October 2004. Contents:
| DAPTFE Seed Grants 2005 — The Impact of Habitat Modifica-
| tion on the Striped Marsh Frog Limnodynastes peronii (Amy
Gye) — Conservation Status of Australian Frogs (Jean-Marc
Hero, Care Morrison, Graeme Gilespie, Dale Roberts. Paul
Horner, David Newell, Ed Meyer, Keith McDonald, Frank
Lemckert, Michhhhael Mahony, Michaelll Tyler, Will Osborne,
Harry Hines, Steve Richards, Conrad Hoskin, Naomi Doak and
Luke Shooo) — New Funds available from the DAPTE (Tim
Halliday) — Alaska Conference Summary (Deborah Rudis —
Froglog Shorts.
| Number 66, December 2004. Contents: New Funds avail-
_ able from the DAPTF (Tim Halliday & Don Church) — U.S.
| Cricket Frog Symposium (Michael Lannoo and Ralph Grundel)
_ — Press Release: Sunburt Frogs a Myth: Pond Scum offers
| Natural Sunscreen (Larry Licht) — Global Amphibian Assess-
/ ment (Simon Stuart, Janice Chanson, Neil Cox and Bruce
| Young) — Atelopus mucubajiensis still survives in Andes of
_ Venezuela. Prelimnary Report (Cesar L. Barrio-Ammmmoros,
| December 2004
Editor’s Note — Thank You from the Meeting Organizer —
_ Overview of the Annual Meeting [Edmonton, Alberta, 24-27
_ September 2004] — 2004 Silver Salamander Award Winners
| [Laura Frits, Steve Brechtel] — 2004 Best Student Presenta-
_ tion [Connie Browne] — Meeting Field Trip: Tyrrell Museum
and Reptile World — Meeting Field Trip: Garter Snake Dens
| Marine Turtle Newsletter (106)
October 2004. 28 pages: EDITORIAL Conceptual Problems
_ with the ICUN Red Listing Assessment for the Green Turtle:
_ Move Over Raine Island — GUEST EDITORIAL: Sea Turtles,
| Red Listing, and the Need for Regional Assessments —
_ ARTICLES: The Trade of Marine Turtles in the Toliara region,
_ Souty West Madagasgar — NOTES: Rat Eradication as Part of
a Green Turtle (Chelonia mydas) Conservation Prograamme
in Indonesia — Fibropapillomatosis and Multiple Fibromas
in a Green Turtle from the South Coast of Pernambucoo State,
Brazil — First Record of a Leatherback Turtle in Syria — MEETING
REPORTS — IUCNMTSG UPDATE — ANNOUNCEMENTS — NEWS &
NEWS AND COMMENT
645
| Froglog: Newsletter of the Declining Amphibian Populations Task Force (65, 66)
Fundacion AndigennA — The Afelopus Initiative: Conserving
Endangered Tropical Andeannn Amphibians (Ariadne Angulo,
Paul Salaman and Jose Vicente Rodriguez — Book Reviews
— Froglog Shorts.
Froglog is the bi-monthly newsletter of the Declining
Amphibian Populations Task Force of The World Conserva-
tion Union (IUCN)/Species Survival Commission (SSC) and
is supported by The Open University, The World Congress
of Herpetology, and Arizona State University. These issues
were edited by John WIlkinson and Jeanne McKay (65) and
Jeanne McKay (66), Department of Biological Sciences, The
Open University, Walton Hall, Milton Keynes, MK7 6AA,
United Kingdom; e-mail: daptf@open.ac.uk. Funding for
Froglog is underwritten by the Detroit Zoological Institute,
P. O. Box 39, Royal Oak, Michigan 48068-0039, USA. Pub-
lication is also supported by Peace Frogs www.peacefrogs.com
and by RANA and the US National Science Foundation grants
DEB-0130273.
_ The Boreal Dip Net/L’Epuisette Boreale: Newsletter of the Canadian Amphibian and Reptile
Conservation Network/Reseau Canadien de Conservation des Amphibiens et des Reptiles 9(1)
— List of Presentations titles at 2004 Annual Meeting —
Attendees of the 2004 Annual Meeting [55]. - Membership
in CARCNET/RECCAR (contact Bruce Pauli, Canadian
Wildlife Service, National Wildlife Research Centre, Carleton
University, Raven Road, Ottawa, Ontario K1A 0H3. Web site:
http://www.carcnet.ca/).
LEGAL BRIEFS — RECENT PUBLICATIONS.
The Marine Turtle Newsletter is edited by Brendan J. Godley
and Annette C. Broderick, Marine Turtle Research Group,
Centre for Ecology and Conservation, University of Exeter
in Cornwall, Tremough Campus, Penryn TR10 9EZ United
Kingdom; e-mail MTN @seaturtle.org; Fax +44 1392 263700.
Subscriptions and donations towards the production of the
MTN can be made online at <http://www.seaturtle.org/mtn/>
or postal mail to Michael Coyne (online Editor) Marine Turtle
Newsletter, 1 Southampton Place, Durham, North Carolina
27705 USA (e-mail: mcoyne @seaturtle.org).
WARS 1983-2002 Special Annual Report Wildlife Accident Reporting and Mitigation
The British Columbia Ministry of Transportation has
published as a CD this report on the Wildlife Accident
Reporting System (WARS) which describes its work and
achievements of the last 20 years as one of the pioneers and
leaders in wildlife accident reporting and mitigation.
The WARS system in used in British Columbia to:
1) quantify the magnitude of wildlife-related vehicle colli-
sions by species
2) identify accident-prone locations and accident trends
3) direct accident mitigation efforts (such as wildlife exclu-
sion fencing and wildlife crossing structures) to problem
locations
4) evaluate the effectiveness of accident risk profiles for
highway corridors
5) develop species-specific accident risk profiles for high-
way corridors
6) advance mitigation efforts to protect rare and endangered
species
7) establish policies and strategies for accident issues and
mitigation iniatives
Copies of the CD can be obtained from Leonard Sielecki,
R. P. Bio, MCIP, Engineering Branch, Environmental Manage-
ment, British Columbia Ministry of Transportation, P.O.
Box 9850, Station Provincial Government, Victoria British
Columbia V8W 9T5 [location address: 4B — 940 Blanshard
Street, Victoria] e-mail: leonard.sielecki@ gems9.gov.be.ca:
telephone (250) 356-2255.
The Ottawa Field-Naturalists’ Club Awards for 2003
IRWIN M. BRopo, CHRISTINE HANRAHAN, BEVERLY MCBRIDE, and SHEILA THOMSON
At the Club’s Annual Soirée, held on 24 April 2004, at St.
Basil’s Church in Ottawa, awards were once again given to
members, and one non-member, who distinguished them-
selves by accomplishments in the field of natural history and
conservation, or by extraordinary activity within the Club.
Daniel Strickland — Honorary Member
The Ottawa Field-Naturalists’ Club takes great pleasure in
honouring Daniel Strickland, not only for his renowned stud-
ies on Gray Jays, but also for the major role that he has played
in fostering an appreciation and enjoyment of natural history
by the general public.
Dan earned his Bachelor of Science degree from the Uni-
versity of Toronto, followed by his Master of Science from the
University of Montreal, choosing as his thesis the life history
of the Gray Jay, which he studied in La Verendrye Park in
Quebec.
For more than thirty years, Dan has been studying and docu-
menting Gray Jay behaviour in Algonquin Park, including the
dynamics of the Gray Jay family unit, its nesting behaviour,
winter survival and food gathering strategies. He is recognized
world-wide as an authority on Gray Jays, and has co-authored
the account on Gray Jays in the prestigious series, The Birds
of North America.
In 1970, Dan became Chief Naturalist for Algonquin Park,
a position he held until his retirement in 2001. Under his
leadership, Algonquin Park’s nature interpretation program
has become renowned continent-wide. Tens of thousands of
park visitors each year enjoy the Park’s nature walks, public
Colin Bowen — George McGee Service Award 2003
When Colin Bowen first joined the Birds Committee 13
years ago, committee members recognized a man who would
do an excellent job at whatever he took on. Since then, he has
put in countless hours of solid, thorough work to keep the
OFNC’s many bird-related materials coherent and accessible.
Colin is extremely well-organized. With his involvement,
information management projects get done effectively. In the
mid-90s the Birds Committee urgently needed to consolidate
and properly archive over thirty years’ worth of bird records
and publications that were scattered in homes around the region.
Colin formed the backbone of a team that worked for almost
three years to bring it all together. He continues to maintain the
archives so that, now, anyone can easily find what they need.
As secretary of the Bird Records Sub-committee, Colin has
a major task on his hands. Sub-committee membership has
changed many times since it first reconstituted itself in the
mid-90s, but Colin has stayed. He receives all rare bird reports
and prepares and redistributes them to committee members
for review. He tracks all debates and decisions at meetings and
prepares the sub-committee’s minutes and reports. On top of
all that, he set up and maintains the extensive cross-referenced
bird records database and photo collection.
A visit to the OFNC’s website will reveal fine examples
of Colin’s efforts to bring Ottawa bird resources to the Internet
As is frequently the case, there isn’t a winner for every poten-
tial award and, this year, the Anne Hanes Natural History
Award was not given. The following citations for those who
did receive an award, however, were read to the members
and guests assembled for the event.
wolf howls, and natural history slide presentations. In addition, |
seventeen self-guided nature trails, dozens of natural history
publications on subjects as diverse as butterflies, mushrooms,
mammals and lichens, as well as a world-class interpretive
centre, all had their genesis under Dan Strickland’s tenure as
Chief Naturalist. In Algonquin Park’s lively and informative
publication, The Raven, Dan shared his broad knowledge and
his fascination with nature in more than 300 articles. The inter-
pretive programs he developed have contributed immeasurably
to the goal of fostering public understanding and appreciation
of nature.
Not the least of Dan Strickland’s legacies is his impact on
a whole generation of young park naturalists, trained under
his guidance, who have moved on to new parks or to new
fields of endeavour, profoundly influenced by Dan’s insight
and his enthusiasm for natural history. In recognition of his
contributions to our knowledge of the natural history of Gray
Jay, as well as his outstanding career in the field of nature
interpretation and public education, it is a pleasure to confer
Honorary Membership in the Ottawa Field-Naturalists’ Club
on Dan Strickland.
and therefore to a broader community. Visitors can see the on-
line. tabular seasonal Ottawa bird checklist, the beautifully
tabulated Christmas Bird Count results or the often-consulted
Ottawa birding site guide, complete with maps.
Colin has volunteered for the Peregrine Falcon Watch and
the Ontario Breeding Bird Atlas. He has helped coordinate
many Christmas and Fall Bird Counts. When out of town bird-
ers contact the club looking for birding information Colin is
one of the generous volunteers who offer hours of their time
to take them to our fine birding spots.
Colin does so much work for the Birds and Bird Records
committees that we wonder how he finds time to do anything
else... but he does. He is a devoted and highly-valued volun-
teer at the Canadian Museum of Nature and, together with his
wife, Pat, were the featured volunteers in the museum’s recent
newsletter. He is a grandfather, an amateur genealogist, a trav-
eller, and is taking up woodworking. He can also fix or build
just about anything.
The OFNC thanks Colin for his tremendous contribution,
and for retiring from his job with Bell Canada so he would
have more time to come and work with us. He has truly never
stopped, and we are proud to present him with this year’s
George McGee Service Award.
646
2004
CLUB AWARDS
647
Daniel Brunton — Conservation Award for Members, 2003
The recipient of the 2003 Conservation Award for Mem-
bers, Daniel Brunton, is an individual well known to mem-
bers of the Ottawa Field-Naturalists’ Club through his active
role in Club affairs for over 20 years, including a term as
President. Indeed, his name is familiar to many residents of
the Ottawa region because he is frequently consulted and
quoted as an expert naturalist and conservationist by the
Ottawa media. Dan has been an ecological consultant since
1979. The award he is receiving today, however, has to do
with only one of his many activities on behalf of wildlife and
wild spaces in the region, namely, his role in the establish-
ment of the RiverKEEPER project for the Ottawa River. Dan
has done almost 200 studies along the river, both as a profes-
sional and amateur naturalist, making him eminently qualified
to take this initiative.
The problems associated with keeping track of the posi-
tive and negative activities that impact the well-being of the
Ottawa River demanded a new approach at coordination.
With federal, two provincial, and dozens of municipal juris-
dictions coming into play, and the high level of pollution af-
fecting this crucial waterway, an initiative with vision was
needed. Dan Brunton, together with some like-minded con-
servationists, particularly George Brown, a Law professor at
the University of Ottawa, and John Almstedt, got together to
tackle the problem and recommended that the United States-
based RiverKEEPER Alliance would provide the best frame-
work within which to proceed. In the spring of 2001, a new
Canadian chapter of RiverKEEPER was established with Dan
as President. Its mission was to oversee the activities and
legislation affecting the health of the river, and to report to the
public. This would be done by hiring a full time KEEPER.
Dan worked tirelessly to secure funding for the project and,
after much work, succeeded in getting a three-year Trillium
grant. In 2002, Laura Van Loon was appointed River KEEPER,
launching the active phase of the project, and, in 2003, Dan
was able to step down as President and allow others to carry
on.
As aresult of Dan Brunton’s efforts and vision, the public
now has a full-time ombudsman to look after the river, advo-
cating compliance with environmental laws, responding to
citizen complaints, identifying problems that affect the river,
and suggesting remedies. We are all beneficiaries of these
efforts and have Dan Brunton to thank for helping to get the
project started. The OFNC is therefore very pleased to pres-
ent him with this year’s Conservation Award for Members.
Friends of the Jock River — Conservation Award for Non-Member, 2003
The OFNC Conservation Award, non-member, is given to
a group or individual who has made an outstanding contribu-
tion in the cause of natural history conservation in the Ottawa
Valley, with particular emphasis on activities within the
Ottawa District.
The Jock River originates in the Goodwood Marsh approx-
imately 50 kilometers west of Ottawa and empties into the
Rideau River after winding through fields, villages, and the
provincially significant Richmond Fen. Many species of fish,
birds, mammals and other wildlife depend on this waterway
for food, breeding sites and shelter. Over the years large areas
of riparian vegetation have been destroyed causing severe
silting of the river, which in turn has had a serious impact on
flora and fauna of the river and its shoreline. The Friends of
the Jock River, a non-profit, volunteer environmental organ-
ization, was formed to look at ways of protecting, restoring,
and enhancing the Jock River and its watershed.
Working with local landowners, government agencies,
recreational users and businesses, the Friends have engaged
in numerous projects aimed at restoring the health of the river’s
ecosystem. The number and types of work they have under-
taken is truly impressive.
The Friends have been planting native trees and shrubs at
various sites along the river and this is helping restore sections
of the river’s shoreline to a more natural forested state. One
example of their work is the Twin Elm restoration project.
This project combines restoration planting with fencing of
Pearl Peterkin -OFNC Member of the Year, 2003
This award is given to a member judged to have made sig-
nificant contributions to the Club during the previous year.
Looking back over the previous recipients of this award, it is
illuminating to see the many and varied services performed
for the Club. From rejuvenating committees, leading an ex-
ceptional number of walks, editing Trail & Landscape, web
site design and maintenance, the list is endless. But one thing
is clear: joining the ranks of these hard-working, dedicated
souls is no small thing.
livestock from the riverbank and installation of a nosepump
to meet their needs. Another important project undertaken
by the group is The Rideau Valley Conservation Authority
(RVCA) Stream Corridor Riparian Vegetation Survey. With
training provided by the Conservation Authority, they col-
lected data according to OMNR stream survey protocols to
determine the ecological health of the river and its shoreline
habitat. These data will become part of the RVCA database,
which, in turn, will be made available to the Friends on CD
to help them plan further riparian restoration projects.
The Friends of the Jock River are involved with issues
affecting the entire Jock River Watershed, thus they have been
monitoring the ecology of the Richmond Conservation Area
and advocating environmentally sound sewage treatment in
Munster.
The group is working on detailed guidelines for all future
projects, including erosion control, buffering run-off, and en-
hancing biodiversity in the watershed. They produce a quar-
terly newsletter, hold regular meetings to which the public
is invited, and maintain an informative website.
For their dedicated, inspired, hard-working and thought-
ful approach to protecting the health of the Jock River and
its watershed, the OFNC is very pleased to give the Friends
of the Jock River this Conservation Award.
[Brian Finch, the present President; Eric Snyder, the
Secretary; and Neil Barrington, the Past President, accepted
the award on behalf of the Friends of the Jock River.]
About ten years ago, it was decided to comb through back
issues of Trail & Landscape and select those issues contain-
ing articles of significant interest and value (for example,
special issues on Butterflies, Reptiles and Amphibians, etc.)
and retain a stockpile of these issues to sell. Since that orig-
inal exercise, however, many more articles of interest have
been published and Pearl Peterkin decided it was time to go
through another selection process. She brought her sugges-
tion to the Education and Publicity Committee who heartily
648
endorsed it. A suggestion was made to bundle together all
issues on a particular topic and sell them as sets. This meant
dealing with the entire 35 year run of Trail & Landscape, find-
ing all the relevant issues, combining them, creating multiple
sets, pricing them, finding adequate storage space at the Fletch-
er Wildlife Garden centre and, of course, transporting the fin-
ished products to the monthly meetings. During the past year,
Pearl was often found ensconced in the back room of the
Fletcher Centre, surrounded by stacks of Trail & Landscape,
creating order out of chaos. She has also spent a lot of time
there organizing the Education and Publicity Committee’s
items so that they are more easily and quickly found.
But it wasn’t only during 2003 that Pearl was active in Club
affairs. Over the 15 years that Pearl has been an OFNC mem-
ber, she has been involved with several club committees. In
the 1990s she volunteered for three years with the Fletcher
Wildlife Garden, becoming one of the stalwarts of this ener-
getic group. In 2000 she took over as Chair of the Education
and Publicity Committee at a time when the committee was
at a low ebb with no leader. During her three years as Chair
she successfully rejuvenated the committee, rounding up new
members, finding judges for the Science Fair (which members
of this Committee have been involved with for some time),
finding volunteers to staff displays at various events, and do-
ing all the other myriad jobs that keep a committee running
THE CANADIAN FIELD-NATURALIST
Vol. 118
smoothly. Once the committee was up and running smoothly,
Pearl decided to step down from that role and concentrate on
other aspects of Education and Publicity committee work.
Many people probably recognize Pearl, even if they don’t
know her name, because she is the friendly face behind the
OFNC sales table at the monthly meetings. It requires a seri-
ous commitment to attend every meeting, and, when people
rely on you to be there, the responsibility is that much greater.
Each month Pearl has to gather together the various sale items
and, with the help of some other volunteers, transport them
to and from the meeting. She also has to keep on top of new
items (such as the new Bird Checklist), and make sure the
stock of regular items is in good supply. This dedication has
paid off, however, because during the last year the sales table
has become a focus of much interest and activity.
In her spare time (what spare time, you may ask), Pearl
is an enthusiastic and long time member of the Rideau Trail
Association. She also volunteers for Bird Studies Canada’s
Loon Survey.
The OFNC is fortunate to have such enthusiastic and com-
mitted volunteers as Pearl Peterkin. For hard work on the Trail
& Landscape project as well as all her involvement with the
Education and Publicity Committee and her dedication to
the club, we are pleased to give Pearl Peterkin the Member
of the Year award for 2003.
. Errata for The Canadian Field Naturalist 118(3)
| Inside front cover bottom: and marine algae, and, still lower, the algae take over. This
Cover. Intertidal zone on rugged rock headland of the Queen — caption and photo (the latter in colour) have previously
Charlotte Islands, British Columbia. Each dominant species —_ appeared as Figure 64, page 77, in Lichens of North America
creates a distinct zone. The white lichen is mainly Coccotrema _ by I. M. Brodo, S. D. Sharnoff, and S. Sharnoff. 2001. Yale
maritimum and the black one is almost entirely Verrucaria University Press, New Haven Connecticut. See article by
maura. Below the Verrucaria is a zone bare of both lichens — Brodo and Sloan on lichen zonation, pages 405-424.
On page 408, Figure 2, the islands were omitted.
132°W 131°W
53°N
53°N
18 Limestone
Island
Moresby
Island
Ep
Gwaii Haanas
National Park Reserve
and Haida Heritage Site
and proposed
National Marine
Conservation Area
52°N
17
Treat Bay
52°N
50 Kilometres
132°W 131°W
FiGuRE 2. Map of the Gwaii Haanas area showing Limestone Island (location 18) to the north and Treat Bay (location 17)
to the south of the insets.
649
Index to Volume 118
Compiled by Leslie Cody
Abies balsamea, 46,95,124,251,268,274,361,388,401,510,530
lasiocarpa, 191,355,584
Abrostola urentis, 541
Acanthopteroctetes bimaculata, 532
Acanthopteroctetidae, 532
Acasis viridata, 539
Acer, 52
negundo, 309
rubrum, 41,96,136,136,251,277,361,508
saccharinum, 41,124,251
saccharum, 361,507
spicatum, 362
Achigan a grande bouche, 523
a petite bouche, 523
Achillea millefolium, 166
Achnatherum richardsonii, 564
Acipenser fulvescens, 523
Acipenseridae, 523
Acleris albicomana, 534
britannia, 534
celiana, 534
emargana, 535
forbesana, 534
logiana, 534
nigrolinea, 535
obligatoria, 534
schalleriana, 534
variana, 534
Acorn, J.H., Review by, 468
Acossus centerensis, 534
populi, 534
Acrobasis betulella, 536
Acrocercops sp., 532
astericola, 532
Acronicta fragilis, 541
grisea, 541
impleta, 541
impressa, 541
innotata, 541
vulpina, 541
Acronictinae, 541
Actaea X ludovici, 612
Actitis macularia, 444
Adalia bipunctata, 312
Adela purpurea, 532
Adelidae, 532
Adelolecia koalensis, 406
Aechmophorus spp., 210
Aepyceros melampus, 185
Aesculus pavia, 612
Aethalura intertexta, 537
Aethes promptana, 535
promptana, 547
Aethusa cynapium, 613
Agabus sp., 431
arcticus, 431
confines, 431
thomsoni, 431
Agelaius phoeniceus, 201
Agelaius phoeniceus, Staging in Eastern South Dakota, Spring
Dispersal Patterns of Red-winged Blackbirds, 201
Aglais milberti, 537
Agonopterix gelidella, 533
Agriphila ruricolella, 536
vulgivagella, 536
Agropyron spp., 400,584
cristatum, 300
pectiniforme, 560
repens, 300
sibiricum, 560
Agrostis sp., 169
filiculmis, 558
gigantea, 560
Aira praecox, 177
Aix sponsa, 131,230
Alaska, Changes in Loon (Gavia spp.) and Red-necked Grebe
(Podiceps grisegena) Populations in the Lower Mata-
nuska-Susitna Valley, 210
Alaska, Interactions of Brown Bears, Ursus arctos, and Gray
Wolves, Canis lupus, at Katmai National Park and Pre-
serve, 247
Alaska, Seed Dispersal by Brown Bears, Ursus arctos, in
Southeastern, 499
Alaska, The Heather Vole, Genus Phenacomys, in, 438
Alberta: Distribution and Status, The Barred Owl, Strix varia
in, 215
Alberta, First Record of Mountain Lions, Puma concolor, in —
Elk Island National Park, 605
Alberta, Including New Provincial Records, Moths and But-
terflies (Lepidoptera) of the Boreal Mixedwood For-
est near Lac La Biche, 530
Alberta, Winter Habitat Use by Wolves, Canis lupus, in Rela- — |
tion to Forest Harvesting in West-central, 368 |
Alca torda, 258
Alces alces, 40,57,61,96,134,185,248,368,.606
Alder, 46,247,268,401
Speckled, 253
Alewife, 319
Alfalfa, 361
Algae, 320
Allium schoenoprasum ssp. sibiricum, 558
Alnus sp., 46,247,401
crispa, 268 i
incana, 253
incana ssp. rugosa, 136
incanatable, 511
rugosa, 268
Alopecurus carolinianus, 170
Alopex lagopus, 602
Alopex lagopus, den by a Polar Bear, Ursus maritimus, Exca-
vation of an Arctic Fox, 602
Alosa pseudoharengus, 319
|
|
|
650 |
4
|
1
— 2004
sapidissima, 77
_ Alucita lalannei, 536
| Alucitidae, 536
Alyssum americanum, 570
| obovatum, 558
| Amandinea coniops, 411
Amaranth, Purplish, 613
Amaranthus blitum, 613
Ambloplites rupestris, 523
_ Amblyptilia pica, 536
| Ambrosia x helenae, 613
Ameiurus nebulosus, 523
Amelanchier sp., 196
alnifolia, 558
| Amirault, D.L., 448
i Amirault, D.L., J. Kierstead, P. MacDonald and L. MacDon-
nell. Sequential Polyandry in Piping Plover, Chara-
drius melodus, Nesting in Eastern Canada, 444
| Ammodytes sp., 262
| Ammophila breviligulata, 444
_ Amphipacifica: Journal of Aquatic Systematic Biology 3(4),
294
| Amphipod, 77
_ Amphipoea americana, 541
| Ampithoe vallida, 79
| Anabeana sp., 320
| Anacampsis conclusella, 534
| Anaplectoides prasina, 543
| pressus, 543
| Anas crecca, 131
| platyrhynchos, 130
| rubripes, 129,268,604
_ Anas rubripes, Broods, Extraordinary Size and Survival of
| American Black Duck, 129
_ Anathix puta, 542
_ Anatis labiculata, 312
_ Ancylis comptana, 535
i diminutana, 535
fuscociliana, 535
laciniana, 535
subaequana, 535
Andres, B.A., 210
Andromeda polifolia, 591
_ Andropogon gerardii, 342
Andropolia contacta, 542
Anguilla rostrata, 523
Anguille d’ Amérique, 523
Anguillidae, 523
Annotated List of the Arctic Marine Fishes of Canada, 156
Anser caerulescens, 602
Antelope, Roan, 185
| Anthoxanthum odoratum, 177
Anthriscus caucalis, 613
Anthyllis vulneraria, 613
| Anticlea multiferata, 539
vasiliata, 539
Apamea cogitata, 541
commoda, 541
Aplectoides condita, 543
Aplodinotus grunniens, 523
Apotomis capreana, 535
deceptana, 535
infida, 535
removana, 535
Apple, 299,361
INDEX TO VOLUME 118
65]
Apple, Crab, 125
Apps, C.D., 191
Arabis caucasica, 558
holboellii var. retrofracta, 558
holboellii var. secunda, 558
Aralia nudicaulis, 46,365
Arbutus menziesii, 174
Arbutus, 174
Arceuthobium americanum, 595
douglasti, 595
laricis, 595
Arceuthobium americanum, on Jack Pine, Pinus banksiana,
Growth in Manitoba, Effects of Lodgepole Pine Dwarf
Mistletoe, 595
Archilochus colubris, 85
Archilochus colubris, Entanglements in Burdock, Arctium
spp., at Delta Marsh, Manitoba, Ruby-throated Hum-
mingbird, 85
Archips argyrospila, 535
Arctiidae, 540
Arctium spp., 85,253,611
lappa, 85
minus, 85
tomentosum, 85
Arctium spp., at Delta Marsh, Manitoba, Ruby-throated Hum-
mingbird, Archilochus colubris, Entanglements in
Burdock, 85
Ardea herodias, 231
Argyresthia sp., 532
abies, 532
conjugella, 532
goedartella, 532
oreasella, 532
pygmaeella, 532
Aristida basiramea, 276
Aristida basiramea Engelm. ex Vasey: A New Addition to
the Flora of Quebec, Forked Three-awned Grass, 276
Armoracia rusticana, 558
Arrow-grass, Marsh, 561
Arrowhead, 318
Artemisia tridentata, 300,584
Arthonia phaeobaea, 410
Arthurs, W.R., Review by, 475
Asaphocrita sp., 533
Ascaphus truei, 447
Ascaphus truei, American Dipper, Cinclus mexicanus, Preys
Upon Larval Tailed Frogs, 446
Ash, 253
Black, 310
Green, 309
Mountain, 362
White, 361,508
Aspen, Quaking, 211,584
Trembling, 46,62,96,218,251,268,274,277,316,342,355
361,370,388,5 15,530
Asphodel, Northern False, 567
Aspicilia caesiocinerea, 411
supertegens, 424
Aspidotis densa, 166
Aster spp., 251
alpinus ssp. vierhapperi, 558
falcatus, 558
Aster, 251
Alpine, 577
Gulf of Saint Lawrence, 105
652
Western Heath, 577
Aster, Symphyotrichum laurentianum, (Fernald) Nesom, Esti-
mation of Seed Bank and Seed Viability of the Gulf
of Saint Lawrence, 105
Atkinson, J., Review by, 283
Atriplex alaskensis, 558
patula, 560
patula sensu, 568
patula var. alaskensis, 568
subspicata, 559
Auklet, Cassin’s, 616
Rhinoceros, 615
Auklet, Cerorhinca monocerata, Fledglings Fly to the Sea
from Their Natal Burrows?, Do Rhinoceros, 615
Austrocedrus chilensis, 132
Autographa ampla, 541
bimaculata, 541
mappa, 541
rubida, 541
Avena sativa, 361,560
Avens, Yellow, 573
Awlwort, 572
Aythya collards, 268
marila, 268
Bacidia alaskensis, 412
Bacidina inundata, 424
Baeus sp., 122
Baeus sp. and Gelis sp., in the Egg Sacs of the Wolf Spiders
Pardosa moesta and Pardosa sternalis (Araneae, Lyco-
sidae) in Southeastern Idaho, Occurrence of Parasi-
toid Wasps, 122
Baillie, S.M., C.D. Wilkerson and T.L. Newbury. “Ashkui”
Vernal Ice-cover Phenomena and Their Ecological
Role in Southern Labrador, 267
Balanus, 406
Ball, P.W., 266
Baneberry, Hybrid, 612
Barbotte brune, 523
Barbue de riviére, 523
Barker, W., Review by, 474
Barley, 361
Barnacle, 406
Bartier, P.M., 77
Basilarchia arthemis, 537
Bass, Largemouth, 113
Basswood, 310
American, 253
Batrachedra praeangusta, 533
Batrachedridae, 533
Bear, 134,443
Barren-ground Grizzly, 239
Black, 41,96,370
Brown, 247,499
Grizzly, 117,239,247,370,603
Polar, 395,602
Bear, Ursus maritimus, Excavation of an Arctic Fox, Alopex
lagopus, den by a Polar, 602
Bears, H. Parasite Prevalence in Dark-eyed Juncos, Junco
hyemalis, Breeding at Different Elevations, 235
Bears, Ursus arctos, and Gray Wolves, Canis lupus, at Katmai
National Park and Preserve, Alaska, Interactions of
Brown, 247
Bears, Ursus arctos, in Southeastern Alaska, Seed Dispersal
by Brown, 499
THE CANADIAN FIELD-NATURALIST
Vol. 118
Bears, Ursus arctos, in the Central Canadian Arctic, Move-
ments of Subadult Male Grizzly, 239
Bears, Ursus maritimus, in the Alaskan Beaufort, Chukchi,
and Northern Bering Seas, Observations of Habitat
Use by Polar, 395
Beaver, 40,129,248,267,606
Eurasian, 434
Beaver, Castor fiber, Collapsing Burrow Causes Death of a
Eurasian, 434
Bedford, R.E., 626
Beech, American, 41,361,507
Beetle, 388
Carabid Intertidal, 79
Colorado Potato, 226
Convergent Lady, 309
Lady, 309
Ladybird, 225
Parenthesis Lady, 309
Seven-spotted Lady, 309
Thirteen-spotted Lady, 309
Transverse, 309
Water, 425
Beetles (Coccinellidae) in Overwintering Sites in Manitoba*,
Density and Survival of Lady, 309
Beetles (Coleoptera: Adephaga: Dytiscidae, Gyrinidae) Col-
lected Along the Horton and Thelon Rivers in the Arc-
tic Central Barrens of Canada, Predaceous Water, 425
Beetles (Coleoptera: Coccinellidae) in Prince Edward Island,
Use of Eelgrass, Zostera marina, Wrack by Three
Species of Ladybird, 225
Bennett, B., 558
Bentgrass, 169
Berberis spp., 132
Beringer, J., 185
Berube, D.K.A., 386
Besma quercivoraria, 538
Betula, 52
alleghaniensis, 41,361,508
glandulosa, 591
papyrifera, 41,46,95,136,211,251,268,274,355,388,510,
530
populifolia, 277
Bibarrambla allenella, 533
Bidens sp., 180
Bigler, L.L., 65
Birch, Dwarf, 591
Gray, 277
Paper, 211,268,355
White, 41,46,95,251,274,388,515,530
Yellow, 41,361,507
Bird rape, 571
Bison bison, 115,606
Bison, 115,606
Bison, Bison bison, Toward Elk, Cervus elaphus, and Wolves,
Canis lupus, Unusual Behavior by, 115
Bison bison, Toward Elk, Cervus elaphus, and Wolves, Canis
lupus, Unusual Behavior by Bison, 115
Biston betularia, 537
Bistort, Alpine, 591
Bittercress, Alpine, 571
Narrow-leaved, 613
Blackbird, Red-winged, 201
Yellow-headed, 207
Blackbirds, Agelaius phoeniceus, Staging in Eastern South
Dakota, Spring Dispersal Patterns of Red-winged, 201
i
— 2004
Bladderwort, Lesser, 576
| Blarina brevicauda, 402
Blastodacna curvilineella, 533
_ Bleptina caradrinalis, 540
Blueberry, 251
Lowbush, 195
Tall, 575
Velvet Leaf, 195
| Blueberry, Vaccinium angustifolium, and Velvet Leaf Blue-
berry, Vaccinium myrtilloides, Production in Eastern
Ontario, Effect of Fire Intensity and Depth of Burn
on Lowbush, 195
Blueberry, Vaccinium myrtilloides, Production in Eastern
Ontario, Effect of Fire Intensity and Depth of Burn
on Lowbush Blueberry, Vaccinium angustifolium,
and Velvet Leaf, 195
_ Bluegill, 318
| Bluegrass, 300
Kentucky, 176
Sandberg, 564
Bluestem, Big, 342
Bobcat, 40
Bog-rosemary, Dwarf, 591
| Bombycilla cedrorum, 232
Bonasa umbellus, 41,232
_ Bondia crescentella, 536
_ Boreal Dip Net/L’Epuisette Boreal: Newsletter of the Canadian
| Amphibian and Reptile Conservation Network — Re-
seau Canadien de Conservation des Amphbiens et des
| Reptiles, The, 155,484,645
- Botrychium sp., 365
| Bousfield, E.L, 626
| Bowen, K.D. Frequency of Tail Breakage of the Northern
Watersnake, Nerodia sipedon sipedon, 435
| Bowerbankia gracilis, 79
Brachylomia algens, 542
discinigra, 542
, Brachythecium spp., 253
| Bracken, 253
Branta canadensis, 268,602
Brassica rapa, 560
Braya glabella, 550
humilis, 550
pilosa, 550
purpurascens, 550
thorild-wulffii, 550
Braya, Pilose, 550
Braya, Braya pilosa Hooker (Cruciferae; Brassicaceae), an
Enigmatic Endemic of Arctic Canada, Pilose, 550
Braya pilosa Hooker (Cruciferae; Brassicaceae), an Enigmat-
ic Endemic of Arctic Canada, Pilose Braya, 550
Brisson, J. Forked Three-awned Grass, Aristida basiramea
Engelm. ex Vasey: A New Addition to the Flora of
Quebec, 276
Bristlegrass, Green, 564
British Columbia, Bird Communities of the Garry Oak Habitat
in Southwestern, 376
British Columbia, Introduced Marine Species in the Haida
Gwaii (Queen Charlotte Islands) Region, 77
British Columbia, Lichen Zonation on Coastal Rocks in Gwati
Haanas National Park Reserve, Haida Gwaii (Queen
Charlotte Islands), 405
British Columbia, 1972-2002, Sea Otter, Enhydra lutris, Sight-
ings off Haida Gwaii/Queen Charlotte Islands, 270
INDEX TO VOLUME 118
653
British Columbia, Observations of Above-Surface Littoral For-
aging in Two Sea Ducks, Barrow’s Goldeneye, Buceph-
ala islandica, and Surf Scoter, Melanitta perspicillata,
in Coastal Southwestern, 264
British Columbia waters: a reassessment, Status of marine
turtles in, 72
Brodo, I.M. and N.A. Sloan. Lichen Zonation on Coastal
Rocks in Gwaii Haanas National Park Reserve, Haida
Gwaii (Queen Charlotte Islands), British Columbia,
405
Brome, Barren, 176
California, 174
Downy, 300
Rip-gut, 174
Smooth, 300,342,562
Soft, 174
Bromus spp., 175
carinatus, 174
ciliatus, 559
hordeaceus, 174
inermis, 300,342,560
rigidus, 174
sterilis, 176
tectorum, 174,300
Brook, R.K., 602
Broom, Scotch, 177
Brunton, D.F. Origins and History of The Ottawa Field-
Naturalists’ Club, 1
Brush, Big Sage, 584
Bryotropha sp., 534
Bryozoan, 79
Bubo virginianus, 222,273
Bucculatricidae, 532
Bucculatrix sp., 532
canadensisella, 532
Bucephala clangula, 267,604
islandica, 264
Bucephala islandica, and Surf Scoter, Melanitta perspicillata,
in Coastal Southwestern British Columbia, Observa-
tions of Above-Surface Littoral Foraging in Two Sea
Ducks, Barrow’s Goldeneye, 264
Buckeye, Red, 612
Budworm, Spruce, 361
Bulrush, 318
Bunchberry, 46
Bunting, Indigo, 232
Bur-chervil, 613
Burdock, 85,253,611
Common, 85
Burdock, Arctium spp., at Delta Marsh, Manitoba, Ruby-
throated Hummingbird, Archilochus colubris, Entan-
glements in, 85
Burnett, D., Review by, 151
Burrows, F.G.M., 95
Buteo lagopus, 268
Buttercup, Western, 570
Butterflies (Lepidoptera) of the Boreal Mixedwood Forest
near Lac La Biche, Alberta, Including New Provin-
cial Records, Moths and, 530
Butterfly, 388
Buttons, Brass, 169
Cabera erythemaria, 538
variolaria, 538
Caenurgina crassiuscula, 541
654
Calafate, 132
Calamagrostis canadensis, 591
Calendar: Endangered Reptiles of Canada 2004 and 2005,
644
Callitriche anceps, 559
Callizzia amorata, 539
Caloplaca, 420
chlorina, 424
citrina, 411
exsecuta, 420
flavogranulosa, 411
inconspecta, 406
litoricola, 406
marina, 420
rosei, 411
verruculifera, 411
Caloptilia alnivorella, 532
anthobaphes, 532
betulivora, 532
canadensisella, 532
coroniella, 532
stigmatella, 532
Caloreas occidentella, 536
Camas, Common, 175
Great, 175
Camassia leichtlinii, 175
quamash, 175
Camelina sativa, 558
Campaea perlata, 538
Campbell, B., 521
Campion, Bladder, 569
Canachites canadensis, 41
Canada, Conservation Evaluation of Howell’s Triteleia, Tri-
teleia howellii, an Endangered Lily in, 174
Canada, Conservation Evaluation of Lemmon’s Holly Fern,
Polystichum lemmonii, a Threatened Fern in, 164
Canada, Conservation Evaluation of Small-flowered Lipo-
carpha, Lipocarpha micrantha (Cyperaceae), in, 179
Canada, Conservation Evaluation of the Pacific Population
of Tall Woolly-heads, Psilocarphus elatior, an Endan-
gered Herb in, 169
Canada, Hybridization between a Green Turtle, Chelonia
mydas, and Loggerhead Turtle, Caretta caretta, and
the First Record of a Green Turtle in Atlantic, 579
Canada, Pilose Braya, Braya pilosa Hooker (Cruciferae; Bras-
sicaceae), an Enigmatic Endemic of Arctic, 550
Canada, Predaceous Water Beetles (Coleoptera: Adephaga:
Dytiscidae, Gyrinidae) Collected Along the Horton
and Thelon Rivers in the Arctic Central Barrens of,
425
Canada, Sequential Polyandry in Piping Plover, Charadrius
melodus, Nesting in Eastern, 444
Canada, Stranding of a Pygmy Sperm Whale, Kogia brevi-
ceps, in the Northern Gulf of St. Lawrence, 495
Canada 2004 and 2005, Calendar: Endangered Reptiles of,
644
Canadian Arctic, Movements of Subadult Male Grizzly Bears,
Ursus arctos, in the Central, 239
Canadian Arctic Islands Using Morphology and Chloroplast
DNA Data, A Systematic Analysis of the Alpine Saxi-
frage Complex (Saxifragaceae) in the, 326
Canadian Field-Naturalist, Advice for Contributors to The,
158,294,494
THE CANADIAN FIELD-NATURALIST
Vol. 118
Canadian Rocky Mountains, Predation on Two Mule Deer,
Odocoileus hemionus, by a Canada Lynx, Lynx
canadensis, in the Southern, 191
Canadian Species at Risk, 484,644
Candelariella sp., 411
Canis domesticus, 247
latrans, 41,96,116,243,278,306,341,368,370,606,608
lupus, 42,57,61,95,115,127,134,194,247,278,350,361,
368,603,608
lupus lycaon, 608
rufus, 608
Canis latrans, Evidence for the Use of Vocalization to Coor-
dinate the Killing of a White-Tailed Deer, Odocoileus
virginianus, by Coyotes, 278
Canis latrans, in a Heterogeneous Environment, The Influ-
ence of Prey Availability and Vegetation Character-
istics on Scent Station Visitation Rates of Coyotes,
341
Canis latrans, Severe Chronic Neck Injury Caused by a Snare
in a Coyote, 243
Canis lupus, at Katmai National Park and Preserve, Alaska,
Interactions of Brown Bears, Ursus arctos, and Gray
Wolves, 247
Canis lupus, in and near Pukaskwa National Park, Ontario,
Demographic patterns and limitations of Grey Wolves,
95
Canis lupus, in Relation to Forest Harvesting in West-central
Alberta, Winter Habitat Use by Wolves, 368
Canis lupus, Pack Density, Record High Wolf, 127
Canis lupus, South of the St. Lawrence River in Over 100
Years, First Confirmed Occurrence of a Wolf, 608
Canis lupus, Unusual Behavior by Bison, Bison bison,
Toward Elk, Cervus elaphus, and Wolves, 115
Capelin, 262
Capreolus capreolus, 134
Caprimulgus vociferus, 230
Capsella bursa-pastoris, 560
Carcinus maenas, 82
Cardamine bellidifolia, 559
impatiens, 613
Carduelis pinus, 378
tristis, 378
Caretta caretta, 579
Caretta caretta, and the First Record of a Green Turtle in At-
lantic Canada, Hybridization between a Green Turtle,
Chelonia mydas, and Loggerhead Turtle, 579
Carex spp., 247,318,400,501
albo-nigra, 559
aquatilis, 591
athrostachya, 169,559
atrosquama, 559
capillaris ssp. chlorostachys, 559
crawfordii, 559
eleusinoides, 559
feta, 170
foenea, 266,559
glareosa, 266
hoodii, 266
houghtonii, 197
lapponica, 266
limosa, 559,591
loliacea, 559
magellanica ssp. irrigua, 266
marina, 266
obtusata, 559
pachystachya, 266,559
pellita, 559
petasata, 559
praegracilis, 559
rossii, 559
stylosa, 558
supina ssp. spaniocarpa, 559
sychnocephala, 559
i} unilateralis, 169
viridula, 559
Caribou, 39,192,241,362,602
Woodland, 57,61,96,119,368
‘Caribou, Rangifer tarandus caribou, in Saskatchewan, Mor-
phology of Female Woodland, 119
: Caripeta divisata, 538
| Carpiodes cyprinus, 523
_ Carpodacus purpureus, 378
Carposinidae, 536
Carter, B. A Tribute to Thomas Henry Manning (1911-1998),
618
Carterocephalus palaemon, 537
Case, R., 239
Cassiope tetragona ssp. saximontana, 559
| Castor canadensis, 40,129,136,248,267,606
fiber, 434
| Castor fiber, Collapsing Burrow Causes Death of a Eurasian
Beaver, 434
Castors, 136
Caswell, P., 558
-Catharus fuscescens, 232
| Catillaria chalybeia, 408
| Catocala briseis, 541
relicta, 541
semirelicta, 541
unijuga, 541
Catocalinae, 541
Catostomidae, 521
Catostomus spp., 521
commersoni, 319,523
| Cattail, 253,318
Common, 545,561
| Cedar, Eastern White, 95,253,361,508
Yellow, 159
Centaurea diffusa, 300
Centipede, 389
Centrarchidae, 523
Cephalophus monticola, 185
| Cepphus grylle, 258
Cerastium arvense, 559
| Cerorhinca monocerata, 615
| Cerorhinca monocerata, Fledglings Fly to the Sea from Their
Natal Burrows?, Do Rhinoceros Auklet, 615
| Certhia americana, 384
Cervus canadensis, 606
elaphus, 115,132,185,368
elaphus nelsoni, 132
nippon, 185
Cervus elaphus, and Wolves, Canis lupus, Unusual Behavior
by Bison, Bison bison, Toward Elk, 115
Cervus elaphus, in Patagonia, Observations of Interactions
between Puma, Puma concolor, and Introduced Euro-
pean Red Deer, 132
Chamaecyparis nootkatensis, 159
Chamaerhodos erecta ssp. nuttallii, 559
| Chapdelaine, G., 256
INDEX TO VOLUME 118
655
Chapleau, F., 521
Charadrius alexandrinus, 445
melodus, 444,448
vociferus, 445
Charadrius melodus, egg viability after seawater immersion,
Piping Plover, 448
Charadrius melodus, Nesting in Eastern Canada, Sequential
Polyandry in Piping Plover, 444
Charlock, 572
Chat-fou liséré, 523
Chelonia mydas, 72,579,611
Chelonia mydas, and Loggerhead Turtle, Caretta caretta, and
the First Record of a Green Turtle in Atlantic Canada,
Hybridization between a Green Turtle, 579
Chelydra serpentina, 610
Chelydra serpentina?, Is Cost of Locomotion the Reason for
Prolonged Nesting Forays of Snapping Turtles, 610
Chenopodium capitatum, 559
Cherry, Choke, 253,362
Sand, 196
Chevalier blanc, 523
de riviere, 521
doré 526
rouge, 523
Chickadee, Black-capped, 232
Boreal, 48
Chestnut-backed, 378
Chickweed, Field, 569
Chilocorus stigma, 312
Chionodes continuella, 534
lugubrella, 534
mediofuscella, 534
occlusus, 534
psilopterus, 534
sattleri, 534
terminimaculella, 534
Chipmunk, Yellow-pine, 299
Chipmunks, Tamias amoenus, in Old Field and Orchard Habi-
tats, Population Dynamics of Deer Mice, Peromyscus
maniculatus, and Yellow-pine, 299
Chondrus crispus, 226
Chorda filum, 226
Chordaria flagelliformis, 226
Choreutidae, 536
Choreutis diana, 536
Choristoneura albaniana, 535
conflictana, 535
fumiferana, 361,535
rosaceana, 535
Choristostigma plumbosignale, 537
Chrysanympha formosa, 541
Chytolita petrealis, 540
Chytonix palliatricula, 542
Cicuta maculata vat. angustifolia, 559
Cinclus mexicanus, 443,446
Cinclus mexicanus, Preys Upon Larval Tailed Frogs, Asca-
phus truei, American Dipper, 446
Cinquefoil, Tall, 573
Ciona intestinalis, 79
Ciprés, 132
Cirsium muticum, 253
Cirtwill, A., 604
Cladara atroliturata,
limitaria, 539
Cladina rangiferina,
539
591
656
Clam, Butter, 77
Manila, 78
Native Littleneck, 77
Soft-shell, 78
Clangula hyemalis, 604
Clangula hyemalis, Two Great Black-backed Gulls, Larus
marinus, Kill Male Longtailed Duck, 604
Clayburn, J.K., 615
Claytonia megarrhiza, 558
Cleavers, 175
Clemensia albata, 540
Clepsis clemensiana, 535
melaleucana, 535
persicana, 535
virescana, 535
Clintonia borealis, 362
Clintonia, Yellow, 362
Cliostomum griffithii, 424
Clostera albosigma, 540
apicalis, 540
strigosa, 540
Clover, 253,362
Red, 574
Cluff, H.D., 239
Coad, B.W., Reviews by, 281,282,469
Cobb, L.M. and V.A. Cobb. Occurrence of Parasitoid Wasps,
Baeus sp. and Gelis sp., in the Egg Sacs of the Wolf
Spiders Pardosa moesta and Pardosa sternalis (Ara-
neae, Lycosidae) in Southeastern Idaho, 122
Cobb, V.A., 122
Coccinella septempunctata, 225,309
transversoguttata, 310
transversoguttata richardsonii, 309
Coccotrema cucurbitula, 420
maritimum, 406
Cochylis nana, 535
Cody, W.J., C.E. Kennedy, B. Bennett, and P. Caswell. New
Records of Vascular Plants in the Yukon Territory VI,
558
Cody, W.J., Reviews by, 147,289,476
Coenophila opacifrons, 543
Coir6n Amargo, 132
Dulce, 132
Colaptes auratus, 358
Coleophora sp., 533
alnifoliae, 533
comptoniella, 533
corylifoliella, 533
dextrella, 533
duplicis, 533
glaucicolella, 533
mayrella, 533
mcedunnoughiella, 533
persimplexella, 533
pruniella, 533
rosaevorella, 533
Coleophoridae, 533
Coleotechnites atrupictella, 534
blastivora, 534
florae, 534
piceaella, 534
Collema fecundum, 411
novozelandicum, 420
Colletia spinosissima, 132
Comptonia peregrina, 196
THE CANADIAN FIELD-NATURALIST
Vol. 118
Comtois, A., F. Chapleau, C.B. Renaud, H. Fournier, B. Camp-)
bell, et R. Pariseau. Inventaire printanier d’une frayére
multispécifique: l’ichtyofaune des rapides de la riv-
iére Gatineau, Québec, 521
Contopus cooperi, 378
virens, 232
Cook, E.R., Reviews by, 138,141,467
Cook, J.A., 438
Copepod, 77
Corispermum hyssopifolium sensu, 568
ochotense var. alaskanum, 558
Cormorant, Double-crested, 257
Great, 257
Corn, 253
Cornus canadensis, 46
racemosa, 342
stolonifera, 253
Coronopus didymus, 613
Corophium acherusicum, 77
Corvus brachyrhynchos, 232
caurinus, 378
corax, 273
Corylus cornuta, 197,251
COSEWIC Assessment Results November 2003, 155
Cosmopterigidae, 534
Cossidae, 534
Cotton-grass, Short-anthered, 566
Cottontail, Eastern, 342
Cottonwood, Black, 211,355
Plains, 309
Cottus bairdi, 323
cognatus, 323
Cotula coronopifolia, 169
Couette, 523
Cougar, 159,370
Cougars, Puma concolor vancouverensis, Morphology and
Population Characteristics of Vancouver Island, 159
Couleuvre brune, 136
mince, 135
rayée de l’est, 135
Couleuvre mince, Thamnophis sauritus septentrionalis, au
Québec, Premiéres mentions de la, 135
Cowbird, Brown-headed, 378
Coyote, 41,96,116,243,278,306,341,368,606,608
Western, 608
Coyote, Canis latrans, Severe Chronic Neck Injury Caused by
a Snare in a, 243
Coyotes, Canis latrans, Evidence for the Use of Vocalization
to Coordinate the Killing of a White-Tailed Deer,
Odocoileus virginianus, by, 278
Coyotes, Canis latrans, in a Heterogeneous Environment,
The Influence of Prey Availability and Vegetation
Characteristics on Scent Station Visitation Rates of,
341
Crab, European Green, 82
Crambidae, 536
Crambus leachellus, 536
perlellus, 536
Crapet arlequin, 523
de roche, 523
soleil, 523
Crassostrea gigas, 77
Crataegus sp., 365
Creeper, Brown, 378
Cress, Penny, 573
ii)
|
2004
| Créte, M., 360
| Crow, American, 232
Northwestern, 378
| Cryptocala acadiensis, 543
| Cryptococcus spp., 41
Cryptogramma crispa vat. acrostichoides, 559
Cryptosula pallasiana, 79
Cuculliinae, 541
Cudweed, Lowland, 169
/ Cumming, E.E. Habitat Segregation Among Songbirds in
Old-Growth Boreal Mixedwood Forest, 45
Cyanocitta cristata, 231
Cyclophora pendulinaria, 538
Cydia flexiloqua, 536
populana, 536
| Cynosurus echinatus, 176
Cyperus sp., 180
squarrosus, 179
Cyperus, Awned, 179
| Cyprinidae, 523
Cytisus scoparius, 177
Dactylis glomerata, 174,300
‘Daigle, C., M. Créte, L. Lesage, J.-P. Ouellet, and J. Huot.
Summer Diet of Two White-tailed Deer, Odocoileus
virginianus, Populations Living at Low and High Den-
sity in Southern Québec, 360
| Danthonia californica, 169
spicata, 277
_| Daoust, P.-Y. and P.H. Nicholson. Severe Chronic Neck Injury
Caused by a Snare in a Coyote, Canis latrans, 243
| Darbyshire, S.J. The Northern True Katydid, Pterophylla
camellifolia (Orthoptera: Pseudophyllidae), at Ottawa,
Ontario, 124
) Darter, Iowa, 319
Johnny, 319
Rainbow, 319
| Dasychira plagiata, 540
vagans, 540
Daucus carota, 342
Deer, 368
Columbia Black-tailed, 162
European Red, 132
Mule, 132,162,185,191,370,606
Red, 185
Roe, 134
Sika, 185
White-tailed, 40,96, 127,185,278,360,370,606
| Deer, Cervus elaphus, in Patagonia, Observations of Inter-
actions between Puma, Puma concolor, and Introduced
European Red, 132
Odocoileus hemionus, by a Canada Lynx, Lynx cana-
densis, in the Southern Canadian Rocky Mountains,
| Predation on Two Mule, 191
Deer, Odocoileus virginianus, by Coyotes, Canis latrans,
| Deer,
Evidence for the Use of Vocalization to Coordinate
the Killing of a White-Tailed, 278
Odocoileus virginianus, Populations Living at Low
and High Density in Southern Québec, Summer Diet
of Two White-tailed, 360
| Deer,
| Deer, Odocoileus virginianus, with Medetomidine and Ket-
amine, and Antagonism with Atipamezole, Immobi-
lization of Clover-trapped White-tailed, 185
| Dendroica castanea, 48
cerulea, 229
INDEX TO VOLUME 118
657
coronata, 48,86,232,378
fusca, 48
magnolia, 48
pensylvanica, 232
petechia, 86,232
virens, 48,232
Dendroica cerulea Management on Eastern Ontario Bird
Species, Predicting the Effects of Cerulean Warbler,
229
Depressariodes ciniflonella, 533
Dermacentor variabilis, 42
Dermochelys coriacea, 72,579
Deschampsia brevifolia, 559
Descurainia incisa vat. incisa, 559
Desmognathus ochrophaeus, 136
de Solla, S.R. and K.J. Fernie. Is Cost of Locomotion the Rea-
son for Prolonged Nesting Forays of Snapping Turtles,
Chelydra serpentina?, 610
Desroches, J.-F. et I. Picard. Extension de I’ aire de distribution
connue de la Musaraigne fuligineuse, Sorex fumeus,
dans le nord-est du Québec, 441
Desroches, J.-F. et R. Lapar. Premiéres mentions de la Cou-
leuvre mince, Thamnophis sauritus septentrionalis,
au Québec, 135
Diachrysia aereoides, 541
Diarsia dislocata, 542
rosaria, 542
rubifera, 542
Dibb, A., 191
Dicamptodon copei, 448
ensatus, 448
Dichomeris levisella, 534
Dicrostonyx hudsonius, 403
richardsoni, 403
Digrammia rippertaria, 537
Dioryctria reniculelloides, 536
Dipper, American, 443,446
Dipper, Cinclus mexicanus, Preys Upon Larval Tailed Frogs,
Ascaphus truei, American, 446
Dock, Curled, 568
Dodecatheon hendersonii, 175
hendersonii ssp. hendersonii, 175
Dogtail, Hedgehog, 176
Dogwood, 253
Gray, 342
Dolichomia thymetusalis, 536
Doré jaune, 523
noir, 523
Dorosoma cepedianum, 318
Douglas, G.W., 179
Douglas, G.W. Conservation Evaluation of Lemmon’s Holly
Fern, Polystichum lemmonii, a Threatened Fern in
Canada, 164
Douglas, G.W. and J.L. Penny. Conservation Evaluation of
Howell’s Triteleia, Triteleia howellii, an Endangered
Lily in Canada, 174
Douglas, G.W. and J.M. Illingworth. Conservation Evalua-
tion of the Pacific Population of Tall Woolly-heads,
Psilocarphus elatior, an Endangered Herb in Canada,
169
Douglasia alaskana, 559
arctica, 558
Dowsley, M. and A. Cirtwill. Two Great Black-backed Gulls,
Larus marinus, Kill Male Longtailed Duck, Clangu-
la hyemalis, 604
658
Draba aurea, 559
corymbosa, 550,559
crassifolia, 559
glabella, 559
nemorosa, 559
ogilviensis, 559
palanderiana, 559
porsildii, 559
stenoloba, 559
Draba, Golden, 571
Drepana arcuata, 537
bilineata, 537
Drepanidae, 537
Dryas hookeriana, 559
Duchesne, L.C. and S. Wetzel. Effect of Fire Intensity and
Depth of Burn on Lowbush Blueberry, Vaccinium
angustifolium, and Velvet Leaf Blueberry, Vaccinium
myrtilloides, Production in Eastern Ontario, 195
Duck, American Black, 129,604
Black, 268
Longtailed, 604
Ring-necked, 268
Ruddy, 604
Wood, 131,230
Duck, Anas rubripes, Broods, Extraordinary Size and Survival
of American Black, 129
Duck, Clangula hyemalis, Two Great Black-backed Gulls,
Larus marinus, Kill Male Longtailed, 604
Ducks, Barrow’s Goldeneye, Bucephala islandica, and Surf
Scoter, Melanitta perspicillata, in Coastal South-
western British Columbia, Observations of Above-
Surface Littoral Foraging in Two Sea, 264
Duiker, Blue, 185
Dulse, 226
Dutton, P.H., 579
Dyke, A.S., D.A. Hodgson, E.L. Bousfield, and R.E. Bedford.
A Tribute to Victor Kent Prest (1913-2003), 626
Dysstroma citrata, 538
formosa, 538
hersiliata, 538
truncata, 538
walkerata, 538
Eagle, Bald, 267
Earthworm, 388
Ecliptopera silaceata, 538
Ectropis crepuscularia, 537
Editor’s Report for Volume 117 (2003), 296
Eelgrass, 225,318
Eelgrass, Zostera marina, Wrack by Three Species of Lady-
bird Beetles (Coleoptera: Coccinellidae) in Prince
Edward Island, Use of, 225
Egira dolosa, 542
Eider, Common, 258
Eilema bicolor, 540
Elachista sp., 533
adempta, 533
albicapitella, 533
Elachistidae, 533
Elaphria alapallida, 542
Elderberry, Red, 577
Eleocharis elliptica, 266
uniglumis, 559
Elk, 115,368
American, 132,606
THE CANADIAN FIELD-NATURALIST
Vol. 118
Elk, Cervus elaphus, and Wolves, Canis lupus, Unusual
Behavior by Bison, Bison bison, Toward, 115
Elm, American, 310,508
Elodea canadensis, 318
Elymus alaskanus ssp. alaskanus, 559
glaucus, 559
macrourus, 559
repens, 253
spicatus, 559
trachycaulus ssp. andinus, 559
Elytrigia intermedia, 560
Empidonax difficilis, 378
minimus, 86,232
Emydura macquarii, 610
Enargia decolor, 542
infumata, 542
Engeman, R.M., 201
Enhydra lutris, 270
Enhydra lutris, Sightings off Haida Gwaii/Queen Charlotte
Islands, British Columbia, 1972-2002, Sea Otter, 270 ©
Ennominae, 537
Ennomos magnaria, 538
Eosphoropteryx thyatyroides, 541
Ephebe lanata, 424
Epilobium angustifolium, 253,365
Epinotia castaneana, 536
criddleana, 536
lindana, 536
momonana, 536
nisella, 536
rectiplicana, 536
solandriana, 536
transmissana, 536
trigonella, 536
Epirrhoe alternata, 539
Epirrita autumnata, 539
Epp, B. and J.C. Tardif. Effects of Lodgepole Pine Dwarf
Mistletoe, Arceuthobium americanum, on Jack Pine,
Pinus banksiana, Growth in Manitoba, 595
Equisetum spp., 46
variegatum, 591
Equus cabalus, 370
Erannis tiliaria, 538
Erethizon dorsatum, 607
Eretmochelys imbricata, 580
Erickson, W.R. Bird Communities of the Garry Oak Habitat
in Southwestern British Columbia, 376
Erigeron caespitosus, 559
hyperboreus, 559
Eriophorum brachyantherum, 559
Eritrichium aretioides, 559
chamissonis, 559
Ermine, 243
Ernst, J., 56,61
Errata for The Canadian Field-Naturalist 118(3), 649
Erratum Canadian Field-Naturalist 118(2), 485
Esocidae, 523
Esox lucius, 523
masquinongy, 523
Espino Negro, 132
Esturgeon jaune, 523
Etheostoma caeruleum, 319
exile, 319
nigrum, 319,523
olmstedi, 523
2004
|
Eubaphe mendica, 539
Euchlaena marginaria, 538
obtusaria, 538
| tigrinaria, 538
_Eudonia albertalis, 536
| Eueretagrotis perattenta, 543
_Euhyponomeutoides gracilariella, 532
Eulia ministrana, 535
| Eulithis explanata, 538
propulsata, 538
| xylina, 538
Eulogia ochrifrontella, 536
_Euonymus fortunei, 614
| Euphrasia subarctica, 559
| Euphyia intermediata, 539
| Eupithecia anticaria, 539
i| assimilata, 539
columbiata, 539
i| perfusca, 539
ravocostaliata, 539
satyrata, 539
stellata, 539
| subfuscata, 539
| Euplexia benesimilis, 542
| Eurois astricta, 543
i occulta, 543
Eustrotiinae, 541
Euthyatira pudens, 537
| Everes amyntula, 537
Everett, K.T. and K.A. Otter. Presence of Cavities in Snags
Retained in Forest Cutblocks: Do Management Poli-
i cies Promote Species Retention?, 354
| | Evergestis pallidata, 537
Fagus, 52
i grandifolia, 41,361,507
Falseflax, 571
| Feathermoss, Red-stemmed, 591
| Felis concolor, 370
| Ferguson, C., 225
Ferguson, S.H. and D.K.A. Berube. Invertebrate Diversity
under Artificial Cover in Relation to Boreal Forest
Habitat Characteristics, 386
“Fern, 159
| Bracken, 196,251
Kruckeberg’s Holly, 164
| Lemmon’s Holly, 164
Mountain Holly, 164
| Nahanni Oak, 560
| Ostrich, 46,253
| Sensitive, 253
Sweet, 196
| Fern, Polystichum lemmonii, a Threatened Fern in Canada,
Conservation Evaluation of Lemmon’s Holly, 164
| Fernie, K.J., 610
| Fescue, Rocky Mountain, 563
i Short-leaf, 562
. Festuca brachyphylla, 559
pallescens, 132
| richardsonii, 559
saximontana, 559
Filatima abactella, 534
_ Finch, Purple, 378
Fir, Balsam, 46,95,251,268,274,361,388,401,514,530
Douglas, 159,355,376,584,595
|
i
|
INDEX TO VOLUME 118
659
Sub-alpine, 191,355,584
Fireweed, 253
Fisher, 56,96,583
Flicker, Common, 379
Northern, 358,378
Flounder, Starry, 248
Flueck, W.T. Observations of Interactions between Puma,
Puma concolor, and Introduced European Red Deer,
Cervus elaphus, in Patagonia, 132
Flycatcher, Least, 232
Olive-sided, 378
Pacific-coast, 378
Pacific-slope, 378
Least, 86
Fool’s-parsley, 613
Forget-me-not, 576
Forshner, S.A., P.C. Paquet, F.G.M. Burrows, G.K. Neale,
K.D. Wade and W.M. Samuel. Demographic patterns
and limitations of Grey Wolves, Canis lupus, in and
near Pukaskwa National Park, Ontario, 95
Fouille-roche gris, 523
zébré, 523
Fournier, H., 521
Fox, 58,273
Arctic, 602
Red, 40,69,96,244,249 368
Fox, Alopex lagopus, den by a Polar Bear, Ursus maritimus,
Excavation of an Arctic, 602
Fragaria sp., 365
Fraser, S., 225
Fratercula arctica, 258,604,615
cirrhata, 615
corniculata, 615
Fraxinus sp., 136,253
americana, 361,508
nigra, 310,365
pennsylvanica, 309
Frog, Red-legged, 448
Tailed, 447
Froglog: Newsletter of the Declining Amphibian Populations
Task Force, 155,294,484,645
Frogs, Ascaphus truei, American Dipper, Cinclus mexicanus,
Preys Upon Larval Tailed, 446
Fucus gardneri, 406
serratus, 226
Fungus, Nectria, 41
Furcellaria lumbricalis, 226
Furcula modesta, 540
occidentalis, 540
scolopendrina, 540
Fuscidea cyathoides, 420
intercincta, 421
mollis, 424
thomsonii, 406
Fuscopannaria leucostictoides, 411
maritima, 411
thiersii, 421
Galeopsis tetrahit ssp. bifida, 560
Galium aparine, 175
Garbary, D.J., S. Fraser, C. Ferguson, and R.F. Lauff. Use of
Eelgrass, Zostera marina, Wrack by Three Species
of Ladybird Beetles (Coleoptera: Coccinellidae) in
Prince Edward Island, 225
660
Gau, R.J., B.D. McLoughlin, R. Case, H.D. Cluff, R. Mulders,
and F. Messier. Movements of Subadult Male Grizzly
Bears, Ursus arctos, in the Central Canadian Arctic,
239
Gaultheria procumbens, 196
shallon, 159
Gavia spp., 210
immer, 210
pacifica, 210
stellata, 258
Gavia spp.) and Red-necked Grebe (Podiceps grisegena)
Populations in the Lower Matanuska-Susitna Valley,
Alaska, Changes in Loon, 210
Gawn, M., Review by, 473
Gelechia dyarella, 534
lynceella, 534
Gelechiidae, 534
Gelis sp., 122
Gelis sp., in the Egg Sacs of the Wolf Spiders Pardosa moesta
and Pardosa sternalis (Araneae, Lycosidae) in South-
eastern Idaho, Occurrence of Parasitoid Wasps, Baeus
sp. and, 122
Gemsbok, 185
Gende, S.M., 499
Gentianella tenella, 559
Geometridae, 537
Geothlypis trichas, 86,232
Geum aleppicum ssp. strictum, 559
rossti, 559
Giberson, D.J., 425
Gillespie, L.J., 326
Ginns, J., Review, by, 146
Gladders, A., 159
Glaux maritimus, 226
Glen, W.M., 504
Gluphisia avimacula, 540
lintneri, 540
septentrionis, 540
Glyceria striata var. stricta, 559
Glycine max, 253
Gnaphalium palustre, 169
Gnatcatcher, Blue-grey, 232
Gnorimoschema septentrionella, 534
vastificum, 534
Goat, Mountain, 370
Goby, Round, 318
Tubenose, 318
Goby, Neogobius melanostomus Pallas (Gobiidae), and Eco-
tone Utilisation in St. Clair Lowland Waters, Ontario,
Description of Age-O0 Round, 318
Goh, K.M.L., 159
Goldeneye, 604
Barrow’s, 264
Common, 267
Goldeneye, Bucephala islandica, and Surf Scoter, Melanitta
perspicillata, in Coastal Southwestern British Colum-
bia, Observations of Above-Surface Littoral Foraging
in Two Sea Ducks, Barrow’s, 264
Goldenrod, 253
Tall, 342
Goldfinch, American, 378
Goodwin, C.E., Review by, 138
Goose, Canada, 268,602
Snow, 602
Gracillariidae, 532
THE CANADIAN FIELD-NATURALIST
Vol. 118
Grand brochet, 523
Graphiphora augur, 543
Grapholita lunatana, 536
Grass, 400
Annual Blue, 563
Cheat, 174
Creeping Bent, 562
Crested Wheat, 561
Forked Three-awned, 276
Fowl Marina, 563
Indian, 342
June, 563
Orchard, 174,300
Quack, 300
Western Rye, 562
Wheat, 584
Grass, Aristida basiramea Engelm. ex Vasey: A New Addition
to the Flora of Quebec, Forked Three-awned, 276
Grayling, Arctic, 111
Grayling, Thymallus arcticus, Consumption of Shrews, Sorex
spp., by Arctic, 111
Grebe, Red-necked, 210
Grebe (Podiceps grisegena) Populations in the Lower Mata-
nuska-Susitna Valley, Alaska, Changes in Loon (Gavia
spp.) and Red-necked, 210
Greya politella, 532
Griselda radicana, 536
Grosbeak, Rose-breasted, 232
Grouse, 41
Ruffed, 232
Guillemot, Black, 257
Gull, 249,442
Bonaparte’s, 443
Glaucous-winged, 443,616
Great Black-backed, 257,604
Herring, 257,443,449
Mew, 443
Ring-billed, 258
Gulls, Larus marinus, Kill Male Longtailed Duck, Clangula
hyemalis, Two Great Black-backed, 604
Gulls, Larus spp., Foraging at Pink Salmon, Oncorhynchus
gorbuscha, Spawning Runs, 442
Gulo gulo luscus, 56,61
Gulo gulo luscus, in the boreal forest, Effects of mid-winter
snow depth on stand selection by Wolverines, 56
Gulo gulo luscus, Resting Sites and Caching Behavior in the
Boreal Forest, Wolverine, 61
Gyalecta jenensis, 406
Gymnocarpium jessoense ssp. parvulum, 559
Gypsonoma adjuncta, 536
fasciolana, 535
salicicolana, 536
substitutionis, 536
Gyrinus opacus, 431
Habrosyne scripta, 537
Hadeninae, 541
Haemoproteus, 236
Hahn, A., 159
Hairgrass, Early, 177
Mountain, 564
Haliaeetus leucocephalus, 267
Hamr, J., 251
2004
Hansen, D.J. Observations of Habitat Use by Polar Bears,
Ursus maritimus, in the Alaskan Beaufort, Chukchi,
and Northern Bering Seas, 395
Hansen, L.P., 185
Haploa lecontei, 540
Hare, 607
Snowshoe, 41,58,191,278,585
Hare, J.F., G. Todd, and W.A. Untereiner. Multiple Mating
Results in Multiple Paternity in Richardson’s Ground
Squirrels, Spermophilus richardsonii, 90
| Harrimanella stellariana, 559
Harris, A.G., 179
Harris, J.G. Pilose Braya, Braya pilosa Hooker (Cruciferae;
Brassicaceae), an Enigmatic Endemic of Arctic Cana-
da, 550
Harris, S.A. and P.W. Ball. New Records of Cyperaceae and
Juncaceae from the Yukon Territory, 266
Harrisimemna trisignata, 541
Hawk, Rough-legged, 268
_ Hay, 361
| Hayward, J.L. and J.K. Clayburn. Do Rhinoceros Auklet,
Cerorhinca monocerata, Fledglings Fly to the Sea
from Their Natal Burrows?, 615
Hazel, Beaked, 251
_ Healy, C. and L.J. Gillespie. A Systematic Analysis of the
Alpine Saxifrage Complex (Saxifragaceae) in the Can-
adian Arctic Islands Using Morphology and Chloro-
plast DNA Data, 326
Hedeoma hispida, 277
Helcystogramma fernaldella, 534
Hellinsia homodactylus, 536
_ Hemicarpha, 179
| Hemlock, 41,361,499
Eastern, 251,508
Mountain, 159
Western, 159
Hemp-nettle, 576
Hepialidae, 532
Heracleum, 501
Herminiinae, 540
Heron, Great Blue, 230
Herteliana alaskensis, 408
Hesperiidae, 537
Heterocodon rariflorum, 170
Heterocodon, 170
Hillia iris, 542
Hinam, H.L., S.G. Sealy, and T.J. Underwood. Ruby-throated
Hummingbird, Archilochus colubris, Entanglements
in Burdock, Arctium spp., at Delta Marsh, Manitoba,
85
| Hiodon tergisus, 523
Hiodontidae, 523
Hippodamia convergens, 309
parenthesis, 309
tredecimpunctata, 225,309
Hippotragus equinus, 185
Hirundo rustica, 230
Hodgson, D.A., 626
Hogue, E.J., 299
Holodiscus discolor, 176
Homan, H.J., G.M. Linz, R.M. Engeman, and L.B. Penry.
Spring Dispersal Patterns of Red-winged Blackbirds,
Agelaius phoeniceus, Staging in Eastern South Dako-
ta, 201
Homarus americanus, 82
INDEX TO VOLUME 118
66]
Homoglaea hircina, 542
Homohadena badistriga, 5:
infixa, 541
Homosetia fasciella, 532
Honeysuckle, Hairy, 176
Hood, G.A. and T. Neufeld. First Record of Mountain Lions,
Puma concolor, in Elk Island National Park, Alberta,
605
Hop-clover, Small, 170
Hordeum brachyantherum, 559
vulgare, 361
Horse, Wild, 370
Houston, C.S., Reviews by, 142,290,465,466,470,47 1,481,631,
633,635
Huckleberry, Blue, 198
Huettmann, F., Reviews by, 478,632
Hummingbird, Ruby-throated, 85
Rufous, 378
Hummingbird, Archilochus colubris, Entanglements in Bur-
dock, Arctium spp., at Delta Marsh, Manitoba, Ruby-
throated, 85
Huot, J., 360
Hydrelia albifera, 539
Hydriomena furcata, 539
perfracta, 538
renunciata, 539
ruberata, 539
Hydroporus appalachius, 431
geniculatus, 431
hudsonicus, 432
morio, 431
Hydrozoan, 78
Hygrotus novemlineatus, 430
HAyles gallii, 540
Hylocichla mustelina, 232
Hylocomium splendens, 591
Hypatopa titanella, 533
Hypena atomaria, 541
edictalis, 541
humuli, 541
Hypeninae, 541
Hypenodes fractilinea, 540
Hyperaspis benedetti, 312
Hyppa contrasta, 542
Ichthyomyzon fossor, 523
unicuspis, 523
Ictaluridae, 523
Ictalurus punctatus, 523
Icterus galbula, 232
Idaea rotundopennata, 538
Idaho, Occurrence of Parasitoid Wasps, Baeus sp. and Gelis
sp., in the Egg Sacs of the Wolf Spiders Pardosa moesta
and Pardosa sternalis (Araneae, Lycosidae) in South-
eastern, 122
Idia aemula, 540
americalis, 540
Illex illecebrosus, 497
Illingworth, J.M., 169
Ilybius erichsoni, 431
Impala, 185
Indian’s Dream, 166
Ipimorpha pleonectusa, 542
Tridopsis larvaria, 537
Tris setosa ssp. interior, 559
662
Iris, Wild, 567
Isoetes ?maritima, 559
echinospora, 559
Isopod, 389
James, M.C., K. Martin, and P.H. Dutton. Hybridization be-
tween a Green Turtle, Chelonia mydas, and Logger-
head Turtle, Caretta caretta, and the First Record of
a Green Turtle in Atlantic Canada, 579
Jay, Blue, 231
Gray, 273
John, R., Reviews by, 140,143,147,150,282,288,291,630,631,
634,636
Joint, Blue, 591
Jolicoeur, H., 608
Jones, J., W.J. McLeish, and R.J. Robertson. Predicting the
Effects of Cerulean Warbler, Dendroica cerulea Man-
agement on Eastern Ontario Bird Species, 229
Junco hyemalis, 235,381
hyemalis cismontanus, 235
hyemalis hyemalis, 235
hyemalis oregonus, 235
Junco, Dark-eyed, 235,381
Junco hyemalis, Breeding at Different Elevations, Parasite
Prevalence in Dark-eyed Juncos, 235
Juncos, Junco hyemalis, Breeding at Different Elevations,
Parasite Prevalence in Dark-eyed, 235
Juncus spp., 400
bufonius, 170,559
filiformis, 559
Stygius SSp. americanus, 267
Juniper, Common, 166
Juniperus communis, 166
Kalmia, 501
angustifolia, 196
Katydid, Northern True, 124
Katydid, Prerophylla camellifolia (Orthoptera: PseudophyI-
lidae), at Ottawa, Ontario, The Northern True, 124
Kemp, J.P. and C.R. Lacroix. Estimation of Seed Bank and
Seed Viability of the Gulf of Saint Lawrence Aster,
Symphyotrichum laurentianum, (Fernald) Nesom, 105
Kenagy, G.J., 111
Kennedy, C.E., 558
Kent, D., 264
Kierstead, J., 444
Killdeer, 445
Kinglet, Golden-crowned, 48,86
Ruby-crowned, 48,86
Kittiwake, Black-legged, 257
Knapweed, Diffuse, 300
Kneteman, J., 368
Kobresia simpliciuscula, 559
Kobresia, Simple, 566
Koeleria macrantha, 559
Kogia breviceps, 495
simus, 495
Kogia breviceps, in the Northern Gulf of St. Lawrence, Cana-
da, Stranding of a Pygmy Sperm Whale, 495
Kohlmeyera complicatula, 420,424
Korscheltellus gracilis, 532
Kuzyk, G.W., J. Kneteman, and F.K.A. Schmiegelow. Winter
Habitat Use by Wolves, Canis lupus, in Relation to
Forest Harvesting in West-central Alberta, 368
THE CANADIAN FIELD-NATURALIST
l’Esturgeon jaune, 521
Labidesthes sicculus, 319
Labrador, “Ashkui” Vernal Ice-cover Phenomena and Their |
Ecological Role in Southern, 267
Labrador, First Record of a Barred Owl, Strix varia, in, 273
Lacanobia radix, 542
Lace, Queen Anne’s, 342
Lacinipolia lorea, 542
renigera, 542
Lacroix, C.R., 105
Lacroix, D.L., K.G. Wright, and D. Kent. Observations of '
Above-Surface Littoral Foraging in Two Sea Ducks, .
Barrow’s Goldeneye, Bucephala islandica, and Surf |
Scoter, Melanitta perspicillata, in Coastal Southwest-
ern British Columbia, 264
Lactuca serriola, 300
Ladies’-tresses, Hooded, 567
Lady’s-fingers, 613
Lagopus lagopus, 602
Lambdina fiscellaria, 538
Lamna nasus, 245
Lampetra appendix, 523
Lamproie argentée, 523
de lest, 523
du nord, 523
Lamy, R., 270
Landry, J.-F., 530
Langor, D.W., 530
Lapar, R., 135
Laquaiche argentée, 523
Larch, Western, 595
Larentiinae, 538
Lariviere, S., Review by, 139
Larix laricina, 63,136,370,510,590
Larus spp., 249,442
argentatus, 258,443,449
canus, 443
delawarensis, 258
glaucescens, 443,616
marinus, 258,604
philadelphia, 443
Larus marinus, Kill Male Longtailed Duck, Clangula hye-
malis, Two Great Black-backed Gulls, 604
Larus spp., Foraging at Pink Salmon, Oncorhynchus gor-
buscha, Spawning Runs, Gulls, 442
Lasiocampidae, 539
Lasionycta poca, 542
antigReke225
Lauff, R.F., Reviews by, 144,145,288,630
Laura, 132
Laurel, Sheep, 196
Lecanora sp., 411
actophila, 420
contractula, 424
dispersa, 421
helicopsis, 420
muralis, 411
poliophaea, 424 |
poliophaea ssp. poliophaea, 421
straminea, 411
tenera, 424
.
:
Lecidea conferenda, 424
Lecidella scabra, 424
stigmatea, 411
stigmatea f. stigmatea, 424
Mi
—
2004
Ledum groenlandicum, 591
Lemming, Brown, 440
Varying, 403
Lemmus trimucronatus, 440
Lenga, 132
| Lepidium densiflorum var. densiflorum, 559
densiflorum var. macrocarpum, 560
Lepidochelys kempii, 580
Lepomis gibbosus, 523
macrochirus, 318,523
Leptinotarsa decemlineata, 226
Lepus spp., 607
americanus, 41,58,191,278,585
Lesage, L., 360
Leslie, J.K. and C.A. Timmins. Description of Age-O Round
Goby, Neogobius melanostomus Pallas (Gobiidae),
and Ecotone Utilisation in St. Clair Lowland Waters,
Ontario, 318
| Lettuce, Prickly, 300
Leucania insueta, 542
Leucocytozoon, 236
Lichen, 408
Grey Reindeer, 591
Lichina pygmaea, 419
Lily-of-the-Valley, Wild, 362,567
Lim, B.K., Reviews by, 286,472
Limnaecia phragmitella, 534
_ Limnodrilus monothecus, 78
Limonium nashii, 226
Lingonberry, 591
Linz, G.M., 201
Lion, Mountain, 159,605
Lions, Puma concolor, in Elk Island National Park, Alberta,
First Record of Mountain, 605
Lipocarpha micrantha, 179
Lipocarpha, Small-flowered, 179
Lipocarpha, Lipocarpha micrantha (Cyperaceae), in Canada,
Conservation Evaluation of Small-flowered, 179
Lipocarpha micrantha (Cyperaceae), in Canada, Conservation
Evaluation of Small-flowered Lipocarpha, 179
Lithacodia albidula, 541
Litholomia napaea, 542
Lithomoia germana, 542
Lithophane innominata, 542
petulca, 542
Lobophora nivigerata, 539
Lobster, Atlantic, 82
Locoweed, Field, 574
_ Lolium perenne, 170,174
Lomatia hirsuta, 132
Longcore, J.R. and D.G. McAuley. Extraordinary Size and
Survival of American Black Duck, Anas rubripes,
Broods, 129
Lonicera hispidula, 176
Lontra canadensis, 96
Loon, 210
Common, 210
Pacific, 210
Red-throated, 256
Loon (Gavia spp.) and Red-necked Grebe (Podiceps grise-
gena) Populations in the Lower Matanuska-Susitna
Valley, Alaska, Changes in, 210
Lophocampa maculata, 540
Lophodytes cucullatus, 131
Lotus corniculatus, 365
INDEX TO VOLUME 118
663
Lousewort, Oeder’s, 576
Lupinus nootkatensis, 559
Lutra canadensis, 267
Luxilus cornutus, 523
Luzula arcuata ssp. unalaschkensis, 559
Lycaenidae, 537
Lycia ursaria, 537
Lycopodium complanatum, 196
Lymantriidae, 540
Lynx, 57,96,134
Canada, 191,583
Lynx canadensis, 57,96,191,583
lynx, 134
rufus, 40
Lynx canadensis, Distributions, A Snow-tracking Protocol
Used to Delineate Local Lynx, 583
Lynx canadensis, in the Southern Canadian Rocky Mountains,
Predation on Two Mule Deer, Odocoileus hemionus,
by a Canada Lynx, 191
Lynx, Lynx canadensis, Distributions, A Snow-tracking Pro-
tocol Used to Delineate Local, 583
Lynx, Lynx canadensis, in the Southern Canadian Rocky
Mountains, Predation on Two Mule Deer, Odocoileus
hemionus, by a Canada, 191
Lyonetia prunifoliella, 533
Lyonetiidae, 533
Macaria bitactata, 537
brunneata, 537
loricaria, 537
signaria, 537
ulsterata, 537
MacDonald, P., 444
MacDonald, S.O., A.M. Runck, and J.A. Cook. The Heather
Vole, Genus Phenacomys, in Alaska, 438
MacDonnell, L., 444
Macleaya cordata, 614
Madden, E.M., 400
Mahonia aquifolium, 176
Maianthemum, 500
canadense, 196,362
canadense ssp. interius, 559
Maier, T.J., 400
Maitén, 132
Malachigan, 523
Malacosoma disstria, 540
Mallard, 130
Mallotus villosus, 262
Malus sp., 125
domestica, 299
pumila, 361
Manitoba*, Density and Survival of Lady Beetles (Coccinel-
lidae) in Overwintering Sites in, 309
Manitoba, Effects of Lodgepole Pine Dwarf Mistletoe, Arceu-
thobium americanum, on Jack Pine, Pinus banksiana,
Growth in, 595
Manitoba, Hummock Vegetation at the Arctic Tree-line near
Churchill, 590
Manitoba, Ruby-throated Hummingbird, Archilochus colubris,
Entanglements in Burdock, Arctium spp., at Delta
Marsh, 85
Manning (1911-1998), A Tribute to Thomas Henry, 618
Maple, Manitoba, 309
Mountain, 362
Red, 41,96,251,277,361,508
664
Silver, 125
Sugar, 41,124,251,361,507
Marigane noire, 523
Marine Turtle Newsletter, 156,294,484,645
Marmot, Hoary, 440
Vancouver, 403
Marmota caligata, 438
vancouverensis, 403
Marten, 58,63
American, 96,438
Pine, 243
Martes americana, 58,63,96,243,438
pennanti, 56,96,583
Martin, K., 579
Maskinongé, 523
Matteuccia struthiopteris, 46,253
Maytenus boaria, 132
McAlpine, D.F., S.A. Orchard, K.A. Sendall, and R. Palm.
Status of marine turtles in British Columbia waters:
a reassessment, 72
McAuley, D.G., 129
McCarthy, J, Reviews by, 150,152,640
McIntyre, R.T., 115
McKelvey, K.S., 583
McKnight, J., L. Thomas, and D.L. Amirault. Piping Plover,
Charadrius melodus, egg viability after seawater im-
mersion, 448
McLeish, W.J., 229
McLoughlin, P.D., 239
McNicholl, M.K., Review by, 285
Meadow-foxtail, Carolina, 170
Measures, L., B. Roberge, and R. Sears. Stranding of a Pygmy
Sperm Whale, Kogia breviceps, in the Northern Gulf
of St. Lawrence, Canada, 495
Mech, L.D. and S. Tracy. Record High Wolf, Canis lupus,
Pack Density, 127
Mech, L.D., R.T. McIntyre and D.W. Smith. Unusual Beha-
vior by Bison, Bison bison, Toward Elk, Cervus ela-
phus, and Wolves, Canis lupus, 115
Medicago sativa, 361
Megasema c-nigrum, 543
Melanchra adjuncta, 542
Melanitta perspicillata, 264
Melanitta perspicillata, in Coastal Southwestern British
Columbia, Observations of Above-Surface Littoral
Foraging in Two Sea Ducks, Barrow’s Goldeneye,
Bucephala islandica, and Surf Scoter, 264
Meleagris gallopavo silvestris, 251
Meleagris gallopavo silvestris, Behavior in Central Ontario
During Winter, Wild Turkey, 251
Melica subulata, 176
Méné a nageoires rouges, 523
émeraude, 523
jaune, 523
Meningeal Worm, 40
Mephitis mephitis, 40,69
Merganser, Hooded, 131
Mertensia paniculata var. alaskana, 559
Mesoleuca ruficillata, 539
Messier, F., 239
Metalepsis salicarum, 543
Metanema determinata, 538
inatomaria, 538
Meunier noir, 523
Meyer, T.M., 185
THE CANADIAN FIELD-NATURALIST
Vol. 118
Mice, Peromyscus maniculatus, and Yellow-pine Chipmunks,
Tamias amoenus, in Old Field and Orchard Habitats, |
Population Dynamics of Deer, 299
Micranthes kumlienti, 326
nivalis, 326
tenuis, 326
Micropterus dolomieu, 523
salmoides, 113,523
Microtus, 345
longicaudus, 300
montanus, 300
ochrogaster, 342
pennsylvanicus, 342,400
Milfoil, Eurasian, 318
Millipede, 388
Mills, T.K. and B.A. Andres. Changes in Loon (Gavia spp.)
and Red-necked Grebe (Podiceps grisegena) Popula-
tions in the Lower Matanuska-Susitna Valley, Alaska,
210
Millspaugh, J.J., B.E. Washburn, T.M. Meyer, J. Beringer,
and L.P. Hansen. Immobilization of Clover-trapped
White-tailed Deer, Odocoileus virginianus, with Med-
etomidine and Ketamine, and Antagonism with Ati-
pamezole, 185
Mimulus guttatus, 559
Mink, 96
European, 185
Minnow, Bluntnose, 318
Minuartia dawsonensis, 559
elegans, 559
macrocarpa, 559
obtusiloba, 166
yukonensis, 559
Minutes of the 125" Annual Business Meeting of the Ottawa
Field-Naturalists’ Club 13 January 2004, 486
Mistletoe, Lodgepole Pine Dwarf, 595
Mistletoe, Arceuthobium americanum, on Jack Pine, Pinus
banksiana, Growth in Manitoba, Effects of Lodgepole
Pine Dwarf, 595
Mizuhopecten yessoensis, 78
Mniotilta varia, 230
Molothrus ater, 382
Mompha sp., 533
albapalpella, 533
terminella, 533
Monarda punctata, 277
Monkeyflower, Yellow, 576
Monopis laevigella, 532
spilotella, 532
Montia fontana, 559
Moore, J.W. and G.J. Kenagy. Consumption of Shrews, Sorex
spp., by Arctic Grayling, Thymallus arcticus, 111
Moose, 40,57,61,96,134,185,248,368,606
Moose Sickness, 40
Morrissey, C.A. and R.J. Olenick. American Dipper, Cinclus
mexicanus, Preys Upon Larval Tailed Frogs, Ascaphus
truei, 446
Moss, 253
Golden Fuzzy Fen, 591
Irish, 226
Stair-step, 591
Moth, 388
Moths and Butterflies (Lepidoptera) of the Boreal Mixedwood
Forest near Lac La Biche, Alberta, Including New
Provincial Records, 530
2004
| Mountain-heather, Yellow, 575
Mountain-parsley, 560
| Mouse, 342
Deer, 299,342,402
Great Basin Pocket, 300
Meadow Jumping, 403
Western Harvest, 300
White-footed, 299,342
Moxostoma spp., 521
anisurum, 523
carinatum, 523
erythrurum, 526
macrolepidotum, 523
Mulders, R., 239
| Mulinum spinosum, 132
! Mullein, Great, 300
Muntz, E.M. and B.R. Patterson. Evidence for the Use of
Vocalization to Coordinate the Killing of a White-
Tailed Deer, Odocoileus virginianus, by Coyotes,
Canis latrans, 278
Murray, D.F., Review by, 637
' Murre, Common, 257
Thick-billed, 602
Musaraigne cendrée, 441
fuligineuse, 441
Musaraigne fuligineuse, Sorex fumeus, dans le nord-est du
Québec, Extension de |’ aire de distribution connue de
la, 441
_ Muskrat, 267,602,607
| Mussel, Bay, 264
- Mustard, Tansy, 571
Mustela spp., 96,306
erminea, 243
lutreola, 185
nivalis, 403
vison, 96
| Mya arenaria, 78
Myelopsis subtetricella, 536
_ Myosotis scorpioides, 560
| Myriophyllum spicatum, 318
verticillatum, 559
Myrrhis odorata, 614
Myrrhis, Scented, 614
Mythimna oxygala, 542
_ Mytilicola orientalis, 77
| Mytilus edulis, 264
trossulus, 264
Nadata gibbosa, 540
| Naemia serriata, 227
Naseux des rapides, 523
Navarretia squarrosa, 169
Neale, G.K., 95
Nectria coecinea vat. faginata, 41
Needle-and-thread, 564
Needlegrass, Spreading, 564
Nemapogon acapnopennella, 532
roburella, 532
Nematocampa resistaria, 538
Nemophila parviflora, 176
Nemophila, Small-flowered, 176
Neneo, 132
Neogobius melanostomus, 318
INDEX TO VOLUME 118
665
Neogobius melanostomus Pallas (Gobiidae), and Ecotone
Utilisation in St. Clair Lowland Waters, Ontario, Des-
cription of Age-O Round Goby, 318
Neotelphusa praefixa, 534
Nepticulidae, 532
Nerodia sipedon sipedon, 435
Nerodia sipedon sipedon, Frequency of Tail Breakage of the
Northern Watersnake, 435
Nettle, Stinging, 567
Neufeld, T., 605
Newbury, T.L., 267
Nguyen, L.P., J. Hamr, and G.H. Parker. Wild Turkey, Melea-
gris gallopavo silvestris, Behavior in Central Ontario
During Winter, 251
Nicholson, P.H., 243
Niditinea orleansella, 532
Nites betulella, 533
Noctuidae, 540
Nostoc sp., 594
Notemigonus crysoleucas, 523
Nothofagus antarctica, 132
pumilio, 132
Notocelia culminana, 535
Notodonta simplaria, 540
Notodontidae, 540
Notropis atherinoides, 319,523
hudsonius, 318,523
Noturus insignis, 523
Nova Scotia, Continuing Environmental Change: An Example
from, 39
Nuphar polysepalum, 559
Nuthatch, Red-breasted, 384
Nycteola frigidana, 540
Nymphalidae, 537
Nymphalis antiopa, 537
Nire, 132
Oak, 342
Bur, 310
California Black, 383
English, 125
Gambel, 383
Garry, 174,376
Red, 124,251
Oak Habitat in Southwestern British Columbia, Bird Com-
munities of the Garry, 376
Oat, 361,562
Oatgrass, California, 169
Oceanodroma leucorhoa, 258
Oceanspray, 176
Ochrolechia subplicans, 411
subplicans ssp. hultenii, 420
subplicans ssp. subplicans, 420
Odocoileus spp., 368
hemionus, 132,162,185,191,370,606
hemionus columbianus, 162
virginianus, 40,96, 127,185,278,360,370.606
Odocoileus hemionus, by a Canada Lynx, Lynx canadensis,
in the Southern Canadian Rocky Mountains, Preda-
tion on Two Mule Deer, 191
Odocoileus virginianus, by Coyotes, Canis latrans, Evidence
for the Use of Vocalization to Coordinate the Killing
of a White-Tailed Deer, 278
666
Odocoileus virginianus, Populations Living at Low and High
Density in Southern Québec, Summer Diet of Two
White-tailed Deer, 360
Odocoileus virginianus, with Medetomidine and Ketamine,
and Antagonism with Atipamezole, Immobilization
of Clover-trapped White-tailed Deer, 185
Oecophoridae, 533
Oenothera biennis, 253
Olenick, R.J., 446
Olethreutes glaciana, 535
metallicana, 535
Olethreutinae, 535
Oligia illocata, 541
mactata, 541
Oligochaete, 78
Omisco, 523
Oncorhynchus gorbuscha, 442
keta, 248
nerka, 111,249,443
Oncorhynchus gorbuscha, Spawning Runs, Gulls, Larus spp..
Foraging at Pink Salmon, 442
Ondatra zibethicus, 267,602,607
Onion, Wild, 567
Oniongrass, Alaska, 176
Onoclea sensibilis, 253
Ontario Bird Species, Predicting the Effects of Cerulean War-
bler, Dendroica cerulea Management on Eastern, 229
Ontario, Demographic patterns and limitations of Grey Wolves,
Canis lupus, in and near Pukaskwa National Park, 95
Ontario, Description of Age-O Round Goby, Neogobius mela-
nostomus Pallas (Gobiidae), and Ecotone Utilisation
in St. Clair Lowland Waters, 318
Ontario During Winter, Wild Turkey, Meleagris gallopavo
silvestris, Behavior in Central, 251
Ontario, Effect of Fire Intensity and Depth of Burn on Low-
bush Blueberry, Vaccinium angustifolium, and Velvet
Leaf Blueberry, Vaccinium myrtilloides, Production
in Eastern, 195
Ontario Natural Heritage Information Centre Science and
Information Newsletter 9(1) Winter 2004, 156
Ontario: rabies management implications, Seasonal home
ranges of raccoons using a common feeding site in rural
eastern, 65
Ontario, Significant Vascular Plant Records from the Hamil-
ton Area, 612
Ontario, The Northern True Katydid, Prerophylla camellifolia
(Orthoptera: Pseudophyllidae), at Ottawa, 124
Opegrapha sp., 411
gyrocarpa, 406
Operophtera bruceata, 539
Oplopanax, 500
horridum, 500
Orache, Alaskan, 568
Orchard, S.A., 72
Oreamnos americanus, 370
Oregon-grape, Tall, 176
Oreodytes laevis, 427
sanmarkii, 427
Oreta rosea, 537
Oriole, Baltimore, 232
Orobanche fasciculata, 559
Orthofidonia exornata, 537
Orthosia hibisci, 542
revicta, 542
segregata, 542
THE CANADIAN FIELD-NATURALIST
Vol. 118
Oryx gazella, 185
Osprey, 267
Otisorex, 400
Ottawa Field-Naturalists’ Club Awards for 2003, The, 646
Otter, K.A., 354
Otter, River, 96,267
Sea, 270
Otter, Enhydra lutris, Sightings off Haida Gwaii/Queen Char- - |
lotte Islands, British Columbia, 1972-2002, Sea, 270 }
Ouellet, J.-P., 360
Ouitouche, 523
Ovenbird, 232
Ovis canadensis, 370
Owl, Barred, 215,273
Great Horned, 222,273
Owl, Strix varia in Alberta: Distribution and Status, The — |
Barred, 215 |
Owl, Strix varia, in Labrador, First Record of a Barred, 273
Oxytrope, Arctic, 574
Oxytropis arctica, 558
campestris ssp. varians, 559
Oxyura jamaicensis, 604
Oyster, Pacific, 77
Pachnobia imperita, 543
mixta, 543
Palm, R., 72
Palmaria palmata, 226
Palthis angulalis, 540.
Pandemis canadana, 535
Pandion haliaetus, 267
Panic-grass, Yellow, 197
Panicum xanthophysum, 197
Panthera tigris, 185
Papaver croceum, 558
nudicaule ssp. nudicaule, 558
Papilio canadensis, 537
Papilionidae, 537
Paquet, P.C., 95
Parapoynx maculalis, 537
Parastichtis suspecta, 541
Pardosa lapidicina, 123
moesta, 122
sternalis, 122
Pardosa moesta and Pardosa sternalis (Araneae, Lycosidae) 1n
Southeastern Idaho, Occurrence of Parasitoid Wasps,
Baeus sp. and Gelis sp., in the Egg Sacs of the Wolf
Spiders, 122
Pardosa sternalis (Araneae, Lycosidae) in Southeastern Idaho,
Occurrence of Parasitoid Wasps, Baeus sp. and Gelis
sp., in the Egg Sacs of the Wolf Spiders Pardosa
moesta and, 122
Parectopa pennsylvaniella, 532
Parelaphostrongylus tenuis, 40
Pariseau, R., 521
Parker, G.H., 251
Parmelia saxatilis, 406
Parornix conspicuella, 532 |
Parrya arctica, 560 |
Parsnip, Cow 196
Partridge, S.T., 247
Passerina cyanea, 232
Patagonia, Observations of Interactions between Puma, Puma _
concolor, and Introduced European Red Deer, Cervus
elaphus, in, 132
—
——S—=
2004
Patinopecten sp., 82
| caurinus, 78
Patterson, B.R., 278
Pediasia dorsipunctella, 537
| Pedicularis oederi, 559
_Pelonaia corrugata, 79
Penny, J.L., 174
#))), Penry, L.B., 201
| Pepper-grass, Common, 572
| Perca flavescens, 521
, Perchaude, 523
| Percidae, 521
| Percina caprodes, 523
| copelandi, 523
| Percopsidae, 523
« Percopsis omiscomaycus, 523
| Perisoreus canadensis, 273
| Perispasta caeculalis, 537
_Perizoma basaliata, 539
| Pero honestaria, 538
| Perognathus parvus, 300
Peromyscus spp., 342
leucopus, 299,342
| maniculatus, 299,342,402
| Peromyscus maniculatus, and Yellow-pine Chipmunks, Tamias
| amoenus, in Old Field and Orchard Habitats, Popu-
| lation Dynamics of Deer Mice, 299
| Perry, N.D., D.T. Stewart, EM. Madden, and T.J. Maier. New
| Records for the Arctic Shrew, Sorex arcticus and the
i] Newly Recognized Maritime Shrew, Sorex mariti-
mensis, 400
| Peterkin, P., Review by, 641
| Petrel, Leach’s Storm, 258
| Petromyzontidae, 523
| Phacelia, Macbryde’s, 576
| Phacelia mollis, 559
Phalacrocorax auritus, 258
carbo, 258
j Phalaenophana pyramusalis, 540
Phalaenostola hanhami, 540
| Phaneta awemeana, 535
convergana, 535
parmatana, 535
Phenacomys intermedius, 438
intermedius intermedius, 438
ungava, 438
i Phenacomys, in Alaska, The Heather Vole, Genus, 438
Pheosia rimosa, 540
Pheucticus ludovicianus, 232
Phillips, F., 273
Phleum pratense, 253
Phlogophora periculosa, 542
Phlox hoodii, 559
Phlox, Moss, 575
Phlyctaenia coronata, 537
Phoca hispida, 395,602
Phragmatobia assimilans, 540
Phyllodesma americana, 539
Phyllodoce glanduliflora, 559
Phyllonorycter sp., 532
martiella, 532
Physcia caesia, 411
Physeter macrocephalus, 495
Picard, [., 441
Picea spp., 57,61
INDEX TO VOLUME 118
667
engelmannii, 191,584
glauca, 46,95,211,218,249,251,274,361,370,388,401,
504,530,590
glauca X engelmannii, 355
mariana, 62,95,268,274,370,388,504,590
rubens, 41,52,510
sitchensis, 499
Picoides pubescens, 358
Pieridae, 537
Pieris oleracea, 537
Pimephales notatus, 318
Pine, Eastern White, 251
Ground, 196
Jack, 95,196,253,388,595
Lodgepole, 58,62,191,355,370,499,561,584,595
Ponderosa, 198,300,383,595
Red, 196,251
White, 41,196,277
Whitebark, 584
Pine, Pinus banksiana, Growth in Manitoba, Effects of Lodge-
pole Pine Dwarf Mistletoe, Arceuthobium america-
num, on Jack, 595
Pinguicula villosa, 559
Pinus spp., 60
albicaulis, 584
banksiana, 95,196,253,388,595
contorta, 58,62,191,370,499,584,595
contorta ssp. latifolia, 559
contorta var. latifolia, 355
ponderosa, 198,300,383,595
resinosa, 196,251
strobus, 41,196,251,277
Pinus banksiana, Growth in Manitoba, Effects of Lodgepole
Pine Dwarf Mistletoe, Arceuthobium americanum, on
Jack Pine, 595
Pipilo maculatus, 378
Piranga ludoviciana, 378
Piranga olivacea, 232
Pisaster ochraceus, 265
Pissodes strobi, 41
Pitcher, K., 270
Placopsis gelida, 424
lambii, 406
Plagiobothrys scouleri, 170
Plagodis alcoolaria, 538
phlogosaria, 538
pulveraria, 538
Plaintain, Seaside, 577
Plantago spp., 247
canescens, 559
maritima, 559
Plasmodium spp., 237
Platarctia parthenos, 540
Platichthys stellatus, 248
Platynota idaeusalis, 535
Platyphyllum concavum, 125
Platypolia anceps, 542
Plemyria georgii, 538
Pleurozium schreberi, 591
Plover, Piping, 444.448
Snowy, 445
Plover, Charadrius melodus, egg viability after seawater im-
mersion, Piping, 448
Plover, Charadrius melodus, Nesting
Sequential Polyandry in Piping,
in Eastern Canada,
444
668
Plume-poppy, 614
Plusia putnami, 541
Plusiinae, 541
Plutella xylostella, 533
Plutellidae, 533
Poa spp., 300
annua, 560
compressa, 277
interior, 558
leptocoma, 559
nemoralis, 558
pratensis, 176
secunda, 559
Podiceps grisegena, 210
Podiceps grisegena) Populations in the Lower Matanuska-
Susitna Valley, Alaska, Changes in Loon (Gavia spp.)
and Red-necked Grebe, 210
Podistera macounii, 559
Poecile atricapillus, 232
hudsonicus, 48
rufescens, 378
Pohl, G.R., D.W. Langor, J.-F. Landry, and J.R. Spence. Moths
and Butterflies (Lepidoptera) of the Boreal Mixed-
wood Forest near Lac La Biche, Alberta, Including
New Provincial Records, 530
Point Pelee Natural History News 3(4), 155
Polemonium acutiflorum forma lacteum, 558
boreale forma albiflorum, 558
Polia imbrifera, 542
nimbosa, 542
Polioptila caerulea, 232
Polix coloradella, 533
Polychidium muscicola, 424
Polychrysia esmerelda, 541
Polygonatum pubescens, 196
Polygonia satyrus, 537
Polygonum lapathifolium, 559
viviparum, 591
Polystichum kruckebergii, 164
lemmonii, 164
mohrioides, 164
scopulinum, 164
Polystichum lemmonii, a Threatened Fern in Canada, Con-
servation Evaluation of Lemmon’s Holly Fern, 164
Polytrichadelphus lyellii, 421
Pomoxis nigromaculatus, 523
Pond-lily, Yellow, 569
Pondweed, 318
Curly, 318
Flatstemmed, 561
Sago, 561
Variable-leaved, 561
White-stemmed, 561
Popcornflower, Scouler’s, 170
Poplar, Balsam, 62,218,268,530
Populus spp., 52,57,61,511
balsamifera, 62,136,218,268,530
balsamifera ssp. trichocarpa, 355
deltoides, 309
grandidentata, 136
tremuloides, 46,62,96,136,211,218,251,268,274,277,
316,342,355,361,370,388,5 15,530,584
trichocarpa, 211
Porbeagle, 245
Porcupine, 607
THE CANADIAN FIELD-NATURALIST
Vol. 118
Porina chlorotica, 421
pacifica, 406
Porpidea speirea, 415
carlottiana, 411
contraponenda, 406
speirea, 406
thomsonii, 406
Poszig, D., C.D. Apps, and A. Dibb. Predation on Two Mule »
Deer, Odocoileus hemionus, by a Canada Lynx, Lynx :
canadensis, in the Southern Canadian Rocky Moun-
tains, 191
Potamogeton spp., 318,365
alpinus ssp. tenuifolius, 559
berchtoldii, 559
crispus, 318
gramineus, 559
pectinatus, 559
praelongus, 559
subsibiricus, 559
zosteriformis, 559
Potentilla arguta ssp. convallaria, 573
arguta var. convallaria, 559
Prairie-crocus, 569
Prest (1913-2003), A Tribute to Victor Kent, 626
Primrose, Evening, 253
Primula eximia, 559
tschuktschorum ssp. cairnesiana, 575
Prince Edward Island, A Mapping of the Present and Past
Forest-types of, 504
Prince Edward Island, Use of Eelgrass, Zostera marina, Wrack
by Three Species of Ladybird Beetles (Coleoptera:
Coccinellidae) in, 225
Prionoxystus robiniae, 534
Procyon lotor, 65
Prodoxidae, 532
Propylea quatuordecimpunctata, 225
Proterorhinus marmoratus, 318
Protitame virginalis, 537
Protoboarmia porcelaria, 537
Protolampra rufipectus, 543
Protolithocolletis lathyri, 532
Protorthodes oviduca, 542
Protothaca staminea, 77
Pruitt, W.O., Jr., Review by, 638
Prunus sp., 136
pennsylvanica, 365
pumila, 196
serotina, 365
virginiana, 253,362
Pseudacris maculata, 136
Pseudexentera oregona, 536
Pseudohermonassa tenuicula, 543
Pseudosciaphila duplex, 535
Pseudothyatira cymatophoroides, 537
Pseudotsuga menziesii, 159,376,584
menziesii var. glauca, 355
menziesii var. menziesii, 599
Psilocarphus elatior, 169
tenellus var. tenellus, 169
Psilocarphus elatior, an Endangered Herb in Canada, Con-
servation Evaluation of the Pacific Population of Tall
Woolly-heads, 169
Psyllobora virginimaculata, 312
Ptarmigan, Willow, 602
Pteridium aquilinum, 196,251
ieee
2004
' Pterophoridae, 536
Pterophylla, 125
camellifolia, 124
Pterophylla camellifolia (Orthoptera: Pseudophyllidae), at
Ottawa, Ontario, The Northern True Katydid, 124
Ptychoramphus aleuticus, 616
| Puccinellia interior, 559
| Puffin, Atlantic, 257,604,615
Horned, 615
| Tufted, 615
| Pulsatilla ludoviciana, 559
Puma concolor, 132,605
concolor vancouverensis, 159
|Puma, 132
| Puma concolor, and Introduced European Red Deer, Cervus
elaphus, in Patagonia, Observations of Interactions
between Puma, 132
‘Puma concolor, in Elk Island National Park, Alberta, First
Record of Mountain Lions, 605
Puma concolor vancouverensis, Morphology and Population
|
Characteristics of Vancouver Island Cougars, 159
Puma, Puma concolor, and Introduced European Red Deer,
Cervus elaphus, in Patagonia, Observations of Inter-
| actions between, 132
| Punctelia stictica, 424
| Pyralidae, 536
! Pyrausta borealis, 537
nicalis, 537
| Pyrenocollema halodytes, 410
| sublitorale, 424
Pyrola minor, 559
Quackgrass, 253
: Quail, California, 378
Québec, Extension de I’aire de distribution connue de la Mus-
araigne fuligineuse, Sorex fumeus, dans le nord-est du,
44]
Quebec, Forked Three-awned Grass, Aristida basiramea
Engelm. ex Vasey: A New Addition to the Flora of,
276
Québec, Inventaire printanier d’une frayére multispécifique:
Vichtyofaune des rapides de la riviére Gatineau, 521
Québec, Premiéres mentions de la Couleuvre mince, Tham-
nophis sauritus septentrionalis, au, 135
Québec, Summer Diet of Two White-tailed Deer, Odocoileus
virginianus, Populations Living at Low and High Den-
sity in Southern, 360
—Quenouilles, 136
Quercus spp., 342,365
alba, 342
candicans, 383
gambellii, 383
garryana, 174,376
kelloggii, 383
laurina, 383
macrocarpa, 310,342
i obtusata, 383
robur, 125
rubra, 124,251,342
rugosa, 383
' Queue 4 tache noire, 523
- Quillwort, Bristle-like, 560
Maritime, 560
INDEX TO VOLUME
118 669
Raccoon, 65
Raccoons using a common feeding site in rural eastern On-
tario: rabies management implications, Seasonal home
ranges of, 65
Radal, 132
Ragweed, Hybrid, 613
Ragwort, Dryland, 577
Rail, J.-F. and G. Chapdelaine. Fifteenth Census of Seabird
Populations in the Sanctuaries of the North Shore of
the Gulf of St. Lawrence, 1998-1999, 256
Rainette faux-grillon boréale, 136
Raisin, Northern Wild, 253
Ramalina siliquosa, 420
Rana aurora, 448
Randa, L.A. and J.A. Yunger. The Influence of Prey Avail-
ability and Vegetation Characteristics on Scent Sta-
tion Visitation Rates of Coyotes, Canis latrans, in a
Heterogeneous Environment, 341
Rangifer tarandus, 39,119,192,241,362,602
tarandus caribou, 57,61,119,368
tarandus tarandus, 96,185
Rangifer tarandus caribou, in Saskatchewan, Morphology
of Female Woodland Caribou, 119
Ranunculus aquatilis var. subrigidus, 559
occidentalis var. brevistylis, 559
Raphia frater, 541
Raptor, 306
Raseux-de-terre gris, 523
noir, 523
Raspberry, 251
Raum-Suryan, K., K. Pitcher, and R. Lamy. Sea Otter, Enhy-
dra lutris, Sightings off Haida Gwaii/Queen Charlotte
Islands, British Columbia, 1972-2002, 270
Raven, 273
Razorbill, 257
Redcedar, Western, 159
Redstart, American, 232
Regulus calendula, 48,86
satrapa, 48,86
Reindeer, 185
Reithrodontomys megalotis, 300
Renaud, C.B., 521
RENEW. 2004. Recovery of Nationally Endangered Wildlife
in Canada. Annual Report (14), 644
Retinia burkeana, 535
Rettie, W.J. Morphoiogy of Female Woodland Caribou,
Rangifer tarandus caribou, in Saskatchewan, 119
Rheum rhabarbarum, 560
Rhigognostis interrupta, 533
Rhinanathus minor ssp. borealis, 559
cataractae, 523
Rhizocarpon, 411
cinereovirens, 421
geminatum, 411
haidensis, 411
hensseniae, 408
hochstetteri, 411
maritimum, 421
Rhubarb, 568
Ribes, 500
oxyacanthoides ssp. oxyacanthoides, 559
Richardson, E.S. and R.K. Brook. Excavation of an Arctic Fox,
Alopex lagopus, den by a Polar Bear, Ursus maritimus,
602
Rinodina gennari, 408
670
Rissa tridactyla, 258
Rivula propinqualis, 540
Rivulinae, 540
Roberge, B., 495
Robertson, R.J., 229
Robin, American, 381
Rock-Cress, Wall, 570
Rockweed, 406
Rorippa barbareifolia, 558
Rosa blanda, 253
woodsii, 559
Rosatte, R.C., 65
Rose, Smooth Wild, 253
Western, 574
Rosell, F., 434
Rothfels, C. Significant Vascular Plant Records from the Ham-
ilton Area, Ontario, 612
Rubus spp., 251,365,500
ideaus, 197
spectabilis, 500
Ruggiero, L.F., 583
Rumex crispus, 560
Runck, A.M., 438
Rush, 400
Toad, 170,567
Russell, 1904-1998, A Tribute to Loris Shano, 451
Ryegrass, Perennial, 170,174
Sabia conica, 78
Sagebrush, 300
Sagittaria sp., 318
Salal, 159
Salamander, Cope’s, 448
Pacific Giant, 448
Salamandre sombre des montagnes, 136
Salix spp., 57,136,180,211,247,253,268,356,365,370,530
alaxensis ssp. longistylis, 559
amagdaloides, 309
glauca var. acutifolia, 559
novae-angliae, 567
pseudomyrsinites, 559
rotundifolia ssp. dodgeana, 559
Salmo clarki, 448
salar, 77
trutta, 113,523
Salmon, Atlantic, 77
Chum, 248
Pink, 442
Red, 249
Sockeye, 111,443
Salmon, Oncorhynchus gorbuscha, Spawning Runs, Gulls,
Larus spp., Foraging at Pink, 442
Salmonidae, 523
Salsify, Yellow, 300
Salvelinus namaycush, 523
Sambucus, 501
racemosa, 500
racemosa ssp. pubens, 559
Samuel, W.M., 95
Sander spp., 521
canadensis, 523
vitreus, 523
Sander-Regier, R., Reviews by, 153,474,477,478,632
Sandlance, 262
Sandpiper, Spotted, 444
THE CANADIAN FIELD-NATURALIST
Vol. 118:
Sandwort, Alpine, 166
Sanicle, Pacific, 174
Sanicula crassicaulis var. crassicaulis, 174
Sargassum muticum, 77
Sarrothripinae, 540
Sarsasparilla, Wild, 46
Saskatchewan, Morphology of Female Woodland Caribou, ,
Rangifer tarandus caribou, in, 119
Saskatoon, 573
Saxidomus giganteus, 77
Saxifraga, 326
caespitosa, 559
eschscholtzii, 559
foliolosa, 327,559
gaspensis, 327
hieracifolia, 336
nelsoniana ssp. pacifica, 559
nivalis, 326
nivalis var. gaspensis, 327
nivalis var. labradorica, 327
nivalis var. rufopilosa, 327
nivalis var. tenuis, 326
rufopilosa, 327,559
tenuis, 326
tricuspidata, 559
Saxifrage, Prickly, 573
Scale, Woolly Beech, 41
Scallop, Weathervane, 82
Scaup, Greater, 268
Schinus patagonicus, 132
Schizoporella unicornis, 79
Schizura leptinoides, 540
unicornis, 540
Schmelzer, [. and F. Phillips. First Record of a Barred Owl,
Strix varia, in Labrador, 273
Schmiegelow, F.K.A., 368
Schoen, J.W., 247
Sciaenidae, 523
Scirpus spp., 318
americanus, 226
cyperinus, 402
maritimus, 226
rollandii, 559
Scoparia biplagialis, 531
Scopula ancellata, 538
frigidaria, 538
junctaria, 538
limboundata, 538
Scoter, Surf, 264
Scoter, Melanitta perspicillata, in Coastal Southwestern
British Columbia, Observations of Above-Surface
Littoral Foraging in Two Sea Ducks, Barrow’s Gold-
eneye, Bucephala islandica, and Surf, 264
Scouring-rush, Variegated, 591
Scymnus (Pullus) brullei, 312
Seal, Ringed, 395,602
Sealy, S.G., 85
Sears, R., 495
Sea Star, Ochre, 265
Seaweed, 77
Sargassum, 78
Seburn, C., Reviews by, 149,635
Seburn, D., Reviews by, 140,143,468,471
Sedge, 318,400
Blunt, 565
===
Green-sheathed, 170
Houton’s, 197
Mud, 591
One-sided, 169
Ross’, 566
Slender-beaked, 169
Two-toned, 564
i Water, 591
Seiurus aurocapilla, 232
noveboracensis, 232
| Selasphorus rufus, 378
| Selenia alciphearia, 538
| Semibalanus spp., 406
| Semioscopis inornata, 533
Semotilus corporalis, 523
| Sendall, K.A., 72
Senecio eremophilus, 558
| Sergeant, D.E., Review by, 144
| Serviceberry, 196
| Setaria viridis, 558
| Setophaga ruticilla, 232
| Seymour, K.L. A Tribute to Loris Shano Russell, 1904-1998,
| 451
| Shackleton, D.M., 159
| Shad, American, 77
| Gizzard, 318
| Sharpe. F., 434
| Shaverdo, H.V. and D.J. Giberson. Predaceous Water Beetles
lected Along the Horton and Thelon Rivers in the
(Coleoptera: Adephaga: Dytiscidae, Gyrinidae) Col-
| Arctic Central Barrens of Canada, 425
| Sheep, Bighorn, 370
Shepherd, German, 247
| Shepherd’s-purse, 571
| Shiner, Emerald, 319
| Spottail, 318
| Shooting-star, Broad-leaved, 175
| Shrew, 111
| Arctic, 400
| Gaspé, 403
| Maritime, 400
]
\
Masked, 400
Northern Short-tailed, 402
Pygmy, 402
Smoky, 400
Tundra, 400
| Shrew, Sorex arcticus and the Newly Recognized Maritime
Shrew, Sorex maritimensis, New Records for the Arctic,
400
|| Shrew, Sorex maritimensis, New Records for the Arctic Shrew,
Til
Sorex arcticus and the Newly Recognized Maritime,
400
Shrews, Sorex spp., by Arctic Grayling, Thymallus arcticus,
Consumption of, 111
Sicya macularia, 538
Silene involucrata ssp. tenella, 559
vulgaris, 560
| williamsii, 559
Silverside, Brook, 319
| Sinapis arvensis, 560
| Sinoe sp., 534
Siskin, Pine, 378
| Sisymbrium altissimum, 300
| Sitta canadensis, 384
Skunk, Striped, 40,69
INDEX TO VOLUME 118
671
Skunkweed, 169
Sloan, N.A., 405
Sloan, N.A. and P.M. Bartier. Introduced Marine Species in
the Haida Gwaii (Queen Charlotte Islands) Region,
British Columbia, 77
Slug, 388
Smartwood, Pale, 568
Smerinthus cerisyi, 540
Smith, C.M., Reviews by, 284,287
Smith, D.W., 115
Smith, T., Reviews by, 146,148,480,641
Smith, T.S., S.T. Partridge, and J.W. Schoen. Interactions of
Brown Bears, Ursus arctos, and Gray Wolves, Canis
lupus, at Katmai National Park and Preserve, Alas-
ka, 247
Smith, T.W., G.W. Douglas and A.G. Harris. Conservation
Evaluation of Small-flowered Lipocarpha, Lipocarpha
micrantha (Cyperaceae), in Canada, 179
Snail, 78,388
Snake, Butler’s Garter, 435
Eastern Garter, 435
Garter, 448
Northern Ribbon, 435
Snowberry, Common, 175
Sobey, D.G. and W.M. Glen. A Mapping of the Present and
Past Forest-types of Prince Edward Island, 504
Solidago spp., 253,365
altissima, 342
canadensis var. salebrosa, 560
Solomon’s Seal, Hairy, 196
Somateria mollissima, 258
Sonchus sp., 365
arvensis ssp. uliginosus, 560
Sorbus americana, 362
Sorex spp., 111,400
araneus, 113
arcticus, 400
arcticus arcticus, 402
arcticus laricorum, 402
arcticus maritimensis, 400
cinereus, 111,400,441
fumeus, 400,441
gaspensis, 403
hoyi, 112,402
maritimensis, 400
monticolus, 111,438
tundrensis, 112,400
yukonicus, 112
Sorex arcticus and the Newly Recognized Maritime Shrew,
Sorex maritimensis, New Records for the Arctic Shrew,
400
Sorex fumeus, dans le nord-est du Québec, Extension de l’aire
de distribution connue de la Musaraigne fuligineuse.
44]
Sorex maritimensis, New Records for the Arctic Shrew, Sorex
arcticus and the Newly Recognized Maritime Shrew,
400
Sorex spp., by Arctic Grayling, Thymallus arcticus, Con-
sumption of Shrews, 111
Sorgastrum nutans, 342
South Dakota, Spring Dispersal Patterns of Red-winged
Blackbirds, Agelaius phoeniceus, Staging in East-
ern, 201
Sow-thistle, Perennial, 578
Soybean, 253
672
Spargania luctuata, 539
Sparganothis sp., 535
reticulatana, 535
xanthoides, 535
Sparrow, Chipping, 378
Song, 378
White-crowned, 378
Spartina spp., 400
alterniflora, 226
patens, 226
Spence, J.R., 530
Spermophilus spp., 90
beecheyi, 90
beldingi, 90
brunneus, 91
columbianus, 90
parryii, 91
richardsonii, 90
tridecemlineatus, 90
Spermophilus richardsonii, Multiple Mating Results in Mul-
tiple Paternity in Richardson’s Ground Squirrels, 90
Sphagnum, 499
Sphingidae, 540
Spider, Wolf, 122
Spiders Pardosa moesta and Pardosa sternalis (Araneae,
Lycosidae) in Southeastern Idaho, Occurrence of Par-
asitoid Wasps, Baeus sp. and Gelis sp., in the Egg Sacs
of the Wolf, 122
Spilonema revertens, 410
Spiraea latifolia, 253
Spiranthes romanzoffiana, 560
Spizella passerine, 378
Springbeauty, Alpine, 568
Springtail, 389
Spruce, Black, 57,61,95,268,274,370,388,504,590
Engelmann, 191,584
Norway, 124
Red, 41,52,514
Sitka, 499
White, 46,57,61,95,211,218,249,251,274,355,361,370,
388,401,504,530,590
Squid, 497
Squires, J.R., K.S. McKelvey, and L.F. Ruggiero. A Snow-
tracking Protocol Used to Delineate Local Lynx, Lynx
canadensis, Distributions, 583
Squirrel, Arctic Ground, 91
Belding’s Ground, 90
California Ground, 90
Columbian Ground, 90
Idaho Ground, 91
Red, 607
Richardson’s Ground, 90
Thirteen-lined Ground, 90
Squirrels, Spermophilus richardsonii, Multiple Mating Results
in Multiple Paternity in Richardson’s Ground, 90
Starflower, 575
Starling, European, 378
Stellaria umbellata, 560
Stenolechia sp., 534
Sterna caspia, 258
hirundo, 258
paradisaea, 258
Sternotherus odoratus, 136
Sterrhinae, 538
Stethorus punctum, 312
THE CANADIAN FIELD-NATURALIST
Stewart, D.T., 400
Stictotarsus griseostriatus, 430
Stigmella sp., 532
Stipa comata, 560
nelsonii ssp. dorei, 560
richardsonii, 560
speciosa var. major, 132
Stoffel, M.J., Review by, 284
Storeria dekayi, 136
Storm-Petrel, Leach’s, 259
Strawberry-blite, 568
Strepsimaninae, 540
Streptopus, 500
amplexifolius, 500
Strix varia, 215,273
Strix varia in Alberta: Distribution and Status, The Barred
Owl, 215 |
Strix varia, in Labrador, First Record of a Barred Owl, 273
Sturnus vulgaris, 378
Subularia aquatica ssp. americana, 560
Sucker, White, 319
Sullivan, D.S., 299 i
Sullivan, T.P., D.S. Sullivan, and E.J. Hogue. Population Dy-
namics of Deer Mice, Peromyscus maniculatus, an
Yellow-pine Chipmunks, Jamias amoenus, in Old dl
Field and Orchard Habitats, 299 |
Swallow, Barn 230 i!
Violet-green, 379
Swammerdamia caesiella, 532
Sweet, Meadow, 253
Sylvilagus, 345
floridanus, 342
Symphoricarpos albus, 175
Symphyotrichum laurentianum, 105
Symphyotrichum laurentianum, (Fernald) Nesom, Estimation }
of Seed Bank and Seed Viability of the Gulf of Saint |
Lawrence Aster, 105
Synaptomys borealis, 438
Synclita obliteralis, 537
Syncopacma sp., 534
Syndemis afflictana, 535
Syngrapha alias, 541
octoscripta, 541
rectangula, 541
viridisigma, 541
Takats Priestley, L. The Barred Owl, Strix varia in Alberta:
Distribution and Status, 215
Tamarack, 63,370,515,590
Tamias amoenus, 299
Tamias amoenus, in Old Field and Orchard Habitats, Popu-
lation Dynamics of Deer Mice, Peromyscus manicu-
latus, and Yellow-pine Chipmunks, 299
Tamiasciurus hudsonicus, 607
Tanacetum vulgare, 560
Tanager, Scarlet, 232
Western, 378
Taniva albolineana, 535
Tansey, Common, 578
Taraxacum officinale, 365
Tardif, J.C., 595
Taxus canadensis, 41,365
Tea, Common Labrador, 591
Teal, Green-winged, 131
Teleiodes proximella, 534
IF
1
ek ITE
2004
SS
Telfer, E.S. Continuing Environmental Change: An Example
from Nova Scotia, 39
| Tephromela atra, 424
Tern, Arctic, 257
Caspian, 258
Common, 257
Tews, J. Hummock Vegetation at the Arctic Tree-line near
i} Churchill, Manitoba, 590
Thamnophis spp., 448
| butleri, 435
sauritus, 135,435
| sauritus septentrionalis, 135
sirtalis, 435
sirtalis sirtalis, 135
Thamnophis sauritus septentrionalis, aa Québec, Premieres
mentions de la Couleuvre mince, 135
| Thistle, Swamp, 253
Thlaspi arvense, 560
Thomas, L., 448
Thomsen, L.R., F. Sharpe, and F. Rosell. Collapsing Burrow
| Causes Death of a Eurasian Beaver, Castor fiber, 434
Thrush, Swainson’s, 382
! Wood, 232
| Thryomanes bewickii, 378
‘f
| Thuja occidentalis, 96,136,253,361,508
| plicata, 159
_Thymallus arcticus, 111
thymallus, 113
Thymallus arcticus, Consumption of Shrews, Sorex spp., by
| Arctic Grayling, 111
Tick, American Dog, 42
Tiger, 185
Tilia americana, 253,310
_| Timmins, C.A., 318
| Timothy, 253
| Tineidae, 532
| Tinline, R.R., 65
| Todd, G., 90
Tofieldia coccinea, 560
| Tomenthypnum nitens, 591
Tortricidae, 534
| Tortricinae, 534
| Tortue musquée, 136
Totton, S.C., R.C. Rosatte, R.R. Tinline, and L.L. Bigler. Sea-
sonal home ranges of raccoons using a common feed-
ing site in rural eastern Ontario: rabies management
implications, 65
| Touladi, 523
_Towhee, Spotted, 378
| Tracheoniscus rathkei, 388
i Tracy, S., 127
Tragopogon dubius, 300
| Trechus obtusus, 79
| Trichodezia albovittata, 539
| Trientalis europaea, 560
Trifolium spp., 253,362
dubium, 170
| pratense, 560
Triglochin spp., 247
maritima, 226
palustre, 560
Trillium sp., 365
Triphosa haesitata, 539
|. Triteleia grandiflora, 174
grandiflora var. howellii, 174
INDEX TO VOLUME 118
673
howellti, 174
Triteleia, Howell’s, 174
Triteleia howellii, an Endangered Lily in Canada, Conserva-
tion Evaluation of Howell’s Triteleia, 174
Triteleia, Triteleia howellii, an Endangered Lily in Canada,
Conservation Evaluation of Howell’s, 174
Troglodytes aedon, 378
Trout, Brown, 113
Cutthroat, 448
Truite brune, 523
Trypanosoma, 236
avium, 237
Tsuga spp., 499
canadensis, 41,251,361,508
heterophylla, 159
mertensiana, 159
Tubularia crocea, 78
Tumble-mustard, Tall, 300
Tunicate, 79
Turdus migratorius, 381
Turkey, Eastern Wild, 251
Turkey, Meleagris gallopavo silvestris, Behavior in Central
Ontario During Winter, Wild, 251
Turnock, W.J. and I.L. Wise. Density and Survival of Lady
Beetles (Coccinellidae) in Overwintering Sites in
Manitoba*, 309
Turtle, Green, 72,579,611
Hawksbill, 580
Kemp’s Ridley, 580
Leatherback, 72,579
Loggerhead, 579
Murray Short-necked, 610
Snapping, 610
Turtle, Caretta caretta, and the First Record of a Green Tur-
tle in Atlantic Canada, Hybridization between a Green
Turtle, Chelonia mydas, and Loggerhead, 579
Turtle, Chelonia mydas, and Loggerhead Turtle, Caretta caret-
ta, and the First Record of a Green Turtle in Atlantic
Canada, Hybridization between a Green, 579
Turtle in Atlantic Canada, Hybridization between a Green Tur-
tle, Chelonia mydas, and Loggerhead Turtle, Caretta
caretta, and the First Record of a Green, 579
Turtles, Chelydra serpentina?, Is Cost of Locomotion the
Reason for Prolonged Nesting Forays of Snapping.
610
Turtles in British Columbia waters: a reassessment, Status
of marine, 72
Tylothallia biformigera, 424
Typha spp., 136,318
latifolia, 253,546,560
Udea itysalis, 537
Ulmus americana, 310,508
Underwood, T.J., 85
Untereiner, W.A., 90
Update on Quebec Amphibian and Reptile Atlas Project: Rana-
Saura 6(2), 294
Uraniidae, 539
Uria aalge, 258
lomvia, 602
Urodidae, 536
Ursus spp., 443
americanus, 41.96,370
arctos, 117,134,239,247,370,499,603
maritimus, 395,602
674
Ursus arctos, and Gray Wolves, Canis lupus, at Katmai Nation-
al Park and Preserve, Alaska, Interactions of Brown
Bears, 247
Ursus arctos, in Southeastern Alaska, Seed Dispersal by
Brown Bears, 499
Ursus arctos, in the Central Canadian Arctic, Movements of
Subadult Male Grizzly Bears, 239
Ursus maritimus, Excavation of an Arctic Fox, Alopex lago-
pus, den by a Polar Bear, 602
Ursus maritimus, in the Alaskan Beaufort, Chukchi, and
Northern Bering Seas, Observations of Habitat Use
by Polar Bears, 395
Urtica dioica ssp. gracilis, 560
Utricularia minor, 560
Vaccinium sp., 159,251,500
alaskense, 500
angustifolium, 195
globulare, 198
membranaceum, 560
myrtilloides, 195
ovalifolium, 500
vitis-idaea, 591
Vaccinium angustifolium, and Velvet Leaf Blueberry, Vac-
cinium myrtilloides, Production in Eastern Ontario,
Effect of Fire Intensity and Depth of Burn on Low-
bush Blueberry, 195
Vaccinium myrtilloides, Production in Eastern Ontario, Effect
of Fire Intensity and Depth of Burn on Lowbush Blue-
berry, Vaccinium angustifolium, and Velvet Leaf Blue-
berry, 195
Vahlodea atropurpurea, 560
Valerian, Sitka, 577
Valeriana sitchensis, 560
Vallisneria americana, 318
Veery, 232
Venerupis philippinarum, 78
Venusia cambrica, 539
pearsalli, 539
Verbascum thapsus, 300
Verbena bonariensis, 614
Vermivora celata, 381
chrysoptera, 232
peregrina, 48
Vernalgrass, Sweet, 177
Verrucaria sp., 406
amphibia, 411
degelii, 411
durietzii, 420
epimaura, 406
erichsenii, 410
halizoa, 424
maura, 408
mucosa, 410
sandstedei, 406
schofieldii, 406
silicicola, 424
striatula, 406
Vervain, Purpletop, 614
Vetch, American, 300,574
Common, 174
Viburnum, 500
cassinoides, 253
Vicia americana, 300,560
sativa, 174
THE CANADIAN FIELD-NATURALIST
Vol. 118
Villemure, M. and H. Jolicoeur. First Confirmed Occurrence
of a Wolf, Canis lupus, South of the St. Lawrence
River in Over 100 Years, 608
Viola praemorsa ssp. praemorsa, 175
renifolia var. brainerdii, 560
Violet, Kidney-leaved, 574
Yellow Montane, 175
Vireo cassinii, 378
flavifrons, 232
gilvus, 232
olivaceus, 231
solitarius, 48
Vireo, Blue-headed, 48
Cassin’s, 378
Red-eyed, 231
Warbling, 232
Yellow-throated, 232
Vole, 342
Heather, 438
Long-tailed, 300
Meadow, 342,400
Montane, 300
Prairie, 342
Vole, Genus Phenacomys, in Alaska, The Heather, 438
Vulpes vulpes, 40,58,69,96,244,249 273,368
Wade, K.D., 95
Wall-creeper, 614
Warbler, Bay-breasted, 48
Black-and-white, 230
Black-throated Green, 48,232
Blackburnian, 48
Cerulean, 229
Chestnut-sided, 232
Golden-winged, 232
Magnolia, 48
Myrtle, 48
Orange-crowned, 381
Tennessee, 48
Townsend’s, 382
* Yellow, 86,232
Yellow-rumped, 48,86,232,378
Warbler, Dendroica cerulea Management on Eastern Ontario
Bird Species, Predicting the Effects of Cerulean,
229
WARS 1983-2002 Special Annual Report Wildlife Accident
Reporting and Mitigation, 645
Wart-cress, Lesser, 613
Washburn, B.E., 185
Wasp, Parasitoid, 122
Wasps, Baeus sp. and Gelis sp., in the Egg Sacs of the Wolf
Spiders Pardosa moesta and Pardosa sternalis (Ara-
neae, Lycosidae) in Southeastern Idaho, Occurrence
of Parasitoid, 122
Water-hemlock, Spotted, 574
Watersnake, Northern, 435
Watersnake, Nerodia sipedon sipedon, Frequency of Tail
Breakage of the Northern, 435
Waterthrush, Northern, 232
Waterweed, Canada, 318
Waxwing, Cedar, 232,378
Weasel, 96,306
Least, 403
Weathervane X Japanese Scallop Hybrid, 78
Weed, Willow, 568
2004
Weevil, White Pine, 41
Wetzel, S., 195
Whale, Dwarf Sperm, 495
Pygmy Sperm, 495
Sperm, 495
Whale, Kogia breviceps, in the Northern Gulf of St. Law-
rence, Canada, Stranding of a Pygmy Sperm, 495
Wheatgrass, Crested, 300
Whip-poor-will, 230
Whitlow-grass, Wood, 572
Wilkerson, C.D., 267
Williston, P., Review by, 290
Willow, 57,211,247,253,268,356,370,530
Peachleaf, 309
Willson, M.F. and S.M. Gende. Seed Dispersal by Brown
Bears, Ursus arctos, in Southeastern Alaska, 499
Willson, M.F. Gulls, Larus spp., Foraging at Pink Salmon,
Oncorhynchus gorbuscha, Spawning Runs, 442
Wilson, S.F., A. Hahn, A. Gladders, K.M.L. Goh, and
D.M. Shackleton. Morphology and Population Char-
acteristics of Vancouver Island Cougars, Puma con-
color vancouverensis, 159
Wintergreen, 196
Wise, I.L., 309
Wockia asperipunctella, 536
Wolf, 115,127,134,278,368,603,608
Eastern, 608
Gray [Grey], 42,57,61,95,194,247,350,361,608
Wolf, Canis lupus, Pack Density, Record High, 127
Wolf, Canis lupus, South of the St. Lawrence River in Over
100 Years, First Confirmed Occurrence of a, 608
Wolverine, 56,61
Wolverine, Gulo gulo luscus, Resting Sites and Caching
Behavior in the Boreal Forest, 61
Wolverines, Gulo gulo luscus, in the boreal forest, Effects
of mid-winter snow depth on stand selection by, 56
Wolves, Canis lupus, at Katmai National Park and Preserve,
Alaska, Interactions of Brown Bears, Ursus arctos,
and Gray, 247
Wolves, Canis lupus, in and near Pukaskwa National Park,
Ontario, Demographic patterns and limitations of Grey,
95
Wolves, Canis lupus, in Relation to Forest Harvesting in
West-central Alberta, Winter Habitat Use by, 368
Wolves, Canis lupus, Unusual Behavior by Bison, Bison
bison, Toward Elk, Cervus elaphus, and, 115
Wood-Peewee, Eastern, 232
Woodlouse, 388
Woodpecker, Downy, 358
Woodsia alpina, 560
ilvensis, 560
Woodsia, Northern, 560
Rusty, 560
Woolly-heads, Slender, 169
Tall, 169
INDEX TO VOLUME 118
675
Woolly-heads, Psilocarphus elatior, an Endangered Herb in
Canada, Conservation Evaluation of the Pacific Pop-
ulation of Tall, 169
Wren, Bewick’s, 378
House, 378
Wright, J.D. and J. Ernst. Effects of mid-winter snow depth
on stand selection by Wolverines, Gulo gulo luscus,
in the boreal forest, 56
Wright, J.D. and J. Ernst. Wolverine, Gulo gulo luscus, Rest-
ing Sites and Caching Behavior in the Boreal Forest,
61
Wright, K.G., 264
Xanthia tatago, 542
Xanthocephalus xanthocephalus, 207
Xanthorhoe abrasaria, 539
decoloraria, 539
ferrugata, 539
fossaria, 539
iduata, 539
lacustrata, 539
Xanthoria, 420
candelaria, 411
parietina, 420
Xanthotype sospeta, 538
Xenolechia aethiops, 534
Xestia normaniana, 543
smithii, 543
Xylena curvimacula, 542
Xylotype arcadia, 542
Yarrow, 166
Yellowthroat, Common, 86,232
Yew, Canada, 41
Yponomeutidae, 532
Ypsolopha canariella, 533
dentiferella, 533
Yukon Territory, New Records of Cyperaceae and Juncaceae
from the, 266
Yukon Territory VI, New Records of Vascular Plants in the,
558
Yunger, J.A., 341
Zanclognatha lutalba, 540
Zapus hudsonius, 403
Zea mays, 253,365
Zeiraphera canadensis, 536
fortunana, 536
unfortunana, 536
Zenophleps alpinata, 539
Zonotrichia leucophrys, 378
Zophodia grossulariella, 536
Zostera marina, 225
Zostera marina, Wrack by Three Species of Ladybird Beetles
(Coleoptera: Coccinellidae) in Prince Edward Island,
Use of Eelgrass, 225
676
Index to Book Reviews
Botany
Berkutenko, A.N., H.G. Lumsden, and D. Lumsden. Flora
and Climatic Conditions of the North Pacific: A Col-
lection of Scientific Papers, 637
Beresford-Kroeger, D. Arboretum America, A Philosophy of
the Forest, 474
Boulet, B. Les champignons des arbres de l’est de |’ Amerique
du Nord, 146
Clark, L.J. Lewis Clarks’s Field Guide to Wild Flowers of
the Sea Coast in the Pacific Northwest, 476
Clark, L.J. Wild Flowers of Field & Slope in the Pacific
Northwest, 289,476
Clark, L.J. Wild Flowers of Forest & Woodland in the Pacific
Northwest, 289,476
Clark, L.J. Wild Flowers of the Mountains in the Pacific
Northwest, 289,476
DiGregorio, M.J. and J. Wallner. Cape Cod Wildflowers: A
Vanishing Heritage, 475
Gleason, H.A. and A. Cronquist. Manual of Vascular Plants
of Northeastern United States and Adjacent Canada:
Second Edition, 147
Martin, N.D. and N.M. Martin. Biotic Forest Communities
of Ontario, 146
Martin, P. The Wild Orchids of North America, North of Mex-
ico, 147
Nicholls G. and R. Lupp. Alpine Plants of North America: An
Encyclopedia of Mountain Flowers from the Rockies
to Alaska, 474
Trelawny, J.G. Wild Flowers of the Yukon, Alaska & North-
western Canada, 2nd Edition, 289
Waldron, G. Trees of the Carolinian Forest: A Guide to
Species, Their Ecology and Uses, 148
Environment
Boelens, B. and M. Watkins. Whose Bird? 150
Bryson, M.A. Visions of the Land: Science, Literature, and the
American Environment from the Era of Exploration
to the Age of Ecology, 478
Conner, J.K. and D.L. Hartl. A Primer of Ecological Genetics,
480
Czajkowski, C. Snowshoes & Spotted Dick; Letters from a
Wilderness Dweller, 151
Dietrich, W. Natural Grace: The Charm, Wonder, & Lessons
of Pacific Northwest Animals & Plants, 152
Frelich, L.E. Forest Dynamics and Disturbance Regimes: Stud-
ies from Temperate Evergreen-Deciduous Forests, 150
Josephson Weddell, B. Conserving Living Resources in the
Context of a Changing World, 477
Mitchell, B. Resource and Environmental Management in
Canada: Addressing Conflict and Uncertainty, 640
Newell, J. The Russian Far East, 638
Suzuki, D. and Dressel, H. Good News for a Change: How
Everyday People are Helping the Planet, 149
Wolfe, D.W. Tales from the Underground: A Natural History
of Subterranean Life, 153
Young, A.G. and G.M. Clarke. Genetics, Demography and via-
bility of Fragmented Populations, 478
Miscellaneous
Burnett, J.A. A Passion for Wildlife: The History of the Cana-
dian Wildlife Service, 290
THE CANADIAN FIELD-NATURALIST
Vol. 118
Edlow, J.A. Bull’s Eye: Unraveling the Medical Mystery of
Lyme Disease, 641
Jennings, J. The Canoe: A Living Tradition, 290
Kareiva, P. and S.A. Levin. The Importance of Species: Per-
spective on Expendability and Triage, 641
Snetsinger, P. Birding on Borrowed Time, 291
Yochelson, E.L. Smithsonian Institution Secretary Charles
Doolittle Walcott, 481
Zoology
Attenborough, D. The Life of Mammals, 286
Bird, D.M. The Bird Almanac, 630
Bowman, T.D. Field Guide to Bird Nests and Eggs of Alaska’s
Coastal Tundra, 632
Bumstead, P.E. Canadian Skin and Scales: A Complete Ency-
clopedia of Canadian Amphibians and Reptiles, 467
Cannings, R. and S. Cannings. British Columbia: A Natural
History. Revised and Updated, 631
Carroll, D. Self-Portrait With Turtles: A Memoir, 471
Cox, B. Conversations with an Eagle, 283
Crump, M. In Search of the Golden Frog, 282
del Hoyo, J., A. Elliott and D. Christie. Handbook of Birds of
the World: Volume 9 Cotingas to Pipits and Wagtails,
631
Ducey, J.E. Birds of the Untamed West: The History of Bird-
life in Nebraska, 1750 to 1975, 466
Duff, A. and A. Lawson. Mammals of the World: A Checklist,
634
Dunne, P. Pete Dune on Bird Watching: The How-to, Where-
to and When-to of Birding, 473
Early, C. Sparrows and Finches of the Great Lakes and Eastern
North America, 288
Early, C. Warblers of the Great Lakes and Eastern North Amer-
ica, 288
Eisner, T. For Love of Insects, 468
Feldhamer, G.A., B.C. Thompson and J.A. Chapman. Wild
Mammals of North America: Biology, Management,
and Conservation (Second edition), 472
Ferrari, A. & A. Sharks, 282
Ferri, V. Turtles and Tortoises, 143
Heide-Jérgensen, M.P., O. Wiig, and D.G. Pike. Belugas in
the North Atlantic and the Russian Arctic, 144
Heintzelman, D. All-Weather Hawk Watcher’s Field Journal,
471
Heintzelman, D.S. Guide to Hawk Watching in North Amer-
ica, 632
Johnsgard, P.A. North American Owls, Biology and Natural
History, Second Edition, 284
Johnston, D.W. The History of Ornithology in Virginia, 470
Jones, H.L. Birds of Belize, 140
Joynt, A. and M.G. Sullivan. Fish of Alberta, 281
Limbert, M. The Uses and Curation of Birds’ Egg Collec-
tions: An Examination and Biography, 465
Linder, G., S.K. Krest, D.W. Sparling. Amphibian Decline:
An Integrated Analysis of Multiple Stressor Effects,
138
Lockwood, J.A. Locust: The Devastating Rise and Mysterious
Disappearance of the Insect that Shaped the American
Frontier, 633
McCabe, R.E., B.W. O’ Gara, and H.M. Reeves. Prairie Ghost:
Pronghorn and Human Interaction in Early America,
635
2004
McCulloch, N. A Guide to the Birds of St. Helena and Ascen-
sion Island, 636
Melvin, E.F. and J.K. Parrish. Seabird Bycatch: Trends, Road-
blocks, and Solutions, 285
Morton, M.L. The Mountain White-Crowned Sparrow: Migra-
tion and Reproduction at High Altitude, 284
O'Toole, C. The Firefly Encyclopedia of Insects and Spiders,
145
Perrins, C. The Firefly Encyclopedia of Birds, 139
Pianka, E.R., L.J. Vitt. Lizards: Windows to the Evolution
of Diversity, 141
Pough, F.H., R.M. Andrews, J.E. Cadle, M.L. Crump, A.H.
Savitsky and D.D. Wells. Herpetology: Third Edition,
140
Richards, J.M., Y.T. Tymstra and A.W. White. Birds of Nuna-
vut: A Checklist, 465
Rising, J.D. Geographic Variation in Size and Shape of Svan-
nah Sparrows (Passerculus sanwichensis), 287
Sharpe, R.S., W.R. Silcock and J.G. Jorgensen. Birds of Neb-
raska: Their Distribution and Temporal Occurrence,
466
INDEX TO VOLUME 118
677
Simpson, K. and N. Day. Birds of Australia (Seventh edition),
630
Sinclair, P.H., W.A. Nixon, C.D. Eckert and N.L. Hughes.
Birds of the Yukon Territory, 288
Somma, L.A. Parental Behavior in Lepidosaurian and Tes-
tudinian Reptiles: A Literature Survey, 635
Stewart, K.W. and D.A. Watkinson. The Freshwater Fishes
of Manitoba, 469
Stuart, C. & T. Birds of Africa: From Seabirds to Seed-eaters,
138
Swarth, C.W., W.M. Roosebrug and E. Kiviat. Conservation
and Ecology of Turtles of the Mid-Atlantic Region:
A Symposium, 468
Waldbauer, G. What Good are Bugs? Insects in the Web of
Life, 144
Wheeler, B. Raptors of Eastern North America, 143
Wheeler, B.K. Raptors of Western North America, 142
Advice for Contributors to The Canadian Field-Naturalist
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678
| TABLE OF CONTENTS (concluded) Volume 118 Number 4
| Tributes
| A tribute to Thomas Henry Manning 1911-1998 BRENDA CARTER
| A tribute to Victor Kent Prest 1913-2003 A. S. Dyke, D. A. Hopcson, E. L. BOUSFIELD, R. E. BEDFORD
‘Book Reviews
| ZOOLOGY: Birds of Australia (Seventh edition) — The Bird Almanac — Handbook of Birds of the World:
Volume 9 Cotingas to Pipits and Wagtails — British Columbia: A Natural History Revised and Updated
—A Field Guide to Bird Nests and Eggs of Alaska’s Coastal Tundra — Guide to Hawk Watching in
North America — Locust: the Devastating Rise and Mysterious Disappearance of the Insect that shaped
the American Frontier — Mammals of the World: A Checklist — Parental Behavior in Lepidosaurian
and Testudinian Reptiles: A Literature Survey — Prairie Ghost: Pronghorn and Human Interaction in
Early America — A Guide to the Birds of St. Helena and Ascension Island
| BoTaNy: Flora and Climatic Conditions of the North Pacific: A Collection of Scientific Papers
| ENVIRONMENT: The Russian Far East — Resource and Evironmental Management in Canada:
Addressing Conflict and Uncertainty
| MISCELLANEOUS: Bull’s Eye: Unraveling the Medical Mystery of Lyme Disease; The Importance of Species:
| Perspective on Expendibility and Triage
q
| NEw TITLES
News and Comment
| RENEW 2004 Recovery of Nationally Endangered Wildlife in Canada Annual Report (14) — Calendar:
| Endangered Reptiles of Canada 2004 and 2005 — Canadian Species at Risk November 2004 —
Froglog: Newsletter of the Declining Amphibian Populations Task Force (65, 66) — The Boreal Dip
Net/L’Epuisette Boreale: Newsletter of the Canadian Amphibian and Reptile Conservation Network/
Reseau Canadien de Conservation des Amphibiens et des Reptiles 9(1) December 2004 — Marine Turtle
Newsletter (106) — WARS 1983-2002 Special Annual Report Wildlife Accident Reporting and Mitigation
The Ottawa Field-Naturalists’ Club Awards for 2003
Errata The Canadian Field-Naturalist 118(3)
| Index to Volume 118 COMPILED BY LESLIE CODY
| Advice to Contributors
| Mailing date of the previous issue 118(3): 21 October 2005
2004
618
626
630
637
638
641
643
644
646
649
650
678
THE CANADIAN FIELD-NATURALIST Volume 118 Number 4
2004)
Articles
Stranding of a Pygmy Sperm Whale, Kogia breviceps, in the northern Gulf of St. Lawrence, Canada
LENA MEASURES, BENOIT ROBERGE, and RICHARD SEARS
Seed dispersal by Brown Bears, Ursus arctos, in southeastern Alaska
Mary F. WILLSON and Scott M. GENDE
A mapping of the present and past forest-types of Prince Edward Island
D. G. SoBey and W. M. GLEN
Inventaire printanier d’une frayere multispécifique: ’ichtyofaune des rapides de la riviere
Gatineau, Québec ANNIE COMTOIS, FRANCOIS CHAPLEAU, CLAUDE B. RENAUD,
HENRI FOURNIER, BRENT CAMPBELL, and RICHARD PARISEAU
Moths and butterflies (Lepidoptera) of the boreal mixedwood forest near Lac La Biche,
Alberta, including new provincial records
GREG R. POHL, DAvID W. LANGOR, JEAN-FRANCOIS LANDRY, and JOHN R. SPENCE
Pilose Braya, Braya pilosa Hooker (Cruciferae, Brassicaceae), an enigmatic endemic of
arctic Canada JAMES G. HARRIS
New records of vascular plants in the Yukon Territory VI
WILLIAM J. Copy, CATHERINE E. KENNEDY, BRUCE BENNETT, and PHIL CASWELL
Hybridization between a Green Turtle, Chelonia mydas, and a Loggerhead Turtle, Caretta caretta,
and the first record of a Green Turtle in Atlantic Canada
MICHAEL C. JAMES, KATHLEEN MARTIN, and PETER H. DUTTON
A snow-tracking protocol used to delineate local Lynx, Lynx canadensis, distributions
JOHN R. SQUIRES, KEVIN S. MCKELVEY, and LEONARD F. RUGGIERO
Hummock vegetation at the arctic tree-line near Churchill, Manitoba JORG TEWS
Effects of Lodgepole Pine Dwarf Mistletoe, Arceuthobium americanum, on Jack Pine,
Pinus banksiana, growth in Manitoba Brock Epp and JACQUES C. TARDIF
Notes
Excavation of an Arctic Fox, Alopex lagopus, den by a Polar Bear, Ursus maritimus
EVAN RICHARDSON and RYAN K. BROOK
Two Great Black-backed Gulls, Larus marinus, kill male Longtailed Duck, Clangula hyemalis
MARTHA DowsLey and ANDREW CIRTWILL
First record of Mountain Lions, Puma concolor, in Elk Island National Park, Alberta
GLYNNIS A. Hoop and TIM NEUFELD
First confirmed occurrence of a Wolf, Canis lupus, south of the St. Lawrence River in over 100 years
Mario VILLEMURE and HELENE JOLICOEUR
Is cost of locomotion the reason for prolonged nesting forays of Snapping Turtles, Chelydra serpentina?
SHANE R. DE SOLLA and KIM J. FERNIE
Significant vascular plant records from the Hamilton area, Ontario CARL ROTHFELS
Do Rhinoceros Auklet, Cerorhinca monocerata, fledglings fly to the sea from their natal burrows
JAMES L. HAYWARD and JERE K. CLAYBURN
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